Awang ,  Vicky

Setelah mengikuti diskusi Anda anda , saya
bertambah yakin betapa pentingnya kita mengikuti  Sandi Startigrafi
.
Sehingga tidak akan pabaliut antara Kikim Tuff , Lahat , Lemat ,
Talang  Akar . Formasi Vulkanik Jatibarang dst..

Mungkin
Awang dalam posisi yang tepat untuk meng"arah"kan para operator
ini.

Si Abah




> 

   Pako Rovicky,
>  
> Data yvang
berhubungan dengan masalahLemat-grite wash dari sumur
>penelitian
itu saya publikasi secara terbatas pada pertemuan Sumatra
>
Stratigraphy Workshop (SSW) di Duri pada September 2005. Presentasi2
dalam
> pertemuan ini kemudian dimintakan makalah lengkapnya dan
dibukukan di
> bawah komando Pak Yarmanto (Chevron) dan dilepas ke
publik pada PIT IAGI
> yang lalu (2008) di Bandung -ini adalah
tradisi workshop stratigrafi,
> seperti juga workshop stratigrafi
Jawa sebelumnya. Sayang, saya tak sempat
> membuat makalah
lengkapnya untuk publikasi SSW -meskipun telah ditagih
> beberapa
kali oleh Pak Yarmanto - maaf Pak Yarmanto, di buku itu saya
>
hanya memberikan abstraknya dan di ex Panitia Workshop ada bahan
>
presentasinya.
>  
> Sumur tersebut sampai sekarang
masih berada di blok aktif. Datanya (raw
> data &
interpretation) bila sudah terbuka kalau mengikuti aturan data
>
terbuka sejak data diperoleh, bisa diakses. Hanya untuk mendapatkannya
> mesti menghubungi Operator terkait (karena blok aktif) secara
business to
> business di bawah fasilitasi dan pengawasan
BPMIGAS.
>  
> Di bawah ada abstrak makalah
tersebut.
>  
> Salam,
> awang
>
 
> INDONESIAN ASSOCIATION OF GEOLOGISTS – RIAU
CHAPTER
> SUMATRA STRATIGRAPHY WORKSHOP
> DURI, RIAU 12
– 13 SEPTEMBER 2005
>  
> “GRANITE
WASH” OF LEMAT FORMATION OR IN-SITU GRANITE OF BASEMENT ? : THE
> PROBLEM OF SOUTH SUMATRA STRATIGRAPHY AND NEW APPROACHES FOR ITS
SOLUTION
>  
> Awang Harun Satyana
>
 
> (BPMIGAS - Badan Pelaksana Kegiatan Usaha Hulu Minyak dan
Gas Bumi)
>  
> Basement of the South Sumatra Basin
is a complex of Mesozoic igneous rocks
> and of Paleozoic and
Mesozoic metamorphics and carbonates intruded by
> Mesozoic
igneous rocks. Structural relationships of rocks composing of the
> basement are complex as can be seen at outcrops in the Barisan
Mountains.
> This complexity extends into the subcrops of the
South Sumatra Basin.
>  
> In some places, strata of
Late Cretaceous to Early Eocene are also grouped
> as the
basement. This has caused a problem of identifying the basement.
>
The problem is more complicated when the strata composed of 
“granite
> wash” – a unit of re-deposited
granite in the lower part Lemat Formation
> (Early Eocene-mid
Oligocene) overlie the basement which also composed of
> in-situ
granite.
>  
> ”Granite wash” can be
difficult to distinguish from in-situ granite, even
> in outcrop,
let alone down hole. Additional complication by alteration may
>
obscure original fabric of the rock. Several approaches have been used
to
> determine whether or not the upper parts of several granite
plutons have
> been eroded and re-deposited as “granite
wash”. The approaches include :
> petrography of granite,
absolute dating of granite and its veins,  and
>
paleomagnetics of granite.
>  
> Petrographic
analysis can reveal sedimentary origin of “granite wash”
like
> the presence of fine grained matrix material or showing
hydrothermal
> origin of in-situ granite. Absolute dating of veins
is done to constraint
> the age of fabric present at the time
of  veining. If the rock is
> considered to be re-deposited,
the re-deposition would have to be older
> than the vein
formation. The vein age would provide a minimum age for
>
granite/”granite wash” fabric. As for paleomagnetics, it is
hypothesized
> that in-situ granite should give a relatively
strong uni-directional
> signal of paleomagnetics whereas granite
broken into constituent sand
> grains and then randomly rearranged
in a sedimentary rock is less likely
> to give a uni-directional
signal.
>  
> Some wells in South Sumatra Basin
penetrated either “granite wash” of
> Lemat Formation
or in-situ granite of the Basement, and/or both of them.
>
Identification of top Basement is problematic when it is not known
> precisely which granite constitutes the lithology. This study shows
how
> the above approaches were applied to solve the
problem.  
> 
> --- On Tue, 1/20/09, Rovicky Dwi
Putrohari <rovi...@gmail.com> wrote:
> 
>
From:
Rovicky Dwi Putrohari <rovi...@gmail.com>
> Subject: Re:
[iagi-net-l] Re: [Forum-HAGI] [iagi-net-l] Talangakar dan
>
Lemat
> To: iagi-net@iagi.or.id
> Date: Tuesday, January
20, 2009, 1:13 PM
> 
> On Tue, Jan 20, 2009 at 1:55 PM,
Awang Satyana <awangsaty...@yahoo.com>
> wrote:
>>
>> Saya punya data sebuah sumur yang menembus baik
Talang
>> Akar-Lemat-granite
> wash-dan insitu granite
(fresh granite) Basement - dan dengan jelas bisa
> didefinisikan
batas-batas batuan itu, kebetulan sumur ini adalah sumur
>
penelitian untuk memahami masalah granite wash dan endapan pre-TAF,
> sehingga
> punya analisis yang lengkap baik petrografinya,
umur absolutnya, bahkan
> geomagnetismenya.
>>
>> salam,
>> awang
> 
> Pak Awang,
> Apakah ada public data (publikasi) sehubungan dengan sumur
> "penelitian" diatas ?
> Sangat menarik tentunya.
Bisa menjadi kunci untuk membuka pintu2
> gudang minyak di sumatra
selatan.
> 
> RDP
> "masih mimpi open file
data policy"
> 
>
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