Untuk orang non Indonesia (termasuk Malaysia) pulau Kalimantan disebutnya
Borneo island yang terdiri dari Kalimantan (Indonesian Borneo), Sarawak,
Sabah (North Borneo) dan Brunei. Nah begitu!
----- Original Message -----
From: "PUTROHARI Rovicky" <[EMAIL PROTECTED]>
To: <[EMAIL PROTECTED]>
Sent: Tuesday, March 18, 2003 5:44 PM
Subject: [iagi-net-l] Tertiary carbonates on the Mangkalihat Peninsula,
> Di paper ini sebelnya cuman satu ...:-(
> kenapa kok disebut Borneo seeh ?
>
> rdp
> "lebih sebel lagi cuman boleh baca abstract ... pelit loe !! ;-("
> ====
> Marine and Petroleum Geology
> Volume 19, Issue 7 , August 2002, Pages 873-900
>
> Sedimentology and diagenesis of Tertiary carbonates on the Mangkalihat
> Peninsula, Borneo: implications for subsurface reservoir quality
>
> Moyra E. J. Wilson, , a and Martin J. Evans, b, 1
>
> a Department of Geological Sciences, University of Durham, South Road,
> Durham DH1 3LE, UK
> b Maersk Oil, 50 Esplanaden, DK-1263, Copenhagen K, Denmark
>
> Received 27 November 2000; revised 13 July 2002; accepted 22 July 2002.
> ; Available online 11 December 2002.
>
>
> Abstract
> Combined field and laboratory studies of surface exposures on the
> Mangkalihat Peninsula, Borneo, provide new constraints on the
> chronostratigraphy, sedimentology and diagenesis of Tertiary carbonate
> deposits. The reservoir characteristics of carbonate facies are described,
> providing an analogue model for carbonate reservoirs in the subsurface of
> this region.
>
> A mixed carbonate-siliciclastic shelf with intervening, probably
> fault-bounded, deeper water areas developed on the eastern part of the
> Mangkalihat Peninsula in the Late Eocene to Oligocene. During the
> Oligo-Miocene shallow-water platform carbonates accumulated over much of
> the area of the Mangkalihat Peninsula. This platform had a steep,
> reef-rimmed or possibly locally faulted northern margin, where high-energy
> conditions prevailed and marine cements were pervasive. In contrast, the
> platform interior was a low energy area, affected by leaching of
> aragonitic bioclasts. The best reservoir quality on the platform occurs in
> moderate energy grainstones and packstones, tens to hundreds of metres
> towards the platform interior from the platform margin, where a
> combination of primary intergranular and secondary mouldic porosity
> results in good porosity and permeability.
>
> Author Keywords: Tertiary; Carbonate platform; Reservoir; Diagenesis;
> Sedimentology; Facies; Indonesia
>
>
> 1 Present address: Anadarko Algeria Company LLC, P.O. Box 576, The Atrium,
> 1 Harefield Road, Uxbridge, Middlesex UB8 1YH, UK.
>
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Komisi Sedimentologi (FOSI) : F. Hasan Sidi([EMAIL PROTECTED])-http://fosi.iagi.or.id
Komisi SDM/Pendidikan : Edy Sunardi([EMAIL PROTECTED])
Komisi Karst : Hanang Samodra([EMAIL PROTECTED])
Komisi Sertifikasi : M. Suryowibowo([EMAIL PROTECTED])
Komisi OTODA : Ridwan Djamaluddin([EMAIL PROTECTED] atau [EMAIL PROTECTED]), Arif
Zardi Dahlius([EMAIL PROTECTED])
Komisi Database Geologi : Aria A. Mulhadiono([EMAIL PROTECTED])
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