[iagi-net-l] gimana ya kira2 akhir dari Cepu
Monday May 2, 2:50 PM INTERVIEW: Indonesia Min Sees Progress In Exxon Dispute By Phelim Kyne Of DOW JONES NEWSWIRES JAKARTA (Dow Jones)--Exxon Mobil Corp. (XOM) of the U.S. and Indonesia's state-owned petroleum firm Pertamina (PTM.YY) have made significant progress toward resolving a long-running investment dispute that has tainted investors' perceptions of Indonesia, Minister of State Enterprises Sugiharto said recently. The government hopes to reach an agreement as soon as possible on extending Exxon's contract to develop the country's largest untapped oil field in Cepu, East Java province, Sugiharto told Dow Jones Newswires. Pertamina's 11-member Cepu negotiating team resumed talks with Exxon late last month in a bid to resolve the dispute by an official May 20 deadline and Sugiharto said an agreement was likely within months, not years. The mutual interest...(of) the government, Pertamina and Exxon is to monetize as soon as possible the strategic reserves that have been discovered on the Cepu blocks, Sugiharto said. That would also give certainty to any investors...(because) this (dispute) isn't good for Indonesia. Exxon Mobil Oil Indonesia Inc. declined to provide specific comment on Sugiharto's comments, but instead released a statement to Dow Jones Newswires that said the firm is committed to reaching an equitable and amicable resolution of Cepu issues...(and) bringing this important resource to market. The statement didn't elaborate. Efforts to contact Pertamina's lead negotiator in the Exxon talks were unsuccessful The dispute over the Cepu oil field, with estimated reserves of about 600 million barrels of crude oil, has been frequently cited as an exemplar of the policy confusion that's caused Indonesia's crude oil production to plunge in recent years. Indonesia, the sole Southeast Asian member of the Organization of Petroleum Exporting Countries, turned into a net importer of crude oil for several months last year due to lack of investment in exploration and development. Indonesia is now mulling downgrading its OPEC participation to observer status as a cost-saving measure. Exxon bought the rights to the Cepu field in 1999 from a company run by a son of Indonesia's former dictator Suharto. Shortly thereafter, the U.S. firm discovered that Cepu contained a commercial quantity of crude oil. However, development of Cepu has floundered on Exxon's inability to date to get an extension of its oil rights contract, which expires in 2010. It's not in our best interest to wait until 2010 (because) we badly need the crude for domestic uses, Sugiharto said. The Exxon dispute, along with other high-profile business conflicts involving Mexican cement producer Cemex S.A. De C.V. (CX) and U.S. power firm Karaha Bodas Co., are complicating efforts of the government of President Susilo Bambang Yudhoyono to lure back foreign investors to help fuel a 6.6% annual average economic expansion target from 2004 to 2009. Indonesia recorded a 26% year-on-year decline in approved foreign direct investment to $10.3 billion in 2004 due to investor perceptions of rampant corruption, shambolic infrastructure and an unpredictable judiciary. Exxon and Pertamina's discussions to negotiate mutually acceptable terms for a renewal of the U.S. firm's contract hinge on agreement on the proportion of oil revenues the two companies will share, Sugiharto said. (Exxon's) already expressed certain requirements, but it's too early to mention to anybody the percentage they want because there's still a gap between what Pertamina wants in terms of percentage and split, he said, without elaborating. __ Do You Yahoo!? Tired of spam? Yahoo! Mail has the best spam protection around http://mail.yahoo.com
Re: [iagi-net-l] gimana ya kira2 akhir dari Cepu
Aku kaget kalau hal ini dianggap sebagai dispute, padahal aku pikir ini hanya masalah negosiasi saja. Sesuatu interaksi kelanjutan usaha yg sudah disepakati sebelumnya, bahwa daerah cepu ini boleh dikelola Exxon sampai akhir masa kontrak itu sebuah kesepakatan bersama itu komitmen bersama, bahwa daerah ini bisa diperpanjang atau dihentikan itu juga sudah ada dlam kesepakatannya. Apakah Exxon tidak bisa dipegang komitmennya ? Jadi aku yakin ini bukan dispute. Bahkan menurut saya kita berhak utk tidak menanggapinya. Sudah berapa saja lapangan minyak di Malaysia ini yg tidak diperpanjang oleh PMU, dan dikelola oleh Petronas. Dan ini semua menjadi salahsatu bentuk usaha yg memajukan Petronas. Perlu kebranian Perlu perhitungan Perlu kemandirian Salam RDP On 5/2/05, Ariadi Subandrio [EMAIL PROTECTED] wrote: Monday May 2, 2:50 PM INTERVIEW: Indonesia Min Sees Progress In Exxon Dispute By Phelim Kyne Of DOW JONES NEWSWIRES JAKARTA (Dow Jones)--Exxon Mobil Corp. (XOM) of the U.S. and Indonesia's state-owned petroleum firm Pertamina (PTM.YY) have made significant progress toward resolving a long-running investment dispute that has tainted investors' perceptions of Indonesia, Minister of State Enterprises Sugiharto said recently. The government hopes to reach an agreement as soon as possible on extending Exxon's contract to develop the country's largest untapped oil field in Cepu, East Java province, Sugiharto told Dow Jones Newswires. Pertamina's 11-member Cepu negotiating team resumed talks with Exxon late last month in a bid to resolve the dispute by an official May 20 deadline and Sugiharto said an agreement was likely within months, not years. The mutual interest...(of) the government, Pertamina and Exxon is to monetize as soon as possible the strategic reserves that have been discovered on the Cepu blocks, Sugiharto said. That would also give certainty to any investors...(because) this (dispute) isn't good for Indonesia. Exxon Mobil Oil Indonesia Inc. declined to provide specific comment on Sugiharto's comments, but instead released a statement to Dow Jones Newswires that said the firm is committed to reaching an equitable and amicable resolution of Cepu issues...(and) bringing this important resource to market. The statement didn't elaborate. Efforts to contact Pertamina's lead negotiator in the Exxon talks were unsuccessful The dispute over the Cepu oil field, with estimated reserves of about 600 million barrels of crude oil, has been frequently cited as an exemplar of the policy confusion that's caused Indonesia's crude oil production to plunge in recent years. Indonesia, the sole Southeast Asian member of the Organization of Petroleum Exporting Countries, turned into a net importer of crude oil for several months last year due to lack of investment in exploration and development. Indonesia is now mulling downgrading its OPEC participation to observer status as a cost-saving measure. Exxon bought the rights to the Cepu field in 1999 from a company run by a son of Indonesia's former dictator Suharto. Shortly thereafter, the U.S. firm discovered that Cepu contained a commercial quantity of crude oil. However, development of Cepu has floundered on Exxon's inability to date to get an extension of its oil rights contract, which expires in 2010. It's not in our best interest to wait until 2010 (because) we badly need the crude for domestic uses, Sugiharto said. The Exxon dispute, along with other high-profile business conflicts involving Mexican cement producer Cemex S.A. De C.V. (CX) and U.S. power firm Karaha Bodas Co., are complicating efforts of the government of President Susilo Bambang Yudhoyono to lure back foreign investors to help fuel a 6.6% annual average economic expansion target from 2004 to 2009. Indonesia recorded a 26% year-on-year decline in approved foreign direct investment to $10.3 billion in 2004 due to investor perceptions of rampant corruption, shambolic infrastructure and an unpredictable judiciary. Exxon and Pertamina's discussions to negotiate mutually acceptable terms for a renewal of the U.S. firm's contract hinge on agreement on the proportion of oil revenues the two companies will share, Sugiharto said. (Exxon's) already expressed certain requirements, but it's too early to mention to anybody the percentage they want because there's still a gap between what Pertamina wants in terms of percentage and split, he said, without elaborating. __ Do You Yahoo!? Tired of spam? Yahoo! Mail has the best spam protection around http://mail.yahoo.com -- Education can't stop natural disasters from occurring, but it can help people prepare for the possibilities ---
RE: [iagi-net-l] derajat compaction antara clastic dan karbonat
Selain overburden yg tersusun oleh batuan karbonat lebih menyebabkan penurunan porositas secara fisik terhadap batuan klastik yg ada di bawahnya, batuan karbonat tersebut dapat pula menyebabkan penurunan porositas melalui proses kimia yaitu sementasi karbonat (i.e. calcite cementation) thd batuan silisiklastik tsb. Semen tsb dpt berasal dari hasil pelarutan batuan karbonat oleh air formasi. Air formasi tsb dapat masuk ke batuan silisiklastik akibat kontak langsung secara stratigrafi antara batuan silisiklastik dg batuan karbonat atau karena posisi struktur yg memungkinkan hal tsb utk terjadi-- (personal judgement). Namun demikian, batuan silisiklastik yg berada di bawah batuan karbonat tidak mesti harus tight. Contohnya F. Talang Akar yg ada dibawah F. Baturaja. Salam Usman Jauhari I Nengah Nuada [EMAIL PROTECTED] wrote: Overburden merupakan fungsi density dari batuan penyusun, semakin besar density batuan akan semakin besar pula angka overburdennya. Karena umumnya karbonat mempunyai density yang lebih besar daripada sedimen klastik maka kemungkinan besar overburden yang terdiri dari 1000 m sedimen klastik dan 1000 m karbonat akan memberikan efek pengurangan density yang lebih besar dibandingan dengan overburden yang tersusun atas 2000 m sedimen klastik. Salam, INN -Original Message- From: [EMAIL PROTECTED] [mailto:[EMAIL PROTECTED] Sent: Thursday, April 28, 2005 7:57 AM To: iagi-net@iagi.or.id Subject: [iagi-net-l] derajat compaction antara clastic dan karbonat Importance: High Kalau kita hendak menghitung potensial porosity di deep reservoir...umumnya kita melakukan model dengan menggunakan derajat overburden / kompaksi di bagian atasnya dan kemudian kita extrapolasikan ke bawah... Kalau kita punya overburden dengan lithology yang berbeda mis : clastic (sand shale ) dan carbonate (platform/ reef ) tentu akan memberikan derajat kompaksi yang berbeda juga pertanyaannya : kalau kita punya deep reservoir (clastic) lalu diatasnya terdapat overburden clastic (2000 m) dibandingkan dengan overburden campuran (clastik 1000 m dan karbonate 1000 m) , manakah yang akan memberikan effect pengurangan porosity karena kompaksi (apakah yang pure clastic atau yang campuran )..? Mungkin ada yang bisa memberi pencerahan... Terima kasih Regards Ferdinandus Kartiko Samodro TOTAL EP Indonesie Balikpapan DKS/EXR/GLG 0542- 533852 - To unsubscribe, send email to: [EMAIL PROTECTED] To subscribe, send email to: [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) : Deddy Sebayang([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, send email to: [EMAIL PROTECTED] To subscribe, send email to: [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) : Deddy Sebayang([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]) - __ Do You Yahoo!? Tired of spam? Yahoo! Mail has the best spam protection around http://mail.yahoo.com
RE: [iagi-net-l] Tanya : Water depth Glossifungites Ichnofacies
1. Utk Pak Herman : dimana bisa dapet publikasi tsb? Kalo punya softcopy-nya, boleh dong saya minta file-nya? 2. Untuk Pak Oki : What is the big picture of your area? Apakah masih berada pada shelf (landward from shelf break) ataukah udah di basin floor (basinward from shelf break)? Kalo kasus I yg terjadi, saya lebih yakin utk mengatakan endapan laut dangkal (beach/inner shelf -- middle shelf)--subaerial exposure then transgression. Kalo kasus II yg terjadi, saya lebih cenderung spt apa yg ada di paper yg Pak Herman sebutkan. Salam Usman Jauhari Darman, Herman H BSP-TSX/4 [EMAIL PROTECTED] wrote: Oki, Mungkin bisa belajar dari New Jersey Slope. Herman ___ Firmground Ichnofabrics in Deep-water Sequence Stratigraphy, Tertiary Clinoform-toe Deposits, New Jersey Slope Savrda et al, Palaios 2001, v. 16, p 294-305 Sixteen erosional surfaces are recognized in a 144-m-thick condensed package of Tertiary (Eocene-Pliocene) clinoformtoe sediments recovered at ODP Site 1073 on theNewJersey slope. Most of these surfaces are associated with significant hiatuses or extremely condensed intervals defined by Sr isotopes or biostratigraphic data, and many can be linked to sequence boundaries defined in onshore and shelf seismic studies. All surfaces define the bases of fining upward sequences; they separate clay or biogenicmuds belowfromauthigenic glauconitic sandy muds or sands above. The entire Tertiary package is thoroughly bioturbated and dominated by ichnotaxa representing softground conditions. Burrow densities, burrow preservation, and the relative importance of certain ichnotaxa vary through the Tertiary package, re- flecting changes in water depth, relative degree of condensation, and associated glaucony authigenesis, all related to margin progradation. Nonetheless, when individual sequences are considered, little or no change in softground ichnofossil assemblages is recognized across bounding surfaces. However, most surfaces are marked clearly by firmground Thalassinoides, burrow systems that penetrate deeply (up to 2 m) into subjacent clays and are characterized by extremely sharp walls and coarser glauconitic fills. In shallower shelf sequences, firmground ichnofabrics develop at sequence boundaries in response to subaerial exposure and transgressive ravinement. In contrast, the Tertiary firmgrounds on the New Jersey margin formed in deep water in response to phases of rapid transgression and net erosion; consolidated mud substrates were exhumed as a result of sediment starvation and bottom-current winnowing, facilitated by bioerosion, at or near the bases of slope clinoforms. These observations extend the previously established sequence stratigraphic utility of the substrate-controlled Glossifungites ichnofacies to deeper water facies. -Original Message- From: [EMAIL PROTECTED] [mailto:[EMAIL PROTECTED] Sent: 26 April 2005 15:14 To: iagi-net@iagi.or.id Subject: Re: [iagi-net-l] Tanya : Water depth Glossifungites Ichnofacies Mas Oki, Pernah kok dibahas mengenai keberadaan glossifungites ichnofacies pada sedimen bathyal. Salah satunya Hayward (1976), Lower Miocene Bathyal Submarine Canyon ichnofacies from Northland, New Zealand. Saya tidak punya papernya, tapi sepertinya ada sedikit di bahas dalam Facies Model-nya Walker. salam, -sw- Musakti, Oki os.com cc: 04/26/2005 10:51 AM Subject: [iagi-net-l] Tanya : Water depth Glossifungites Please respond to Ichnofacies iagi-net Glossifungites ichnofacies selalu didefinisikan dengan kumpulan trace fossil (an. Thallasinoides, Rhizocorralium etc) pada firm ground (semi lithified) sediment. Dalam konteks sequence stratigraphy, glossifungites ichnofacies ini sering dikaitkan dengan transgressive surface atau ravinement, karena indikasi bahwa telah terjadi erosi dan 'removal' dari unconsolidated sediment diatasnya. Dari segi water depth, Glossi surface ini biasanya diasosiasikan dengan near shore environment, inner sampai mid neritik. Pokoknya diatas wave base. Pertanyaan: Apakah ada kemungkinan glossi ini terjadi juga di tempat yang lebih dalam ie. Outer sublittoral bahkan bathyal seperti diindikasikan secara konsisten oleh biostratigraphy (ie. Plankton-benton foram ratio, deep water bentonic taxa etc). Bagaimana kalau sang ichnologist berkeras menyebut shallow marine environment sedangkan biostratigrapher 'kekeuh' pada deep water untuk interval yang sama. Mana yang harus kita 'percaya' dan apakah mungkin ada kompromi diantara keduanya ie. erosi dan pemindahan sediment penutup terjadi secara subaquaous via contourite current dan semacamnya. Ada yang punya contoh2 glossi surface di deep water...? Thanks Oki Santos Ltd A.B.N. 80 007 550 923 Disclaimer: The information contained in this email is intended only for the use of the person(s) to whom it is addressed and may be confidential or contain privileged information. If you are not the intended recipient you are hereby notified that any perusal, use,
[iagi-net-l] Fwd: May 11 and June 22 Tsunami Lectures from Dr. Imamura
Info buat pengamat, pemerhati serta peminat gejala tsunami. trims buat Dikshie RDP -- Forwarded message -- From: Dikshie [EMAIL PROTECTED] Date: May 2, 2005 10:51 PM Subject: May 11 and June 22 Tsunami Lectures from Dr. Imamura To: [EMAIL PROTECTED] Salah satu pakar tsunami di Jepang Prof Fumihiko Immamura dari DCRC Tohoku Univ akan memberikan Tsunami lecture/course. Tempat di Ruang B gedung Litbang, Integrasi, dan Aplikasi (d/h gedung PAU) tgl 11 May 2005 jam 14-15.30 tgl 22 Juni 2005 jam 09.00-10.30 silahkan hadir dan ajak teman2 ! - Forwarded message from Sayaka Fukuda - Dear SOI Asia Partners, Prof. Dr. Fumihiko Imamura, Tohoku U., will give two lectures for SOI Asia Project!! (1) May 11 JST 16:00-17:30 Mechanism of tsunami generation, propagation, and runup (2) June 22 JST11:00-12:30 Tsunamis disaster and lessons for mitigation His bio date is here: http://www.tsunami.civil.tohoku.ac.jp/hokusai2/main/eng/imamura.html Please invite participants to the upcoing lectures!!! In addition to these two lectures, we are now planning Tsunami lectures from Indonesia, Thailand and Japan. Please wait for detailed contents and schedule! Sayaka Fukuda SOI Asia Project - End forwarded message - -dikshie- -- Education can't stop natural disasters from occurring, but it can help people prepare for the possibilities ---
RE: [iagi-net-l] derajat compaction antara clastic dan karbonat
kalau boleh tahu berapa kedalaman (ssea) dari formasi talang akar yang ada di bawah baturaja di daerah bapak...? Regards Ferdinandus Kartiko Samodro TOTAL EP Indonesie Balikpapan DKS/EXR/GLG 0542- 533852 usman jauhari [EMAIL PROTECTED] 02/05/2005 09:34 PM Please respond to iagi-net To: iagi-net@iagi.or.id cc: Subject:RE: [iagi-net-l] derajat compaction antara clastic dan karbonat Selain overburden yg tersusun oleh batuan karbonat lebih menyebabkan penurunan porositas secara fisik terhadap batuan klastik yg ada di bawahnya, batuan karbonat tersebut dapat pula menyebabkan penurunan porositas melalui proses kimia yaitu sementasi karbonat (i.e. calcite cementation) thd batuan silisiklastik tsb. Semen tsb dpt berasal dari hasil pelarutan batuan karbonat oleh air formasi. Air formasi tsb dapat masuk ke batuan silisiklastik akibat kontak langsung secara stratigrafi antara batuan silisiklastik dg batuan karbonat atau karena posisi struktur yg memungkinkan hal tsb utk terjadi-- (personal judgement). Namun demikian, batuan silisiklastik yg berada di bawah batuan karbonat tidak mesti harus tight. Contohnya F. Talang Akar yg ada dibawah F. Baturaja. Salam Usman Jauhari I Nengah Nuada [EMAIL PROTECTED] wrote: Overburden merupakan fungsi density dari batuan penyusun, semakin besar density batuan akan semakin besar pula angka overburdennya. Karena umumnya karbonat mempunyai density yang lebih besar daripada sedimen klastik maka kemungkinan besar overburden yang terdiri dari 1000 m sedimen klastik dan 1000 m karbonat akan memberikan efek pengurangan density yang lebih besar dibandingan dengan overburden yang tersusun atas 2000 m sedimen klastik. Salam, INN -Original Message- From: [EMAIL PROTECTED] [mailto:[EMAIL PROTECTED] Sent: Thursday, April 28, 2005 7:57 AM To: iagi-net@iagi.or.id Subject: [iagi-net-l] derajat compaction antara clastic dan karbonat Importance: High Kalau kita hendak menghitung potensial porosity di deep reservoir...umumnya kita melakukan model dengan menggunakan derajat overburden / kompaksi di bagian atasnya dan kemudian kita extrapolasikan ke bawah... Kalau kita punya overburden dengan lithology yang berbeda mis : clastic (sand shale ) dan carbonate (platform/ reef ) tentu akan memberikan derajat kompaksi yang berbeda juga pertanyaannya : kalau kita punya deep reservoir (clastic) lalu diatasnya terdapat overburden clastic (2000 m) dibandingkan dengan overburden campuran (clastik 1000 m dan karbonate 1000 m) , manakah yang akan memberikan effect pengurangan porosity karena kompaksi (apakah yang pure clastic atau yang campuran )..? Mungkin ada yang bisa memberi pencerahan... Terima kasih Regards Ferdinandus Kartiko Samodro TOTAL EP Indonesie Balikpapan DKS/EXR/GLG 0542- 533852 - To unsubscribe, send email to: [EMAIL PROTECTED] To subscribe, send email to: [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) : Deddy Sebayang([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, send email to: [EMAIL PROTECTED] To subscribe, send email to: [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) : Deddy Sebayang([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]) - __ Do You Yahoo!? Tired of spam? Yahoo! Mail has the best spam protection around http://mail.yahoo.com - To unsubscribe, send email to: [EMAIL PROTECTED] To subscribe, send email to: [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
RE: [iagi-net-l] Tanya : Water depth Glossifungites Ichnofacies
Repotnya disitu, kita nggak pasti dimana (atau apakah ada) shelf-slope break pada saat itu.. -Original Message- From: usman jauhari [mailto:[EMAIL PROTECTED] Sent: Monday, 2 May 2005 9:07 PM To: iagi-net@iagi.or.id Subject: RE: [iagi-net-l] Tanya : Water depth Glossifungites Ichnofacies 1. Utk Pak Herman : dimana bisa dapet publikasi tsb? Kalo punya softcopy-nya, boleh dong saya minta file-nya? 2. Untuk Pak Oki : What is the big picture of your area? Apakah masih berada pada shelf (landward from shelf break) ataukah udah di basin floor (basinward from shelf break)? Kalo kasus I yg terjadi, saya lebih yakin utk mengatakan endapan laut dangkal (beach/inner shelf -- middle shelf)--subaerial exposure then transgression. Kalo kasus II yg terjadi, saya lebih cenderung spt apa yg ada di paper yg Pak Herman sebutkan. Salam Usman Jauhari Darman, Herman H BSP-TSX/4 [EMAIL PROTECTED] wrote: Oki, Mungkin bisa belajar dari New Jersey Slope. Herman Santos Ltd A.B.N. 80 007 550 923 Disclaimer: The information contained in this email is intended only for the use of the person(s) to whom it is addressed and may be confidential or contain privileged information. If you are not the intended recipient you are hereby notified that any perusal, use, distribution, copying or disclosure is strictly prohibited. If you have received this email in error please immediately advise us by return email and delete the email without making a copy. - To unsubscribe, send email to: [EMAIL PROTECTED] To subscribe, send email to: [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) : Deddy Sebayang([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]) -
