Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-24 Thread MEM
Morning Jim   How, you ask? 


Take two large meteoroids and wack them together at incredible speeds.  What is 
not vaporized or pulverized will sheer and move in an opposite vector to 
relieve compressional forces where the two meteoroids interfaced. The 
compression varies according to the macro surface: where there are ridges/bumps 
on one body, the other body at that junction will see more compressional force 
and where there are valleys one will see less compressional and vice versa.  
The rupture of the matrix is nature's way of balancing the competition for 
space and the kinetic energy vectors: the inertia thingy. We know it as equal 
and opposite reactions.  Since silicate is not elastic, it will break and areas 
of it will be displaced relative to the other side of the fracture. Since the 
rupture is rarely even, the two sides will grind against each other leaving 
skid marks all other things considered.

Both the energy and masses have to return to balance after the impact. 
Slickensides represent areas of the original body where sheer exceeds physical 
bonds and will be displaced to accommodate the compression forces(solids don't 
compress but they do respond to compressional forces)

Elton




 From: Jim Wooddell jim.woodd...@suddenlink.net
To: meteorite-list@meteoritecentral.com 
Sent: Wednesday, May 22, 2013 8:31 AM
Subject: Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?
 

Good morning all!

Can anyone explain to me how slickensides are created in bonded matrix 
in space in only minute areas of a large body?

Thanks!

Jim Wooddell
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-22 Thread Meteoriteshow
Yes it is. A very famous meteorite that shows great slickensides is Zag
actually.

Have all a great day!
Frederic Beroud
www.meteoriteshow.com
IMCA #2491

-Message d'origine-
De : meteorite-list-boun...@meteoritecentral.com
[mailto:meteorite-list-boun...@meteoritecentral.com] De la part de Anne
Black
Envoyé : mardi 21 mai 2013 23:03
À : jim.woodd...@suddenlink.net; meteorite-list@meteoritecentral.com
Objet : Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

Does this help Jim?

http://www.impactika.com/CH-126slick.jpg

To me, slickensides look almost like streaks, and yes, shiny.
Like my cat scratched it!  ;-)


Anne M. Black
www.IMPACTIKA.com
impact...@aol.com


-Original Message-
From: Jim Wooddell jim.woodd...@suddenlink.net
To: meteorite-list meteorite-list@meteoritecentral.com
Sent: Tue, May 21, 2013 2:08 pm
Subject: Re: [meteorite-list] Chelyabinsk - slickensides or shock 
planes?


Welp, I just need to see one up close. But in the mean time here is a
paper on the subject that may be of interest...

http://adsabs.harvard.edu/full/1966Metic...3...31D

Jim


On 5/21/2013 10:26 AM, Michael Farmer wrote:
 Jim, there are shock veins and slickensides. They are not the same 
thing. They
are result of shock but not melting like the full melt veins are.
 I have hundreds of pieces with slickensides. I am traveling so I 
can't show
photos.
 Perhaps later.
 Michael Farmer

 Sent from my iPhone

 On May 21, 2013, at 12:19 PM, Jim Wooddell 
jim.woodd...@suddenlink.net
wrote:

 Hi Jim Baxter,
 And, that is what I am not seeing.  I'am going to be a very hard 
sell on the
term slickensides until I see something that scientifically supports it 
and why
it is there.  Do the threads actually appear and are they threads??
 In my mind, the coming apart part would not create a slickenside 
(cool state)
where as the coming together with great pressure and time would.  Just 
thinking
out loud, not qualified to say one way or the other!
 I also see where this appearance is shown lower in topography in 
it's area
which, to me, would be odd for slickenside.

 Cheers!

 Jim Wooddell




 On 5/21/2013 9:18 AM, Jim Baxter wrote:
 Slickensides are polished surfaces caused by lateral movement along 
a fault
plane. In hand specimens they feel rough when you rub your finger in 
one
direction and smooth when you rub it in the other. Not sure that test 
would be
feasible on the size specimens most of us own. In theory if the fault 
planes
represent planes of weakness along which breaks occur then you could be 
seeing
both things - slickensides that formed by lateral movement along the 
shock plane
when the stone fractured.

 Jim Baxter
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 -
 No virus found in this message.
 Checked by AVG - www.avg.com
 Version: 2013.0.3343 / Virus Database: 3162/6344 - Release Date: 
05/21/13




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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-22 Thread Derek Yoost
I've also seen them in the Ochansk meteorite.

Thanks, Derek.

Meteoriteshow meteorites...@free.fr wrote:

Yes it is. A very famous meteorite that shows great slickensides is Zag
actually.

Have all a great day!
Frederic Beroud
www.meteoriteshow.com
IMCA #2491

-Message d'origine-
De : meteorite-list-boun...@meteoritecentral.com
[mailto:meteorite-list-boun...@meteoritecentral.com] De la part de Anne
Black
Envoyé : mardi 21 mai 2013 23:03
À : jim.woodd...@suddenlink.net; meteorite-list@meteoritecentral.com
Objet : Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

Does this help Jim?

http://www.impactika.com/CH-126slick.jpg

To me, slickensides look almost like streaks, and yes, shiny.
Like my cat scratched it!  ;-)


Anne M. Black
www.IMPACTIKA.com
impact...@aol.com


-Original Message-
From: Jim Wooddell jim.woodd...@suddenlink.net
To: meteorite-list meteorite-list@meteoritecentral.com
Sent: Tue, May 21, 2013 2:08 pm
Subject: Re: [meteorite-list] Chelyabinsk - slickensides or shock 
planes?


Welp, I just need to see one up close. But in the mean time here is a
paper on the subject that may be of interest...

http://adsabs.harvard.edu/full/1966Metic...3...31D

Jim


On 5/21/2013 10:26 AM, Michael Farmer wrote:
 Jim, there are shock veins and slickensides. They are not the same 
thing. They
are result of shock but not melting like the full melt veins are.
 I have hundreds of pieces with slickensides. I am traveling so I 
can't show
photos.
 Perhaps later.
 Michael Farmer

 Sent from my iPhone

 On May 21, 2013, at 12:19 PM, Jim Wooddell 
jim.woodd...@suddenlink.net
wrote:

 Hi Jim Baxter,
 And, that is what I am not seeing.  I'am going to be a very hard 
sell on the
term slickensides until I see something that scientifically supports it 
and why
it is there.  Do the threads actually appear and are they threads??
 In my mind, the coming apart part would not create a slickenside 
(cool state)
where as the coming together with great pressure and time would.  Just 
thinking
out loud, not qualified to say one way or the other!
 I also see where this appearance is shown lower in topography in 
it's area
which, to me, would be odd for slickenside.

 Cheers!

 Jim Wooddell




 On 5/21/2013 9:18 AM, Jim Baxter wrote:
 Slickensides are polished surfaces caused by lateral movement along 
a fault
plane. In hand specimens they feel rough when you rub your finger in 
one
direction and smooth when you rub it in the other. Not sure that test 
would be
feasible on the size specimens most of us own. In theory if the fault 
planes
represent planes of weakness along which breaks occur then you could be 
seeing
both things - slickensides that formed by lateral movement along the 
shock plane
when the stone fractured.

 Jim Baxter
 __

 Visit the Archives at http://www.meteorite-list-archives.com
 Meteorite-list mailing list
 Meteorite-list@meteoritecentral.com
 http://six.pairlist.net/mailman/listinfo/meteorite-list

 -
 No virus found in this message.
 Checked by AVG - www.avg.com
 Version: 2013.0.3343 / Virus Database: 3162/6344 - Release Date: 
05/21/13




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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-22 Thread Jim Wooddell

Good morning all!

Can anyone explain to me how slickensides are created in bonded matrix 
in space in only minute areas of a large body?


Thanks!

Jim Wooddell
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-22 Thread Malvin Bishop Jr


Since the reference to slickensides has been a topic recently, I thought 
some would be interested in this nice example I just found being offered 
on eBay.  It shows the feature very well.



http://www.ebay.com/itm/HUGE-FIREBALL-NEWEST-FALL-SLICKENSIDE-FRAGMENT-CHELYABINSK-METEORITE-22-5-GM-/190831604603?pt=LH_DefaultDomain_0hash=item2c6e73337b


Mal
IMCA#6819
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-22 Thread Graham Ensor
I'm not so sure this picture shows slickensides...if you look closely
at the picture there are veins of melt running from the black
areaI think it is just a break through one of the large melt
pockets that are evident in Chelyabinsk.it does have the look of a
slickenside but they are just paper thin black melt sheets scored in
one direction and would not have thicker melt veins coming from them.

Graham

On Wed, May 22, 2013 at 2:17 PM, Malvin Bishop Jr
magbi...@lowcountry.com wrote:

 Since the reference to slickensides has been a topic recently, I thought
 some would be interested in this nice example I just found being offered on
 eBay.  It shows the feature very well.


 http://www.ebay.com/itm/HUGE-FIREBALL-NEWEST-FALL-SLICKENSIDE-FRAGMENT-CHELYABINSK-METEORITE-22-5-GM-/190831604603?pt=LH_DefaultDomain_0hash=item2c6e73337b


 Mal
 IMCA#6819

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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Jim Wooddell
Hi Bob and all!
I might be wrong in assuming, but your slickensides sounds like you
are attempting to describe secondary fusion???

We have lots of evidence in various meteorites where they broke apart
for whatever reason at the weak boundaries.  For example, Franconia
area meteorites (some) break apart from both sides of a metal vein
leaving three pieces...two chondrite fragments and an H-Metal
cornflake.
It's sort of like looking at a bad weld through xray.
How can you tell?  Look at more and look closer.  A 3D CT sort of scan
that has become popular with Sutter's Mill or Dr. Agee's research on
Black Beauty may reveal what you speak of.   Just my thoughts.

Kind Regards,

Jim


On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:
 Hi everyone,
 Many pieces of broken Chelyabinsk specimens display what appears like
 fusion crust over slickensides, but is that what it really is? I've
 talked with Blaine Reed and he thinks we're seeing blackish shock
 veins (planes really) where the meteorite split along a line of
 weakness. He even mentioned a piece he's seen where a large shock vein
 in the matrix leads directly to the broken, dark face. Assuming
 Chelyabinsk shows both slickensides and shock vein planes, how do you
 tell them apart?
 Thanks for your thoughts.
 Bob
 __

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 Meteorite-list mailing list
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928-247-2675
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Malvin Bishop Jr

Hi Bob, Jim, and list -

One of my Chelyabinsk specimens shows a feature where it appears
to be fractured along a weakened shock vein/point where melt had
filled the vein before the actual splitting apart.  The melt is still
very evident covering a large portion of the fresh exposed matrix after 
the specimen split in two.


In short, I tend to agree with Blaine.


Regards,
Mal




On 5/21/2013 10:29 AM, Jim Wooddell wrote:

Hi Bob and all!
I might be wrong in assuming, but your slickensides sounds like you
are attempting to describe secondary fusion???

We have lots of evidence in various meteorites where they broke apart
for whatever reason at the weak boundaries.  For example, Franconia
area meteorites (some) break apart from both sides of a metal vein
leaving three pieces...two chondrite fragments and an H-Metal
cornflake.
It's sort of like looking at a bad weld through xray.
How can you tell?  Look at more and look closer.  A 3D CT sort of scan
that has become popular with Sutter's Mill or Dr. Agee's research on
Black Beauty may reveal what you speak of.   Just my thoughts.

Kind Regards,

Jim


On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:

Hi everyone,
Many pieces of broken Chelyabinsk specimens display what appears like
fusion crust over slickensides, but is that what it really is? I've
talked with Blaine Reed and he thinks we're seeing blackish shock
veins (planes really) where the meteorite split along a line of
weakness. He even mentioned a piece he's seen where a large shock vein
in the matrix leads directly to the broken, dark face. Assuming
Chelyabinsk shows both slickensides and shock vein planes, how do you
tell them apart?
Thanks for your thoughts.
Bob
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Bob King
Hi Jim,
Thanks for your reply. No, what I'm seeing is different from the
secondary fusion crusts I typically see, and it's nearly identical on
many pieces. The broken faces have a planar, slickenside texture and
appear coated with gray material that's either fusion crust or as
Blaine thinks, an exposed shock plane.
Bob

On Tue, May 21, 2013 at 9:29 AM, Jim Wooddell jimwoodd...@gmail.com wrote:
 Hi Bob and all!
 I might be wrong in assuming, but your slickensides sounds like you
 are attempting to describe secondary fusion???

 We have lots of evidence in various meteorites where they broke apart
 for whatever reason at the weak boundaries.  For example, Franconia
 area meteorites (some) break apart from both sides of a metal vein
 leaving three pieces...two chondrite fragments and an H-Metal
 cornflake.
 It's sort of like looking at a bad weld through xray.
 How can you tell?  Look at more and look closer.  A 3D CT sort of scan
 that has become popular with Sutter's Mill or Dr. Agee's research on
 Black Beauty may reveal what you speak of.   Just my thoughts.

 Kind Regards,

 Jim


 On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:
 Hi everyone,
 Many pieces of broken Chelyabinsk specimens display what appears like
 fusion crust over slickensides, but is that what it really is? I've
 talked with Blaine Reed and he thinks we're seeing blackish shock
 veins (planes really) where the meteorite split along a line of
 weakness. He even mentioned a piece he's seen where a large shock vein
 in the matrix leads directly to the broken, dark face. Assuming
 Chelyabinsk shows both slickensides and shock vein planes, how do you
 tell them apart?
 Thanks for your thoughts.
 Bob
 __

 Visit the Archives at http://www.meteorite-list-archives.com
 Meteorite-list mailing list
 Meteorite-list@meteoritecentral.com
 http://six.pairlist.net/mailman/listinfo/meteorite-list



 --
 Jim Wooddell
 jimwoodd...@gmail.com
 928-247-2675
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Michael Mulgrew
Bob, Jim, List,

I have a small piece that displays the slickenside in 3 distinct
locations; it's definitely not secondary fusion crust.  Looking
forward to hearing more on the subject.

Michael in so. Cal.

On Tue, May 21, 2013 at 7:29 AM, Jim Wooddell jimwoodd...@gmail.com wrote:

 Hi Bob and all!
 I might be wrong in assuming, but your slickensides sounds like you
 are attempting to describe secondary fusion???

 We have lots of evidence in various meteorites where they broke apart
 for whatever reason at the weak boundaries.  For example, Franconia
 area meteorites (some) break apart from both sides of a metal vein
 leaving three pieces...two chondrite fragments and an H-Metal
 cornflake.
 It's sort of like looking at a bad weld through xray.
 How can you tell?  Look at more and look closer.  A 3D CT sort of scan
 that has become popular with Sutter's Mill or Dr. Agee's research on
 Black Beauty may reveal what you speak of.   Just my thoughts.

 Kind Regards,

 Jim


 On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:
  Hi everyone,
  Many pieces of broken Chelyabinsk specimens display what appears like
  fusion crust over slickensides, but is that what it really is? I've
  talked with Blaine Reed and he thinks we're seeing blackish shock
  veins (planes really) where the meteorite split along a line of
  weakness. He even mentioned a piece he's seen where a large shock vein
  in the matrix leads directly to the broken, dark face. Assuming
  Chelyabinsk shows both slickensides and shock vein planes, how do you
  tell them apart?
  Thanks for your thoughts.
  Bob
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  Meteorite-list mailing list
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 --
 Jim Wooddell
 jimwoodd...@gmail.com
 928-247-2675
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Bob King
Michael and all,
I forgot to add that even small 2-3g Chelyabinsks show this same
slick, grey material coating their broken faces. Can slickensides form
on rocks this small?
Bob

On Tue, May 21, 2013 at 9:43 AM, Michael Mulgrew mikest...@gmail.com wrote:
 Bob, Jim, List,

 I have a small piece that displays the slickenside in 3 distinct
 locations; it's definitely not secondary fusion crust.  Looking
 forward to hearing more on the subject.

 Michael in so. Cal.

 On Tue, May 21, 2013 at 7:29 AM, Jim Wooddell jimwoodd...@gmail.com wrote:

 Hi Bob and all!
 I might be wrong in assuming, but your slickensides sounds like you
 are attempting to describe secondary fusion???

 We have lots of evidence in various meteorites where they broke apart
 for whatever reason at the weak boundaries.  For example, Franconia
 area meteorites (some) break apart from both sides of a metal vein
 leaving three pieces...two chondrite fragments and an H-Metal
 cornflake.
 It's sort of like looking at a bad weld through xray.
 How can you tell?  Look at more and look closer.  A 3D CT sort of scan
 that has become popular with Sutter's Mill or Dr. Agee's research on
 Black Beauty may reveal what you speak of.   Just my thoughts.

 Kind Regards,

 Jim


 On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:
  Hi everyone,
  Many pieces of broken Chelyabinsk specimens display what appears like
  fusion crust over slickensides, but is that what it really is? I've
  talked with Blaine Reed and he thinks we're seeing blackish shock
  veins (planes really) where the meteorite split along a line of
  weakness. He even mentioned a piece he's seen where a large shock vein
  in the matrix leads directly to the broken, dark face. Assuming
  Chelyabinsk shows both slickensides and shock vein planes, how do you
  tell them apart?
  Thanks for your thoughts.
  Bob
  __
 
  Visit the Archives at http://www.meteorite-list-archives.com
  Meteorite-list mailing list
  Meteorite-list@meteoritecentral.com
  http://six.pairlist.net/mailman/listinfo/meteorite-list



 --
 Jim Wooddell
 jimwoodd...@gmail.com
 928-247-2675
 __

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 Meteorite-list mailing list
 Meteorite-list@meteoritecentral.com
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Michael Mulgrew
Bob,

My piece is just over 5g, but it was broken off a slightly larger
piece, probably less than 50g before it broke.

Michael in so. Cal.

On Tue, May 21, 2013 at 7:48 AM, Bob King nightsk...@gmail.com wrote:
 Michael and all,
 I forgot to add that even small 2-3g Chelyabinsks show this same
 slick, grey material coating their broken faces. Can slickensides form
 on rocks this small?
 Bob

 On Tue, May 21, 2013 at 9:43 AM, Michael Mulgrew mikest...@gmail.com wrote:
 Bob, Jim, List,

 I have a small piece that displays the slickenside in 3 distinct
 locations; it's definitely not secondary fusion crust.  Looking
 forward to hearing more on the subject.

 Michael in so. Cal.

 On Tue, May 21, 2013 at 7:29 AM, Jim Wooddell jimwoodd...@gmail.com wrote:

 Hi Bob and all!
 I might be wrong in assuming, but your slickensides sounds like you
 are attempting to describe secondary fusion???

 We have lots of evidence in various meteorites where they broke apart
 for whatever reason at the weak boundaries.  For example, Franconia
 area meteorites (some) break apart from both sides of a metal vein
 leaving three pieces...two chondrite fragments and an H-Metal
 cornflake.
 It's sort of like looking at a bad weld through xray.
 How can you tell?  Look at more and look closer.  A 3D CT sort of scan
 that has become popular with Sutter's Mill or Dr. Agee's research on
 Black Beauty may reveal what you speak of.   Just my thoughts.

 Kind Regards,

 Jim


 On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:
  Hi everyone,
  Many pieces of broken Chelyabinsk specimens display what appears like
  fusion crust over slickensides, but is that what it really is? I've
  talked with Blaine Reed and he thinks we're seeing blackish shock
  veins (planes really) where the meteorite split along a line of
  weakness. He even mentioned a piece he's seen where a large shock vein
  in the matrix leads directly to the broken, dark face. Assuming
  Chelyabinsk shows both slickensides and shock vein planes, how do you
  tell them apart?
  Thanks for your thoughts.
  Bob
  __
 
  Visit the Archives at http://www.meteorite-list-archives.com
  Meteorite-list mailing list
  Meteorite-list@meteoritecentral.com
  http://six.pairlist.net/mailman/listinfo/meteorite-list



 --
 Jim Wooddell
 jimwoodd...@gmail.com
 928-247-2675
 __

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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Sergey Vasiliev
Hi All,
Look at the two pictures of the same stone.

This is a fresh broken side with black shock veins on a very light matrix:
-  http://sv-meteorites.com/gallery/chelybinsk/02.jpg

And this side is secondary crust over the shock vein:
- http://sv-meteorites.com/gallery/chelybinsk/01.jpg

You can find a lot of interesting things in Chelyabinsk ;-)

All the best,
Sergey

On Tue, May 21, 2013 at 4:59 PM, Michael Mulgrew mikest...@gmail.com wrote:
 Bob,

 My piece is just over 5g, but it was broken off a slightly larger
 piece, probably less than 50g before it broke.

 Michael in so. Cal.

 On Tue, May 21, 2013 at 7:48 AM, Bob King nightsk...@gmail.com wrote:
 Michael and all,
 I forgot to add that even small 2-3g Chelyabinsks show this same
 slick, grey material coating their broken faces. Can slickensides form
 on rocks this small?
 Bob

 On Tue, May 21, 2013 at 9:43 AM, Michael Mulgrew mikest...@gmail.com wrote:
 Bob, Jim, List,

 I have a small piece that displays the slickenside in 3 distinct
 locations; it's definitely not secondary fusion crust.  Looking
 forward to hearing more on the subject.

 Michael in so. Cal.

 On Tue, May 21, 2013 at 7:29 AM, Jim Wooddell jimwoodd...@gmail.com wrote:

 Hi Bob and all!
 I might be wrong in assuming, but your slickensides sounds like you
 are attempting to describe secondary fusion???

 We have lots of evidence in various meteorites where they broke apart
 for whatever reason at the weak boundaries.  For example, Franconia
 area meteorites (some) break apart from both sides of a metal vein
 leaving three pieces...two chondrite fragments and an H-Metal
 cornflake.
 It's sort of like looking at a bad weld through xray.
 How can you tell?  Look at more and look closer.  A 3D CT sort of scan
 that has become popular with Sutter's Mill or Dr. Agee's research on
 Black Beauty may reveal what you speak of.   Just my thoughts.

 Kind Regards,

 Jim


 On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:
  Hi everyone,
  Many pieces of broken Chelyabinsk specimens display what appears like
  fusion crust over slickensides, but is that what it really is? I've
  talked with Blaine Reed and he thinks we're seeing blackish shock
  veins (planes really) where the meteorite split along a line of
  weakness. He even mentioned a piece he's seen where a large shock vein
  in the matrix leads directly to the broken, dark face. Assuming
  Chelyabinsk shows both slickensides and shock vein planes, how do you
  tell them apart?
  Thanks for your thoughts.
  Bob
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 --
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 jimwoodd...@gmail.com
 928-247-2675
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Sean T. Murray
I've noticed the same thing... I think this is a laterally exposed shock 
vein... sometimes they are crusted over, other times they are pretty fresh, 
so you can see the size of the exposed plane...


http://www.fallingrocks.com/Collections/Chelyabinsk.htm (4th picture down, 
top left of photo...)


It's hard to take a picture of because it is so reflective, but it it quite 
a beautiful feature of this fall.


Sean.

-Original Message- 
From: Sergey Vasiliev

Sent: Tuesday, May 21, 2013 11:16 AM
To: Michael Mulgrew
Cc: meteorite list
Subject: Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

Hi All,
Look at the two pictures of the same stone.

This is a fresh broken side with black shock veins on a very light matrix:
-  http://sv-meteorites.com/gallery/chelybinsk/02.jpg

And this side is secondary crust over the shock vein:
- http://sv-meteorites.com/gallery/chelybinsk/01.jpg

You can find a lot of interesting things in Chelyabinsk ;-)

All the best,
Sergey

On Tue, May 21, 2013 at 4:59 PM, Michael Mulgrew mikest...@gmail.com 
wrote:

Bob,

My piece is just over 5g, but it was broken off a slightly larger
piece, probably less than 50g before it broke.

Michael in so. Cal.

On Tue, May 21, 2013 at 7:48 AM, Bob King nightsk...@gmail.com wrote:

Michael and all,
I forgot to add that even small 2-3g Chelyabinsks show this same
slick, grey material coating their broken faces. Can slickensides form
on rocks this small?
Bob

On Tue, May 21, 2013 at 9:43 AM, Michael Mulgrew mikest...@gmail.com 
wrote:

Bob, Jim, List,

I have a small piece that displays the slickenside in 3 distinct
locations; it's definitely not secondary fusion crust.  Looking
forward to hearing more on the subject.

Michael in so. Cal.

On Tue, May 21, 2013 at 7:29 AM, Jim Wooddell jimwoodd...@gmail.com 
wrote:


Hi Bob and all!
I might be wrong in assuming, but your slickensides sounds like you
are attempting to describe secondary fusion???

We have lots of evidence in various meteorites where they broke apart
for whatever reason at the weak boundaries.  For example, Franconia
area meteorites (some) break apart from both sides of a metal vein
leaving three pieces...two chondrite fragments and an H-Metal
cornflake.
It's sort of like looking at a bad weld through xray.
How can you tell?  Look at more and look closer.  A 3D CT sort of scan
that has become popular with Sutter's Mill or Dr. Agee's research on
Black Beauty may reveal what you speak of.   Just my thoughts.

Kind Regards,

Jim


On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:
 Hi everyone,
 Many pieces of broken Chelyabinsk specimens display what appears like
 fusion crust over slickensides, but is that what it really is? I've
 talked with Blaine Reed and he thinks we're seeing blackish shock
 veins (planes really) where the meteorite split along a line of
 weakness. He even mentioned a piece he's seen where a large shock 
 vein

 in the matrix leads directly to the broken, dark face. Assuming
 Chelyabinsk shows both slickensides and shock vein planes, how do you
 tell them apart?
 Thanks for your thoughts.
 Bob
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--
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jimwoodd...@gmail.com
928-247-2675
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Jim Wooddell

Hi Sergey,

Those are nice pictures.
I see the secondary, I do not see slickenside.

I decided to take a look at all the samples for sale on Ebay. There is a 
fellow there selling slickenside fragments.   Even with those, I say 
look closer.


I imagine you have been very busy!  That's a good thing!

Cheers!

Jim Wooddell


On 5/21/2013 8:16 AM, Sergey Vasiliev wrote:

Hi All,
Look at the two pictures of the same stone.

This is a fresh broken side with black shock veins on a very light matrix:
-  http://sv-meteorites.com/gallery/chelybinsk/02.jpg

And this side is secondary crust over the shock vein:
- http://sv-meteorites.com/gallery/chelybinsk/01.jpg

You can find a lot of interesting things in Chelyabinsk ;-)

All the best,
Sergey



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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Sergey Vasiliev
Hi Jim,
There is a slickensides there, but very difficult to make a picture of
it because of reflection.
Best regards,
Sergey

On Tue, May 21, 2013 at 5:32 PM, Jim Wooddell
jim.woodd...@suddenlink.net wrote:
 Hi Sergey,

 Those are nice pictures.
 I see the secondary, I do not see slickenside.

 I decided to take a look at all the samples for sale on Ebay. There is a
 fellow there selling slickenside fragments.   Even with those, I say look
 closer.

 I imagine you have been very busy!  That's a good thing!

 Cheers!

 Jim Wooddell



 On 5/21/2013 8:16 AM, Sergey Vasiliev wrote:

 Hi All,
 Look at the two pictures of the same stone.

 This is a fresh broken side with black shock veins on a very light matrix:
 -  http://sv-meteorites.com/gallery/chelybinsk/02.jpg

 And this side is secondary crust over the shock vein:
 - http://sv-meteorites.com/gallery/chelybinsk/01.jpg

 You can find a lot of interesting things in Chelyabinsk ;-)

 All the best,
 Sergey


 __

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 Meteorite-list mailing list
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Michael Farmer
Chelyabinsk is an incredible meteorite with so many lithologies and variations, 
it is almost unlike any meteorite I have ever seen. You can have 5 pieces side 
by side and swear all are from different meteorite falls. Some pieces are 
hardly recognizable as meteorites.
Many pieces exhibit amazing slickensides and most of the fragmented pieces 
broke along those planes. Don't forget, virtually nothing broke on impact, it 
was all in the massive disruptions in flight that created uncountable fragments 
and individuals. 
The impact-melt material is basically Cat Mountain without the metal. The 
shock-melt pieces with huge glass veins are breathtaking when sliced.
Most oriented pieces are small, though a couple large ones were found. One 
sitting beside me at this moment:)
No meteorite collection will be complete  if it lacks Chelyabinsk, especially 
Binsk Berries. 
Michael Farmer




On May 21, 2013, at 10:36 AM, Sergey Vasiliev vs.petrov...@gmail.com wrote:

 Hi Jim,
 There is a slickensides there, but very difficult to make a picture of
 it because of reflection.
 Best regards,
 Sergey
 
 On Tue, May 21, 2013 at 5:32 PM, Jim Wooddell
 jim.woodd...@suddenlink.net wrote:
 Hi Sergey,
 
 Those are nice pictures.
 I see the secondary, I do not see slickenside.
 
 I decided to take a look at all the samples for sale on Ebay. There is a
 fellow there selling slickenside fragments.   Even with those, I say look
 closer.
 
 I imagine you have been very busy!  That's a good thing!
 
 Cheers!
 
 Jim Wooddell
 
 
 
 On 5/21/2013 8:16 AM, Sergey Vasiliev wrote:
 
 Hi All,
 Look at the two pictures of the same stone.
 
 This is a fresh broken side with black shock veins on a very light matrix:
 -  http://sv-meteorites.com/gallery/chelybinsk/02.jpg
 
 And this side is secondary crust over the shock vein:
 - http://sv-meteorites.com/gallery/chelybinsk/01.jpg
 
 You can find a lot of interesting things in Chelyabinsk ;-)
 
 All the best,
 Sergey
 
 
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Bob King
Hi Sean,
That photo shows it exactly!
Thanks,
Bob

On Tue, May 21, 2013 at 10:24 AM, Sean T. Murray s...@bellsouth.net wrote:
 I've noticed the same thing... I think this is a laterally exposed shock
 vein... sometimes they are crusted over, other times they are pretty fresh,
 so you can see the size of the exposed plane...

 http://www.fallingrocks.com/Collections/Chelyabinsk.htm (4th picture down,
 top left of photo...)

 It's hard to take a picture of because it is so reflective, but it it quite
 a beautiful feature of this fall.

 Sean.

 -Original Message- From: Sergey Vasiliev
 Sent: Tuesday, May 21, 2013 11:16 AM
 To: Michael Mulgrew
 Cc: meteorite list
 Subject: Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?


 Hi All,
 Look at the two pictures of the same stone.

 This is a fresh broken side with black shock veins on a very light matrix:
 -  http://sv-meteorites.com/gallery/chelybinsk/02.jpg

 And this side is secondary crust over the shock vein:
 - http://sv-meteorites.com/gallery/chelybinsk/01.jpg

 You can find a lot of interesting things in Chelyabinsk ;-)

 All the best,
 Sergey

 On Tue, May 21, 2013 at 4:59 PM, Michael Mulgrew mikest...@gmail.com
 wrote:

 Bob,

 My piece is just over 5g, but it was broken off a slightly larger
 piece, probably less than 50g before it broke.

 Michael in so. Cal.

 On Tue, May 21, 2013 at 7:48 AM, Bob King nightsk...@gmail.com wrote:

 Michael and all,
 I forgot to add that even small 2-3g Chelyabinsks show this same
 slick, grey material coating their broken faces. Can slickensides form
 on rocks this small?
 Bob

 On Tue, May 21, 2013 at 9:43 AM, Michael Mulgrew mikest...@gmail.com
 wrote:

 Bob, Jim, List,

 I have a small piece that displays the slickenside in 3 distinct
 locations; it's definitely not secondary fusion crust.  Looking
 forward to hearing more on the subject.

 Michael in so. Cal.

 On Tue, May 21, 2013 at 7:29 AM, Jim Wooddell jimwoodd...@gmail.com
 wrote:


 Hi Bob and all!
 I might be wrong in assuming, but your slickensides sounds like you
 are attempting to describe secondary fusion???

 We have lots of evidence in various meteorites where they broke apart
 for whatever reason at the weak boundaries.  For example, Franconia
 area meteorites (some) break apart from both sides of a metal vein
 leaving three pieces...two chondrite fragments and an H-Metal
 cornflake.
 It's sort of like looking at a bad weld through xray.
 How can you tell?  Look at more and look closer.  A 3D CT sort of scan
 that has become popular with Sutter's Mill or Dr. Agee's research on
 Black Beauty may reveal what you speak of.   Just my thoughts.

 Kind Regards,

 Jim


 On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:
  Hi everyone,
  Many pieces of broken Chelyabinsk specimens display what appears like
  fusion crust over slickensides, but is that what it really is? I've
  talked with Blaine Reed and he thinks we're seeing blackish shock
  veins (planes really) where the meteorite split along a line of
  weakness. He even mentioned a piece he's seen where a large shock 
  vein
  in the matrix leads directly to the broken, dark face. Assuming
  Chelyabinsk shows both slickensides and shock vein planes, how do you
  tell them apart?
  Thanks for your thoughts.
  Bob
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  Meteorite-list mailing list
  Meteorite-list@meteoritecentral.com
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 --
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 jimwoodd...@gmail.com
 928-247-2675
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Sergey Vasiliev
Not really a good focus (try full screen!) but at the end you can see
both: slickensides and crust over it on the smaller surface.

http://www.youtube.com/watch?v=IVnerr2giL0feature=youtu.be

Reagrds,
Sergey

On Tue, May 21, 2013 at 5:43 PM, Michael Farmer m...@meteoriteguy.com wrote:
 Chelyabinsk is an incredible meteorite with so many lithologies and 
 variations, it is almost unlike any meteorite I have ever seen. You can have 
 5 pieces side by side and swear all are from different meteorite falls. Some 
 pieces are hardly recognizable as meteorites.
 Many pieces exhibit amazing slickensides and most of the fragmented pieces 
 broke along those planes. Don't forget, virtually nothing broke on impact, it 
 was all in the massive disruptions in flight that created uncountable 
 fragments and individuals.
 The impact-melt material is basically Cat Mountain without the metal. The 
 shock-melt pieces with huge glass veins are breathtaking when sliced.
 Most oriented pieces are small, though a couple large ones were found. One 
 sitting beside me at this moment:)
 No meteorite collection will be complete  if it lacks Chelyabinsk, especially 
 Binsk Berries.
 Michael Farmer




 On May 21, 2013, at 10:36 AM, Sergey Vasiliev vs.petrov...@gmail.com wrote:

 Hi Jim,
 There is a slickensides there, but very difficult to make a picture of
 it because of reflection.
 Best regards,
 Sergey

 On Tue, May 21, 2013 at 5:32 PM, Jim Wooddell
 jim.woodd...@suddenlink.net wrote:
 Hi Sergey,

 Those are nice pictures.
 I see the secondary, I do not see slickenside.

 I decided to take a look at all the samples for sale on Ebay. There is a
 fellow there selling slickenside fragments.   Even with those, I say look
 closer.

 I imagine you have been very busy!  That's a good thing!

 Cheers!

 Jim Wooddell



 On 5/21/2013 8:16 AM, Sergey Vasiliev wrote:

 Hi All,
 Look at the two pictures of the same stone.

 This is a fresh broken side with black shock veins on a very light matrix:
 -  http://sv-meteorites.com/gallery/chelybinsk/02.jpg

 And this side is secondary crust over the shock vein:
 - http://sv-meteorites.com/gallery/chelybinsk/01.jpg

 You can find a lot of interesting things in Chelyabinsk ;-)

 All the best,
 Sergey


 __

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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Jim Wooddell

Hi Bob and all!

When I think slickenside, I think of a polished surface where something 
rubbed on the surface to polish it.  I don't see this in any of the 
pictures.  My samples do not have thisso I guess I will have to just 
buy some more!!! Very interesting.  What do you guys suppose did this?  
It would not have had anything to do with the break up, I suppose.


Jim


On 5/21/2013 8:48 AM, Bob King wrote:

Hi Sean,
That photo shows it exactly!
Thanks,
Bob



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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Jim Wooddell

Hi Jim Baxter,
And, that is what I am not seeing.  I'am going to be a very hard sell on 
the term slickensides until I see something that scientifically supports 
it and why it is there.  Do the threads actually appear and are they 
threads??
In my mind, the coming apart part would not create a slickenside (cool 
state) where as the coming together with great pressure and time would.  
Just thinking out loud, not qualified to say one way or the other!
I also see where this appearance is shown lower in topography in it's 
area which, to me, would be odd for slickenside.


Cheers!

Jim Wooddell




On 5/21/2013 9:18 AM, Jim Baxter wrote:
Slickensides are polished surfaces caused by lateral movement along a 
fault plane. In hand specimens they feel rough when you rub your 
finger in one direction and smooth when you rub it in the other. Not 
sure that test would be feasible on the size specimens most of us own. 
In theory if the fault planes represent planes of weakness along which 
breaks occur then you could be seeing both things - slickensides that 
formed by lateral movement along the shock plane when the stone fractured.


Jim Baxter


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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Michael Farmer
Jim, there are shock veins and slickensides. They are not the same thing. They 
are result of shock but not melting like the full melt veins are.
I have hundreds of pieces with slickensides. I am traveling so I can't show 
photos.
Perhaps later.
Michael Farmer

Sent from my iPhone

On May 21, 2013, at 12:19 PM, Jim Wooddell jim.woodd...@suddenlink.net wrote:

 Hi Jim Baxter,
 And, that is what I am not seeing.  I'am going to be a very hard sell on the 
 term slickensides until I see something that scientifically supports it and 
 why it is there.  Do the threads actually appear and are they threads??
 In my mind, the coming apart part would not create a slickenside (cool state) 
 where as the coming together with great pressure and time would.  Just 
 thinking out loud, not qualified to say one way or the other!
 I also see where this appearance is shown lower in topography in it's area 
 which, to me, would be odd for slickenside.
 
 Cheers!
 
 Jim Wooddell
 
 
 
 
 On 5/21/2013 9:18 AM, Jim Baxter wrote:
 Slickensides are polished surfaces caused by lateral movement along a fault 
 plane. In hand specimens they feel rough when you rub your finger in one 
 direction and smooth when you rub it in the other. Not sure that test would 
 be feasible on the size specimens most of us own. In theory if the fault 
 planes represent planes of weakness along which breaks occur then you could 
 be seeing both things - slickensides that formed by lateral movement along 
 the shock plane when the stone fractured.
 
 Jim Baxter
 
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Graham Ensor
hi Bobto my knowledge the slickensides most likely form in the
original asteroidal body in space (large collision or impact) and then
are left in the small stones after the atmospheric breakup.

Graham

On Tue, May 21, 2013 at 3:48 PM, Bob King nightsk...@gmail.com wrote:
 Michael and all,
 I forgot to add that even small 2-3g Chelyabinsks show this same
 slick, grey material coating their broken faces. Can slickensides form
 on rocks this small?
 Bob

 On Tue, May 21, 2013 at 9:43 AM, Michael Mulgrew mikest...@gmail.com wrote:
 Bob, Jim, List,

 I have a small piece that displays the slickenside in 3 distinct
 locations; it's definitely not secondary fusion crust.  Looking
 forward to hearing more on the subject.

 Michael in so. Cal.

 On Tue, May 21, 2013 at 7:29 AM, Jim Wooddell jimwoodd...@gmail.com wrote:

 Hi Bob and all!
 I might be wrong in assuming, but your slickensides sounds like you
 are attempting to describe secondary fusion???

 We have lots of evidence in various meteorites where they broke apart
 for whatever reason at the weak boundaries.  For example, Franconia
 area meteorites (some) break apart from both sides of a metal vein
 leaving three pieces...two chondrite fragments and an H-Metal
 cornflake.
 It's sort of like looking at a bad weld through xray.
 How can you tell?  Look at more and look closer.  A 3D CT sort of scan
 that has become popular with Sutter's Mill or Dr. Agee's research on
 Black Beauty may reveal what you speak of.   Just my thoughts.

 Kind Regards,

 Jim


 On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:
  Hi everyone,
  Many pieces of broken Chelyabinsk specimens display what appears like
  fusion crust over slickensides, but is that what it really is? I've
  talked with Blaine Reed and he thinks we're seeing blackish shock
  veins (planes really) where the meteorite split along a line of
  weakness. He even mentioned a piece he's seen where a large shock vein
  in the matrix leads directly to the broken, dark face. Assuming
  Chelyabinsk shows both slickensides and shock vein planes, how do you
  tell them apart?
  Thanks for your thoughts.
  Bob
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Jim Wooddell
Welp, I just need to see one up close. But in the mean time here is a 
paper on the subject that may be of interest...


http://adsabs.harvard.edu/full/1966Metic...3...31D

Jim


On 5/21/2013 10:26 AM, Michael Farmer wrote:

Jim, there are shock veins and slickensides. They are not the same thing. They 
are result of shock but not melting like the full melt veins are.
I have hundreds of pieces with slickensides. I am traveling so I can't show 
photos.
Perhaps later.
Michael Farmer

Sent from my iPhone

On May 21, 2013, at 12:19 PM, Jim Wooddell jim.woodd...@suddenlink.net wrote:


Hi Jim Baxter,
And, that is what I am not seeing.  I'am going to be a very hard sell on the 
term slickensides until I see something that scientifically supports it and why 
it is there.  Do the threads actually appear and are they threads??
In my mind, the coming apart part would not create a slickenside (cool state) 
where as the coming together with great pressure and time would.  Just thinking 
out loud, not qualified to say one way or the other!
I also see where this appearance is shown lower in topography in it's area 
which, to me, would be odd for slickenside.

Cheers!

Jim Wooddell




On 5/21/2013 9:18 AM, Jim Baxter wrote:

Slickensides are polished surfaces caused by lateral movement along a fault 
plane. In hand specimens they feel rough when you rub your finger in one 
direction and smooth when you rub it in the other. Not sure that test would be 
feasible on the size specimens most of us own. In theory if the fault planes 
represent planes of weakness along which breaks occur then you could be seeing 
both things - slickensides that formed by lateral movement along the shock 
plane when the stone fractured.

Jim Baxter

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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Anne Black

Does this help Jim?

http://www.impactika.com/CH-126slick.jpg

To me, slickensides look almost like streaks, and yes, shiny.
Like my cat scratched it!  ;-)


Anne M. Black
www.IMPACTIKA.com
impact...@aol.com


-Original Message-
From: Jim Wooddell jim.woodd...@suddenlink.net
To: meteorite-list meteorite-list@meteoritecentral.com
Sent: Tue, May 21, 2013 2:08 pm
Subject: Re: [meteorite-list] Chelyabinsk - slickensides or shock 
planes?



Welp, I just need to see one up close. But in the mean time here is a
paper on the subject that may be of interest...

http://adsabs.harvard.edu/full/1966Metic...3...31D

Jim


On 5/21/2013 10:26 AM, Michael Farmer wrote:
Jim, there are shock veins and slickensides. They are not the same 

thing. They
are result of shock but not melting like the full melt veins are.
I have hundreds of pieces with slickensides. I am traveling so I 

can't show
photos.

Perhaps later.
Michael Farmer

Sent from my iPhone

On May 21, 2013, at 12:19 PM, Jim Wooddell 

jim.woodd...@suddenlink.net
wrote:



Hi Jim Baxter,
And, that is what I am not seeing.  I'am going to be a very hard 

sell on the
term slickensides until I see something that scientifically supports it 
and why

it is there.  Do the threads actually appear and are they threads??
In my mind, the coming apart part would not create a slickenside 

(cool state)
where as the coming together with great pressure and time would.  Just 
thinking

out loud, not qualified to say one way or the other!
I also see where this appearance is shown lower in topography in 

it's area
which, to me, would be odd for slickenside.


Cheers!

Jim Wooddell




On 5/21/2013 9:18 AM, Jim Baxter wrote:
Slickensides are polished surfaces caused by lateral movement along 

a fault
plane. In hand specimens they feel rough when you rub your finger in 
one
direction and smooth when you rub it in the other. Not sure that test 
would be
feasible on the size specimens most of us own. In theory if the fault 
planes
represent planes of weakness along which breaks occur then you could be 
seeing
both things - slickensides that formed by lateral movement along the 
shock plane

when the stone fractured.


Jim Baxter

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05/21/13






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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Michael Farmer
I found a very nice Chelyabinsk while running to the truck after finding a 1.2 
kg stone. I saw it flash in the sun, a half stone with silver slickenside up, 
it was like a mirror.
Michael Farmer

Sent from my iPhone

On May 21, 2013, at 4:36 PM, Bernd V. Pauli bernd.pa...@paulinet.de wrote:

 Hello All,
 
 We had a similar discussion many, many years ago
 (September 2001). Here's a short overview of our results:
 
 Summary:
 
 - broken surface is covered with glossy striations
 - slickensides are identified by shiny mirror like surfaces
  on an otherwise rough rock
 
 - they are the product of faulting in a rock body (as the crust
  shifts, even slightly, the roughness of the rock tends to smooth)
 
 - slickensides are formed from the movement of rocks relative to each other
  along fracture planes in fault zones
 
 - rub your finger along the grooves which make up the slickensides:
 
 * they feel rough when you move your finger in the direction opposite
  to which the adjacent rock moved to form the slickensides
 
 + they feel smooth when you rub in the same direction the adjacent rock
  moved because it sheared off any microscopic projections or rough
  edges as it moved
 
 = Not found in shatter cones!
 
 - slickensides are formed when opposite sides of rock faults
  move in different directions
 
 - extreme pressure generates frictional heat as the rock faces are forced
  past each other partially melting a thin veneer of rock at the interface
  (result: smoothing of rough edges and a polished looking surface)
 
 - they are not formed by explosive breakup in the earth's atmosphere
  (in such a breakup pieces would be flying apart from each other
  whereas in slickensides the opposite is happening: the rock faces
  are being forced against each other) but: see below **
 
 - possible formation scenario: an impact event in space results in
  movement of two adjacent parts of  the stony meteorite relative to
  each other along a preexisting fracture plane thus creating grooves
 
 - slickensides are polished, grooved surfaces that occur along shear planes
 
 - slickensides form along internal shear planes as opposite parts
  move past one another
 
 - opposite parts rub against each other, their surfaces become smoothed,
  lineated, and grooved
 
 - slickensides are formed when two planar sides grind past each other
 
 - slickensides can be created at the moment of breakup (not by the explosive
  part of this breakup but rather when two parts of the meteorite grind past
  each other along a pre-existing fracture – so-called shear rupturing) **
 
 and here are some of the listees that participated in the discussion:
 
 Charlie Devine (started the discussion), Eric Olson, Robert Verish,
 ... to name a few.
 
 Cheers,
 
 Bernd
 
 
 
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Malvin Bishop Jr
This is what I was referring to in my previous email regarding one of my 
Chelyabinsk specimens showing a feature where it appears

to be fractured along a weakened shock vein/point where melt had
filled the vein before the actual splitting apart.  The melt is
very evident.  Am I thinking correctly on this Mike, Sean, or whomever
wishes to respond?

http://s1300.photobucket.com/user/N68830/media/Chelyabinsk_fragment_zps1a7dfce6.jpg.html

Mal


On 5/21/2013 11:48 AM, Bob King wrote:

Hi Sean,
That photo shows it exactly!
Thanks,
Bob

On Tue, May 21, 2013 at 10:24 AM, Sean T. Murray s...@bellsouth.net wrote:

I've noticed the same thing... I think this is a laterally exposed shock
vein... sometimes they are crusted over, other times they are pretty fresh,
so you can see the size of the exposed plane...

http://www.fallingrocks.com/Collections/Chelyabinsk.htm (4th picture down,
top left of photo...)

It's hard to take a picture of because it is so reflective, but it it quite
a beautiful feature of this fall.

Sean.

-Original Message- From: Sergey Vasiliev
Sent: Tuesday, May 21, 2013 11:16 AM
To: Michael Mulgrew
Cc: meteorite list
Subject: Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?


Hi All,
Look at the two pictures of the same stone.

This is a fresh broken side with black shock veins on a very light matrix:
-  http://sv-meteorites.com/gallery/chelybinsk/02.jpg

And this side is secondary crust over the shock vein:
- http://sv-meteorites.com/gallery/chelybinsk/01.jpg

You can find a lot of interesting things in Chelyabinsk ;-)

All the best,
Sergey

On Tue, May 21, 2013 at 4:59 PM, Michael Mulgrew mikest...@gmail.com
wrote:


Bob,

My piece is just over 5g, but it was broken off a slightly larger
piece, probably less than 50g before it broke.

Michael in so. Cal.

On Tue, May 21, 2013 at 7:48 AM, Bob King nightsk...@gmail.com wrote:


Michael and all,
I forgot to add that even small 2-3g Chelyabinsks show this same
slick, grey material coating their broken faces. Can slickensides form
on rocks this small?
Bob

On Tue, May 21, 2013 at 9:43 AM, Michael Mulgrew mikest...@gmail.com
wrote:


Bob, Jim, List,

I have a small piece that displays the slickenside in 3 distinct
locations; it's definitely not secondary fusion crust.  Looking
forward to hearing more on the subject.

Michael in so. Cal.

On Tue, May 21, 2013 at 7:29 AM, Jim Wooddell jimwoodd...@gmail.com
wrote:



Hi Bob and all!
I might be wrong in assuming, but your slickensides sounds like you
are attempting to describe secondary fusion???

We have lots of evidence in various meteorites where they broke apart
for whatever reason at the weak boundaries.  For example, Franconia
area meteorites (some) break apart from both sides of a metal vein
leaving three pieces...two chondrite fragments and an H-Metal
cornflake.
It's sort of like looking at a bad weld through xray.
How can you tell?  Look at more and look closer.  A 3D CT sort of scan
that has become popular with Sutter's Mill or Dr. Agee's research on
Black Beauty may reveal what you speak of.   Just my thoughts.

Kind Regards,

Jim


On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com wrote:

Hi everyone,
Many pieces of broken Chelyabinsk specimens display what appears like
fusion crust over slickensides, but is that what it really is? I've
talked with Blaine Reed and he thinks we're seeing blackish shock
veins (planes really) where the meteorite split along a line of
weakness. He even mentioned a piece he's seen where a large shock 
vein
in the matrix leads directly to the broken, dark face. Assuming
Chelyabinsk shows both slickensides and shock vein planes, how do you
tell them apart?
Thanks for your thoughts.
Bob
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Jim Wooddell

Hi Bernd!

Doesn't sound like that discussion came to any conclusion. I think there 
was one in 2003 too!


I think this discussion has been going on since prior to 1966, ref the 
abstract link I posted.
I do see striations and typically the slickensides I am familiar with 
are typically larger, not tiny parts of very small rocks. Hundreds of 
pictures of it on the web.
I'd really like to see a scientific explanation for them in meteorites 
as very small parts of small rocks as they are being defined. Sort of 
looking around for an explanation and haven't found anything at this 
time. The ones in Anne's pictures, for example, are not part of an 
individual clast that could have been a bigger rock that had 
slickensides and you can clearly see breccias suggesting that feature 
happened after things came together. I think I also see a contiguous 
border, not strings that are continuous which, to me, would indicate it 
part of something bigger.
Then how to explain a weak boundary that just happens to contain 
slickensides considering how these boundaries were formed in the first 
place! I love it!



Jim


On 5/21/2013 2:36 PM, Bernd V. Pauli wrote:

Hello All,

We had a similar discussion many, many years ago
(September 2001). Here's a short overview of our results:

Summary:

- broken surface is covered with glossy striations
- slickensides are identified by shiny mirror like surfaces
   on an otherwise rough rock

- they are the product of faulting in a rock body (as the crust
   shifts, even slightly, the roughness of the rock tends to smooth)

- slickensides are formed from the movement of rocks relative to each other
   along fracture planes in fault zones

- rub your finger along the grooves which make up the slickensides:

* they feel rough when you move your finger in the direction opposite
   to which the adjacent rock moved to form the slickensides

+ they feel smooth when you rub in the same direction the adjacent rock
   moved because it sheared off any microscopic projections or rough
   edges as it moved

  = Not found in shatter cones!

- slickensides are formed when opposite sides of rock faults
   move in different directions

- extreme pressure generates frictional heat as the rock faces are forced
   past each other partially melting a thin veneer of rock at the interface

   (result: smoothing of rough edges and a polished looking surface)

- they are not formed by explosive breakup in the earth's atmosphere
   (in such a breakup pieces would be flying apart from each other
   whereas in slickensides the opposite is happening: the rock faces
   are being forced against each other) but: see below **

- possible formation scenario: an impact event in space results in
   movement of two adjacent parts of  the stony meteorite relative to
   each other along a preexisting fracture plane thus creating grooves

- slickensides are polished, grooved surfaces that occur along shear planes

- slickensides form along internal shear planes as opposite parts
   move past one another

- opposite parts rub against each other, their surfaces become smoothed,
   lineated, and grooved

- slickensides are formed when two planar sides grind past each other

- slickensides can be created at the moment of breakup (not by the explosive
   part of this breakup but rather when two parts of the meteorite grind past
   each other along a pre-  existing fracture – so-called shear rupturing) 
**

and here are some of the listees that participated in the discussion:

Charlie Devine (started the discussion), Eric Olson, Robert Verish,
... to name a few.

Cheers,

Bernd



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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Malvin Bishop Jr


Thank you, Anne, I was pretty sure I was correct in my opinion on this, 
but verification by other esteemed list members NEVER hurts!


Copying my photo?... no harm, no foul. Taking liberties sometimes is a 
good thing. :-)


Thanks again -
Mal


On 5/21/2013 6:10 PM, Anne Black wrote:

Yes, Mal,
I believe that what you are looking at on this picture is a fracture
along a shock vein, it is patchy, it is not as shiny and it is not
fibrous looking like a slickenside.
I took the liberty of copying your picture and putting side by side with
mine, I hope you don't mind.
Look at the difference.


Anne M. Black
www.IMPACTIKA.com
impact...@aol.com


-Original Message-
From: Malvin Bishop Jr magbi...@lowcountry.com
To: meteorite-list meteorite-list@meteoritecentral.com
Sent: Tue, May 21, 2013 3:51 pm
Subject: Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?


This is what I was referring to in my previous email regarding one of my
Chelyabinsk specimens showing a feature where it appears
to be fractured along a weakened shock vein/point where melt had
filled the vein before the actual splitting apart.  The melt is
very evident.  Am I thinking correctly on this Mike, Sean, or whomever
wishes to respond?

http://s1300.photobucket.com/user/N68830/media/Chelyabinsk_fragment_zps1a7dfce6.jpg.html


Mal


On 5/21/2013 11:48 AM, Bob King wrote:

Hi Sean,
That photo shows it exactly!
Thanks,
Bob

On Tue, May 21, 2013 at 10:24 AM, Sean T. Murray s...@bellsouth.net

wrote:

I've noticed the same thing... I think this is a laterally exposed

shock

vein... sometimes they are crusted over, other times they are pretty

fresh,

so you can see the size of the exposed plane...

http://www.fallingrocks.com/Collections/Chelyabinsk.htm (4th picture

down,

top left of photo...)

It's hard to take a picture of because it is so reflective, but it

it quite

a beautiful feature of this fall.

Sean.

-Original Message- From: Sergey Vasiliev
Sent: Tuesday, May 21, 2013 11:16 AM
To: Michael Mulgrew
Cc: meteorite list
Subject: Re: [meteorite-list] Chelyabinsk - slickensides or shock

planes?



Hi All,
Look at the two pictures of the same stone.

This is a fresh broken side with black shock veins on a very light

matrix:

-  http://sv-meteorites.com/gallery/chelybinsk/02.jpg

And this side is secondary crust over the shock vein:
- http://sv-meteorites.com/gallery/chelybinsk/01.jpg

You can find a lot of interesting things in Chelyabinsk ;-)

All the best,
Sergey

On Tue, May 21, 2013 at 4:59 PM, Michael Mulgrew

mikest...@gmail.com

wrote:


Bob,

My piece is just over 5g, but it was broken off a slightly larger
piece, probably less than 50g before it broke.

Michael in so. Cal.

On Tue, May 21, 2013 at 7:48 AM, Bob King nightsk...@gmail.com

wrote:


Michael and all,
I forgot to add that even small 2-3g Chelyabinsks show this same
slick, grey material coating their broken faces. Can slickensides

form

on rocks this small?
Bob

On Tue, May 21, 2013 at 9:43 AM, Michael Mulgrew

mikest...@gmail.com

wrote:


Bob, Jim, List,

I have a small piece that displays the slickenside in 3 distinct
locations; it's definitely not secondary fusion crust.  Looking
forward to hearing more on the subject.

Michael in so. Cal.

On Tue, May 21, 2013 at 7:29 AM, Jim Wooddell

jimwoodd...@gmail.com

wrote:



Hi Bob and all!
I might be wrong in assuming, but your slickensides sounds like

you

are attempting to describe secondary fusion???

We have lots of evidence in various meteorites where they broke

apart

for whatever reason at the weak boundaries.  For example,

Franconia

area meteorites (some) break apart from both sides of a metal

vein

leaving three pieces...two chondrite fragments and an H-Metal
cornflake.
It's sort of like looking at a bad weld through xray.
How can you tell?  Look at more and look closer.  A 3D CT sort

of scan

that has become popular with Sutter's Mill or Dr. Agee's

research on

Black Beauty may reveal what you speak of.   Just my thoughts.

Kind Regards,

Jim


On Tue, May 21, 2013 at 7:06 AM, Bob King nightsk...@gmail.com

wrote:

Hi everyone,
Many pieces of broken Chelyabinsk specimens display what

appears like

fusion crust over slickensides, but is that what it really is?

I've

talked with Blaine Reed and he thinks we're seeing blackish

shock

veins (planes really) where the meteorite split along a line of
weakness. He even mentioned a piece he's seen where a large

shock 

vein
in the matrix leads directly to the broken, dark face. Assuming
Chelyabinsk shows both slickensides and shock vein planes, how

do you

tell them apart?
Thanks for your thoughts.
Bob
__

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Meteorite-list mailing list
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Richard Montgomery

Bernd, perfect summary. Thanks.


- Original Message - 
From: Bernd V. Pauli bernd.pa...@paulinet.de

To: meteorite-list@meteoritecentral.com
Sent: Tuesday, May 21, 2013 2:36 PM
Subject: [meteorite-list] Chelyabinsk - slickensides or shock planes?


Hello All,

We had a similar discussion many, many years ago
(September 2001). Here's a short overview of our results:

Summary:

- broken surface is covered with glossy striations
- slickensides are identified by shiny mirror like surfaces
 on an otherwise rough rock

- they are the product of faulting in a rock body (as the crust
 shifts, even slightly, the roughness of the rock tends to smooth)

- slickensides are formed from the movement of rocks relative to each other
 along fracture planes in fault zones

- rub your finger along the grooves which make up the slickensides:

* they feel rough when you move your finger in the direction opposite
 to which the adjacent rock moved to form the slickensides

+ they feel smooth when you rub in the same direction the adjacent rock
 moved because it sheared off any microscopic projections or rough
 edges as it moved

= Not found in shatter cones!

- slickensides are formed when opposite sides of rock faults
 move in different directions

- extreme pressure generates frictional heat as the rock faces are forced
 past each other partially melting a thin veneer of rock at the interface
 (result: smoothing of rough edges and a polished looking surface)

- they are not formed by explosive breakup in the earth's atmosphere
 (in such a breakup pieces would be flying apart from each other
 whereas in slickensides the opposite is happening: the rock faces
 are being forced against each other) but: see below **

- possible formation scenario: an impact event in space results in
 movement of two adjacent parts of  the stony meteorite relative to
 each other along a preexisting fracture plane thus creating grooves

- slickensides are polished, grooved surfaces that occur along shear planes

- slickensides form along internal shear planes as opposite parts
 move past one another

- opposite parts rub against each other, their surfaces become smoothed,
 lineated, and grooved

- slickensides are formed when two planar sides grind past each other

- slickensides can be created at the moment of breakup (not by the explosive
 part of this breakup but rather when two parts of the meteorite grind past
 each other along a pre- existing fracture - so-called shear rupturing) **

and here are some of the listees that participated in the discussion:

Charlie Devine (started the discussion), Eric Olson, Robert Verish,
... to name a few.

Cheers,

Bernd



__

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Meteorite-list mailing list
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Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

2013-05-21 Thread Count Deiro
Thank you, Bernd. You are a river to your fellow enthusiasts.
Guido

-Original Message-
From: Richard Montgomery rickm...@earthlink.net
Sent: May 21, 2013 5:21 PM
To: Bernd V. Pauli bernd.pa...@paulinet.de, 
meteorite-list@meteoritecentral.com
Subject: Re: [meteorite-list] Chelyabinsk - slickensides or shock planes?

Bernd, perfect summary. Thanks.


- Original Message - 
From: Bernd V. Pauli bernd.pa...@paulinet.de
To: meteorite-list@meteoritecentral.com
Sent: Tuesday, May 21, 2013 2:36 PM
Subject: [meteorite-list] Chelyabinsk - slickensides or shock planes?


Hello All,

We had a similar discussion many, many years ago
(September 2001). Here's a short overview of our results:

Summary:

- broken surface is covered with glossy striations
- slickensides are identified by shiny mirror like surfaces
  on an otherwise rough rock

- they are the product of faulting in a rock body (as the crust
  shifts, even slightly, the roughness of the rock tends to smooth)

- slickensides are formed from the movement of rocks relative to each other
  along fracture planes in fault zones

- rub your finger along the grooves which make up the slickensides:

* they feel rough when you move your finger in the direction opposite
  to which the adjacent rock moved to form the slickensides

+ they feel smooth when you rub in the same direction the adjacent rock
  moved because it sheared off any microscopic projections or rough
  edges as it moved

 = Not found in shatter cones!

- slickensides are formed when opposite sides of rock faults
  move in different directions

- extreme pressure generates frictional heat as the rock faces are forced
  past each other partially melting a thin veneer of rock at the interface
  (result: smoothing of rough edges and a polished looking surface)

- they are not formed by explosive breakup in the earth's atmosphere
  (in such a breakup pieces would be flying apart from each other
  whereas in slickensides the opposite is happening: the rock faces
  are being forced against each other) but: see below **

- possible formation scenario: an impact event in space results in
  movement of two adjacent parts of  the stony meteorite relative to
  each other along a preexisting fracture plane thus creating grooves

- slickensides are polished, grooved surfaces that occur along shear planes

- slickensides form along internal shear planes as opposite parts
  move past one another

- opposite parts rub against each other, their surfaces become smoothed,
  lineated, and grooved

- slickensides are formed when two planar sides grind past each other

- slickensides can be created at the moment of breakup (not by the explosive
  part of this breakup but rather when two parts of the meteorite grind past
  each other along a pre- existing fracture - so-called shear rupturing) **

and here are some of the listees that participated in the discussion:

Charlie Devine (started the discussion), Eric Olson, Robert Verish,
... to name a few.

Cheers,

Bernd



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