I also agree with Kim about the bulk of the IP response coming form the 
propylitic zone.  However, I would like to see a few more examples of frequency 
domain IP done over some porphyry systems.  I like the thought of being able to 
discern grainsize and/or mineral species.  

 

Cheers

Barry

 

From: SEGMIN <[email protected]> On Behalf Of Kim Frankcombe via 
SEGMIN
Sent: Sunday, 24 January 2021 9:46 AM
To: [email protected]
Cc: Kim Frankcombe <[email protected]>
Subject: Re: [SEGMIN] Question for porphyry explorers

 

Sergio

It also depends on the integration window you use for chargeability, the 
frequency of your Tx or more correctly the length of the on time and a bunch of 
other geology factors. I don't stress too much about absolute values although I 
know plenty who do. If they want to walk away from an anomaly that is >2 times 
background it just leaves more for the rest of us to find. Having said all that 
typical anomalies are usually in the 2 - 4 x background level but I still 
wouldn't walk from something bigger, particularly if you can make a 
geologically cohearent story around it. The survey obviously has to be big 
enough to know what background is and for porphyries too many surveys never get 
out of alteration.

The bulk of the IP response is coming from the propylitic zone not the primary 
mineralisation which while often chargeable is usually drowned out by the 
propylitic response. i.e you are looking for alteration more so than the ore.

Cheers
Kim





On 24/1/21 4:49 am, S E Geoscience and Exploration via SEGMIN wrote:

Dear all,

 

Question for all those porphyry explorers: What chargeability value would you 
consider to be already anomalous for primary mineralization?

 

Of course this value does not only depend on Sulphide-%, but also on its type 
of occurrence.

 

Thank you in advance for the discussion,

 

Regards


-- 

Sergio Espinosa, Ph.D., P.Geo

Director, Geophysics

S E Geoscience & Exploration





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-- 

Kim Frankcombe

Senior Consulting Geophysicist

 

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