Pak Awang, Mohon maaf lupa merespon langsung. Iya, memang super lengkap. Saya tunggu kiriman digital abstrak (dan mungkin kalau ada yg lebih lengkap) via japri.
Terimakasih dan salam, syaiful On Thu, Apr 24, 2008 at 10:53 AM, Awang Satyana <[EMAIL PROTECTED]> wrote: > Pak Syaiful, > > Berikut daftar acara lengkap workshop carbonate complexity IATMI diurutkan > dari hari pertama – hari ke-4. > > Tidak ada makalah lengkap. Abstrak dari semua pembicara bisa saya kirimkan > ke ja-pri. Bisa dilihat bahwa workshop ini meliputi A to Z karbonat. > > salam, > awang > > Pre-workshop course > > > Introduction to carbonate rocks and sedimentology (Alit Ascaria -Premier > Oil) > From laboratory to optimum reservoir simulation for naturally fractured > carbonate reservoir – (Doddy Abdassah-ITB) > > Keynote speech/presentation > > > Uncertainties in carbonate reservoir in Indonesia (Handoyo Wahono-BPMIGAS) > Exploration in carbonate life (Bob Yulian-BPMIGAS) > Increasing reserves and hydrocarbons production out of carbonate rocks : > challenges and opportunities in Indonesia (Gatot Wiroyudo-Shell) > > Technical presentation > > > Geologic controls on carbonate reservoirs in Indonesia : regional overview > (Awang Satyana-BPMIGAS) > Carbonate seismology (Ardiansyah-Pertamina) > To perforate or not perforate (Robert Park-Kodeco) > Borehole images : an alternative method for carbonate characterization > (Richard Netherwood-Schlumberger) > Fracture characterization and modeling with automated seismic volume > interpretation : example from SE Asia (Georg Warrlich-Shell) > Carbonate reservoir : challenges in facies modeling and fracture > characterization (Subrata Chakraborty-Schlumberger) > Carbonate facies analyses and reservoir characterization, early Miocene > Baturaja formation; Bernai structure, South Sumatra Basin (Alit > Ascaria-Premier Oil) > 4D (time-lapse) microgravity survey for monitoring HC reservoir,case study > :carbonate reservoir of Baturaja formation (Wawan Gunawan-ITB) > So similar and yet so different : comparing and contrasting the controlling > factors for reservoir development of two SE Asia Tertiary carbonate build-ups > (Georg Warrlich-Shell) > Innovation in petropysical techniques for carbonate characterization (Udit > Kumar-Schlumberger) > The practical technique and its complexity of static modeling in > autochtonous and allochtonous carbonates, a case study in Thamama (United > Arab Emirate) and Baturaja reservoir (Indonesia) (Abdul Latif-Roxar) > carbonate petrophysics from borehole image logs (Richard > Netherwood-Schlumberger) > Formation log analysis : formation factor adjustment to accommodate > porosity types in carbonate reservoir, case study (Argha Satya-JOB > Pertamina-PetroChina Salawati) > Integrated reservoir characterization in thin oil column carbonate > reservoir for depletion plan scenario (Dwi Febrianto-Medco) > Technical aspect to develop carbonate fractured reservoir (Galih > Agusetiawan-BPMIGAS) > A study of porosity and carbonate facies in Prupuh formation, > Lamongan-Gresik, East Java (Premonowati-UPN Yogyakarta) –alternate > > Field Trip (karbonate Formasi Wonosari) > > Karang Duwet, Paliyan,Gunung Kidul – field guide : Wartono Rahardjo (UGM) > - Kamis 24/4/2008 –setengah hari > > > mohammad syaiful <[EMAIL PROTECTED]> wrote: bravo, pak awang! terimakasih > atas infonya. > > 1) boleh juga nih kalau diinfokan juga apa saja judul ke-16 makalah yg > dipresentasikan tsb. lebih lanjut, apakah bagi yg tidak hadir pada > acara tsb, dapat memperoleh makalah lengkapnya (kalau ada), mungkin > lewat iatmi ya? > > 2) tentang format presentasi secara formal, tentu saja waktunya selalu > terbatas atau dibatasi. seharusnya tidak ada istilah terburu-buru, > karena si presenter sudah tahu alokasi waktunya dan tentunya dapat > menyesuaikan diri dan memberikan presentasi (oral) secara pas. > > masih mengenai presentasi, apabila ingin memberikan presentasi dg > lebih leluasa dan ilmunya dapat saling dicerna, maka presentasi > berbentuk poster adalah pilihan yg lebih baik dibandingkan dg > presentasi oral. saya bisa panjang-lebar cerita ini, tetapi pada > intinya bahwa presentasi poster bukanlah kelas dua dibandingkan dg > presentasi oral yg katanya (oleh sebagian orang) dianggap lebih > bergengsi. > > salam, > syaiful > > > On Thu, Apr 24, 2008 at 2:16 AM, Awang Satyana wrote: > > IATMI sedang mengadakan worshop "carbonate complexity : characterization, > > modeling and simulation" di Yogyakarta dari 22-25 April 2008. Workshop > > dihadiri sekitar 80 orang dari berbagai institusi pemerintah, oil > > companies, service companies, dan perguruan tinggi. > > > > Workshop didahului oleh kursus satu hari tentang aspek geologi dan > > reservoir engineering karbonat dibawakan oleh Alit Ascaria (Premier Oil) > > dan Doddy Abdassah (ITB). > > > > Workshop dibuka pada 23 April 2008 oleh Ketua IATMI Kuswo Wahyono, > > dilanjutkan dengan pidato sambutan oleh John Sinulingga mewakili Pertamina > > Eksploitasi (panitia workshop adalah IATMI Komda Cirebon –Pertamina), dan > > pidato/presentasi kunci dari Handoyo Eko Wahono (BPMIGAS) tentang > > lapangan-lapangan karbonat yang dikembangkan dalam lima tahun terakhir, Bob > > Yulian (BPMIGAS) tentang kemajuan eksplorasi target karbonat di Indonesia, > > dan Gatot Kariyoso Wiroyudo (Shell) tentang investasi teknologi Shell dalam > > mengerjakan karbonat. > > > > Makalah teknis yang dipresentasikan sebanyak 16 makalah. Workshop diselingi > > dengan fieldtrip ke Gunung Kidul mengunjungi singkapan karbonat Wonosari. > > > > Pembicara mendapatkan kesempatan berbicara cukup tenang karena waktu yang > > diberikan antara 20-30 menit, pertanyaan 5-10 menit. Workshop ini jelas > > bermanfaat menambah wawasan aspek GGRE karbonat. Karbonat merupakan > > objektif sangat penting karena menyusun sekitar 50 % reservoir lapangan2 > > produksi di Indonesia. Bahkan dalam lima tahun terakhir, 54 % recoverable > > reserve lapangan-lapangan baru berasal dari reservoir karbonat, maka > > karbonat tak kalah penting dari reservoir silisiklastik, bahkan bisa lebih. > > > > Saya diundang IATMI berkontribusi makalah tentang geologi regional karbonat > > di Indonesia. Di bawah ini adalah abstraknya, semoga berguna. > > > > Mahasiswa tidak banyak yang hadir. Karena merasa ada yang kurang kalau saya > > hanya mempresentasikan makalah saya kepada para profesional di workshop, > > maka pada hari yang sama saya ke UGM dan mempresentasikan materi yang sama > > di hadapan para mahasiswa tetapi dalam format penyampaian kepada mahasiswa. > > Setelah itu, masih di UGM, saya melanjutkan mempresentasikan makalah > > "Sandhyakala ning Jenggala dan Majapahit : Hipotesis Kebencanaan Geologi" – > > kali ini jauh lebih tenang tak seperti saat mempresentasikan makalah ini di > > PIT IAGI 2007 Bali yang mesti berpacu dengan waktu yang terbatas. Waktu > > yang terbatas atau terburu2 akan menyulitkan pendengar mencerna materi yang > > disampaikan. Sebagai informasi, hipotesis ini telah "ditangkap" National > > Geographic Channel untuk menjadi tayangan (pengambilan gambar sudah > > dilalukan) di dalam film dokumenter "LUSI". > > > > Demikian, laporan singkat. > > awang – Grand Mercure – 24/4/2008, 02.15 > > > > LAMPIRAN > > > > Geologic Controls on Carbonate Reservoirs in Indonesia : > > Regional Overview > > > > Awang Harun Satyana > > > > (BPMIGAS) > > > > Carbonate reservoirs are characterized by extreme heterogeneity of porosity > > and permeability. This is related to the complexities of the original > > depositional environment and the diagenetic influences that can modify the > > original textures. Wide variety of environmental facies and diagenetic > > changes express controls of geologic factors. Therefore, in characterizing > > carbonate reservoirs, it is important to evaluate geologic controls which > > influence carbonate sedimentation and diagenesis. > > > > Being located at warm humid tropical shallow water, in Indonesia carbonates > > are geographically and temporally widespread. They occur in a range of ages > > and depositional settings which were often affected by coeval tectonism, > > siliciclastic input or volcanism. The carbonates developed in various > > tectonic settings of back-arc, intra-arc, fore-arc, and foreland basins; > > island arc; micro-continents; and continental passive margins. They > > developed as patch reefs of land-attached platform such as Baturaja > > buildups in South Sumatra and West Java, fringing reefs such as Kais > > buildups on Arar High, the Bird's Head of Papua, barrier reefs such as > > Ujung Pangkah reefs in East Java, and pinnacle reefs overlying offshore > > isolated platforms such as reefs of the Cepu High, East Java and Arun reefs > > in North Sumatra. In each a variety of carbonate depositional systems, the > > reefs often developed on structural highs. Subsidence, uplift, active > > faulting, tilting or associated > > silici/volcaniclastic input strongly affected facies variability, > > stratal/platform geometries, sequence development and carbonate > > termination. These geologic factors influence distribution and continuity > > of the carbonate reservoirs. > > > > Ages of carbonates influence the basic ingredients of carbonates. > > Diversity, abundance, dominant mineralogy, and relative importance of > > sediment-producing marine invertebrates are various through the geologic > > periods. This will influence the response of carbonates when they are > > changed by diagenesis. Producing carbonate reservoirs in Indonesia range in > > ages from the Jurassic Manusela fractured oolitic carbonates in Seram > > Island, Eastern Indonesia to Pliocene globigerinid limestones of the Madura > > Strait. Paleogene carbonates in Indonesia are commonly dominated by larger > > foraminifera. These carbonates typically form large-scale platforms or > > isolated shoals. Good poroperms can be preserved in shoal or redeposited > > carbonates lacking micrite. Secondary porosities developed due to > > fracturing, chemical dissolution during burial, or as karstic cavities. > > However, the opportunities for leaching were limited. Neogene carbonates > > often contain abundant aragonitic bioclasts, such as > > corals. They typically develop as reefal buildups, shelfal deposits or as > > isolated platforms. Compared with Paleogene carbonates, poroperms are > > generally higher in Neogene carbonates, various porosities all occur. The > > most important, common and economic carbonate reservoirs in Indonesia are > > the Miocene buildups such as Arun in North Sumatra, Baturaja in South > > Sumatra and West Java, Kujung I or Prupuh in East Java, and Kais in > > Salawati, Papua. > > > > Petrographic studies of carbonate reservoirs in Indonesia have shown that > > they have been subjected to a number of diagenetic processes including > > compaction (stylolization), dissolution, cementation, neomorphism, > > silicification, dolomitization and fracturing. Most of these processes are > > common to all depositional facies types (reefal, near reef, shallow shelf > > and outer shelf open marine). Original particle types of the sediments > > inherited from the deposition play an important role in this respect. > > Interconnected corallites commonly suffer dissolution resulting in > > porosities. Neomorphism is especially common in micritic carbonates > > reducing their porosities. Dolomitization has a varied distribution and in > > many cases is associated with clay minerals. It may affect reservoir > > poroperms and be a factor in generation of undesirable non-hydrocarbon > > gases. Stylolization and silicification are localized features. Study of > > sequence of diagenetic events is important for knowing the > > preservation or occlusion of porosities. > > > > An understanding of the geologic controls on carbonate depositional > > environments, spatial and temporal facies distributions and controls on > > deposition and diagenesis is essential in order to characterize carbonate > > reservoirs and to evaluate their considerable economic potential.*** > > > > > > --------------------------------- > > Be a better friend, newshound, and know-it-all with Yahoo! Mobile. Try it > > now. > > > > -- > Mohammad Syaiful - Explorationist, Consultant Geologist > Mobile: 62-812-9372808 > Email: [EMAIL PROTECTED] > > Technical Manager of > Exploration Think Tank Indonesia (ETTI) > > -------------------------------------------------------------------------------- > PIT IAGI KE-37 (BANDUNG) > * acara utama: 27-28 Agustus 2008 > * penerimaan abstrak: kemarin2 s/d 30 April 2008 > * pengumuman penerimaan abstrak: 15 Mei 2008 > * batas akhir penerimaan makalah lengkap: 15 Juli 2008 > * abstrak / makalah dikirimkan ke: > www.grdc.esdm.go.id/aplod > username: iagi2008 > password: masukdanaplod > > -------------------------------------------------------------------------------- > PEMILU KETUA UMUM IAGI 2008-2011: > * pendaftaran calon ketua: 13 Pebruari - 6 Juni 2008 > * penghitungan suara: waktu PIT IAGI Ke-37 di Bandung > AYO, CALONKAN DIRI ANDA SEKARANG JUGA!!! > > ----------------------------------------------------------------------------- > To unsubscribe, send email to: iagi-net-unsubscribe[at]iagi.or.id > To subscribe, send email to: iagi-net-subscribe[at]iagi.or.id > Visit IAGI Website: http://iagi.or.id > Pembayaran iuran anggota ditujukan ke: > Bank Mandiri Cab. Wisma Alia Jakarta > No. Rek: 123 0085005314 > Atas nama: Ikatan Ahli Geologi Indonesia (IAGI) > Bank BCA KCP. Manara Mulia > No. Rekening: 255-1088580 > A/n: Shinta Damayanti > IAGI-net Archive 1: http://www.mail-archive.com/iagi-net%40iagi.or.id/ > IAGI-net Archive 2: http://groups.yahoo.com/group/iagi > --------------------------------------------------------------------- > DISCLAIMER: IAGI disclaims all warranties with regard to information posted > on its mailing lists, whether posted by IAGI or others. In no event shall > IAGI and its members be liable for any, including but not limited to direct > or indirect damages, or damages of any kind whatsoever, resulting from loss > of use, data or profits, arising out of or in connection with the use of any > information posted on IAGI mailing list. > --------------------------------------------------------------------- > > > > > > --------------------------------- > Be a better friend, newshound, and know-it-all with Yahoo! Mobile. Try it > now. -- Mohammad Syaiful - Explorationist, Consultant Geologist Mobile: 62-812-9372808 Email: [EMAIL PROTECTED] Technical Manager of Exploration Think Tank Indonesia (ETTI) -------------------------------------------------------------------------------- PIT IAGI KE-37 (BANDUNG) * acara utama: 27-28 Agustus 2008 * penerimaan abstrak: kemarin2 s/d 30 April 2008 * pengumuman penerimaan abstrak: 15 Mei 2008 * batas akhir penerimaan makalah lengkap: 15 Juli 2008 * abstrak / makalah dikirimkan ke: www.grdc.esdm.go.id/aplod username: iagi2008 password: masukdanaplod -------------------------------------------------------------------------------- PEMILU KETUA UMUM IAGI 2008-2011: * pendaftaran calon ketua: 13 Pebruari - 6 Juni 2008 * penghitungan suara: waktu PIT IAGI Ke-37 di Bandung AYO, CALONKAN DIRI ANDA SEKARANG JUGA!!! ----------------------------------------------------------------------------- To unsubscribe, send email to: iagi-net-unsubscribe[at]iagi.or.id To subscribe, send email to: iagi-net-subscribe[at]iagi.or.id Visit IAGI Website: http://iagi.or.id Pembayaran iuran anggota ditujukan ke: Bank Mandiri Cab. Wisma Alia Jakarta No. Rek: 123 0085005314 Atas nama: Ikatan Ahli Geologi Indonesia (IAGI) Bank BCA KCP. Manara Mulia No. Rekening: 255-1088580 A/n: Shinta Damayanti IAGI-net Archive 1: http://www.mail-archive.com/iagi-net%40iagi.or.id/ IAGI-net Archive 2: http://groups.yahoo.com/group/iagi --------------------------------------------------------------------- DISCLAIMER: IAGI disclaims all warranties with regard to information posted on its mailing lists, whether posted by IAGI or others. In no event shall IAGI and its members be liable for any, including but not limited to direct or indirect damages, or damages of any kind whatsoever, resulting from loss of use, data or profits, arising out of or in connection with the use of any information posted on IAGI mailing list. ---------------------------------------------------------------------
