Her,..... Tertarik sekali , saya dengan paper tersebut....kalo bisa bagi2...yah wait for ur action.
salam yunianto -----Original Message----- From: Herry Maulana [mailto:[EMAIL PROTECTED]] Sent: Kamis, 23 Januari 2003 7:34 To: [EMAIL PROTECTED] Subject: RE: [iagi-net-l] Deep water source rock ... dimana dikau ? Kalo untuk Kutai Basin, ada paper bagus dari Peters et. al "A New Geochemical Seq. Stratigraphioc Model for the Mahakam Delta and Makassar Slope, Kalimantan, Indonesia", yg pada prinsipnya membahas kemungkinan Lowstand Sediments (Coal) sebagai source rock utk DW HC. aku ada pdfnya kalo mau. Kalo untuk North Sea, source untuk Paleogene Fan nya tetep di Kimmerdige Clay, yg mengandung banyak kerogen Type I (algal) dari endapan laut dalam. Kalo balik ke east kal lagi, untuk prediksi balik lagi ke regional setting. banyak kenampakan high amplitude reflectivity di slope setting, yg diperkirakan coal lowstand deposit dan mempunyai TOC yg significant untuk menghasilkan HC. untuk hard dan soft shale, things are bit complicated. Soft shale bisa jadi merupakan source rock yg bagus, tapi soft shale juga berarti over-pressured area (?) yg bisa hinder potential HC-nya. Hard shale? Ndak punya ide ;) tapi aku tau pasti beberapa hard shale di slope dan basin floor, TOC-nya rendah.. > -----Original Message----- > From: PUTROHARI Rovicky [SMTP:[EMAIL PROTECTED]] > Sent: Wednesday, 22 January, 2003 9:00 AM > To: [EMAIL PROTECTED] > Subject: [iagi-net-l] Deep water source rock ... dimana dikau ? > > Balik ke diskusi ilmiah aah .... > > HC Source rock utk deepwater sedimen sangat jarang dijumpai, walopun > deepwater HC sudah banyak terbukti. > Ada yg tahu tentang deepwater hydrocarbon source rock ? > Apa saja kendalanya ? ... adakah relasi dengan hingstand-lowstand period > dengan source potential ? oil/gas-pronnes .... > ... bagaimana memprediksikannya ...... logicnya saja lah ... trutama kalo > ndak ada data sumur, karena dimana-mana paling banyak data seismicnya > sajah..... namun sebenernya kita bisa juga melihat dari analogi well data > dimana udah penetrated deep water deposit namun setting saat ini ada di > shallow water (land) misal di East Java Basin). > Dari geophysics (seismic) point of view apakah kemungkinan potensial > source softshale lebih bagus dari hardshale, atau sebaliknya ? > > rdp > > > --------------------------------------------------------------------- > To unsubscribe, e-mail: [EMAIL PROTECTED] > Visit IAGI Website: http://iagi.or.id > IAGI-net Archive 1: http://www.mail-archive.com/iagi-net%40iagi.or.id/ > IAGI-net Archive 2: http://groups.yahoo.com/group/iagi > > 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]) > --------------------------------------------------------------------- --------------------------------------------------------------------- To unsubscribe, e-mail: [EMAIL PROTECTED] Visit IAGI Website: http://iagi.or.id IAGI-net Archive 1: http://www.mail-archive.com/iagi-net%40iagi.or.id/ IAGI-net Archive 2: http://groups.yahoo.com/group/iagi 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]) --------------------------------------------------------------------- EOM NOTICE - This message and any attached files may contain information that is confidential and/or subject of legal privilege intended only for use by the intended recipient. If you are not the intended recipient or the person responsible for delivering the message to the intended recipient, be advised that you have received this message in error and that any dissemination, copying or use of this message or attachment is strictly forbidden, as is the disclosure of the information therein. If you have received this message in error please notify the sender immediately and delete the message.
