abah, kalo soal kredit utk makalah yg dipresentasikan oral dan poster, saya enggak tahu. mungkin teman2 di kampus atau lembaga pemerintahan lebih mengerti. silakan dibagikan ceritanya..
saya munculkan hal ini, sebab sudah lebih dari 5 tahun, iagi mengikuti jejak ipa utk menganggap bahwa presentasi poster adalah sama derajatnya dengan oral. kebetulan saat ini saya diserahi amanah utk pegang tongkat di kepanitiaan ipa 2008 bagian tpc (technical program committee). eh, enggak disangka, secara tidak langsung ternyata ada bule (anggota komisi ini ada sekitar 20 orang dan separuhnya adalah bule) yg masih 'membedakan' antara poster dan oral. jelasnya, poster masih dianggap sbg kelas dua. sudah waktunya kita menganggap, di lingkungan iagi, hagi, perhapi, iatmi, ipa, dll, bahwa poster adalah sama derajatnya dg oral dan mempunyai kelebihan masing2. artinya, pada suatu acara formal, tentunya setiap penulis mesti mengirimkan makalah lengkap utk dua jenis presentasi tsb. salam, syaiful On Thu, Apr 24, 2008 at 7:36 AM, yanto R.Sumantri <[EMAIL PROTECTED]> wrote: > > > > > Mas Ipul > > Saya kira Anda benar bahw waktu diskusi > yang paling leluasa adalah apabila kita melakukan poster session. > > > Akan tetapi para calon pemakalah kelihatan-nya lebih senang > untuk melakukan Oral Presentation , Apakah hal ini al disebabkan nliai > kredit - nya yang lebih rendah ? > > Si Abah > > > 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 <[EMAIL PROTECTED]> > > 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. > > > --------------------------------------------------------------------- > > > > > > > -- > _______________________________________________ > Nganyerikeun hate > batur hirupna mo bisa campur, ngangeunahkeun hate jalma hirupna pada > ngupama , Elmu tungtut dunya siar Ibadah kudu lakonan. > -- 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. ---------------------------------------------------------------------
