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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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(One-page communication summarizing work on molluscs from ~3000m thick Pliocene deposits <strong>of</strong> N Aceh.<br />

Department <strong>of</strong> Mines collected >6000 molluscs, belonging to 347 different species. Typical Indo-Pacific fauna)<br />

Martin, K. (1929)- Ein neues Argonautiden Geschlecht von <strong>Sumatra</strong>. Leidsche Geol. Meded. 3, p. 221-226.<br />

('A new Argonaut genus from <strong>Sumatra</strong>'. New octopod nautiloid shell, described as Kapal batavus, from clay<br />

nodule in M-L Miocene Lower Palembang Beds <strong>of</strong> Pangadang, 25 km W <strong>of</strong> Sekayu, S <strong>Sumatra</strong>)<br />

Ma'ruf, M.F., A. Arsyad, G. Crouzet, S. Handoko & F. Langitan (1996)- Improved reservoir geology model<br />

using seismic 3D and Well Data, a case study, Rantau Field, <strong>Indonesia</strong>. In: SPE Asia Pacific Oil and Gas<br />

Conference, Adelaide 1996, 12p.<br />

(Reservoir geology model for part <strong>of</strong> Rantau oil field, N <strong>Sumatra</strong>. Discovered by BPM in 1929, 550 oil wells<br />

and recoverable reserves ~300 MMBO, most if which has been produced)<br />

Maryanto, S. (2001)- Stratigrafi cekungan Tersier Bengkulu: kaitannya dengan keterdapatan batubara. Geol.<br />

Res. Dev. Centre, Bandung, Spec. Publ. 26, p. 53-71.<br />

(‘Stratigraphy <strong>of</strong> the Bengkulu Basin and links with coal’. Late Miocene- Pliocene Simpangaur Fm important<br />

coal formation. Coalification due to Pliocene (~3.5 Ma) dacite intrusions. Coal seams 30 cm- 7m thick)<br />

Maryanto, S. (2002)- Stratigrafi formasi pembawa batubara Paleogen di Linggapura, Padangratu, Lampung. J.<br />

Geol. Sumberdaya Min. 12, 126, p. .<br />

('Stratigraphy <strong>of</strong> the Paleogene lower coal formation in Linggapura, Lampung', S <strong>Sumatra</strong>')<br />

Maryanto, S. (2005)- Sedimentology batuan karbonat Tersier, Formasi Baturaja, di lintasan Air Napalan,<br />

Baturaja, <strong>Sumatra</strong> Selatan. J. Sumber Daya Geol. (GRDC) 15, 1, p. 83-101.<br />

('Sedimentology <strong>of</strong> Tertiary Baturaja Fm carbonate at the Air Napalan section, S <strong>Sumatra</strong>')<br />

Maryanto, S. (2007)- Petrografi dan proses diagenesis batugamping Baturaja di lintasan Air Saka, OKU Selatan,<br />

<strong>Sumatra</strong> Selatan. J. Sumber Daya Geol. (GRDC) 17, 1, p.<br />

('Petrograpy and diagenetic processes <strong>of</strong> the Baturaja Fm limestone at the Air Saka section, S <strong>Sumatra</strong>')<br />

Maryanto, S. (2008)- Hubungan antarkomponen mikr<strong>of</strong>asies lereng Terumbu dan cekungan lokal terumbu<br />

belakang batugamping bioklastika Formasi Baturaja di daerah sekitar Muaradua, Sumatera Selatan. J. Sumber<br />

Daya Geol. (GRDC) 18, 2, p. 107-120.<br />

(Micr<strong>of</strong>acies <strong>of</strong> bioclastic Baturaja Limestone in Muaradua area, S <strong>Sumatra</strong>)<br />

Masturyono, R. McCaffrey, D.A. Wark, S.W. Roecker, Fauzi, G. Ibrahim & Sukhyar (2001)- Distribution <strong>of</strong><br />

magma beneath Toba Caldera, North <strong>Sumatra</strong>, <strong>Indonesia</strong>, constrained by 3-dimensional P-wave velocities,<br />

seismicity, and gravity data. Geochem., Geoph. & Geosyst. 2, 24 p.<br />

Matasak, T. & R. Kendarsi (1980)- Geologi endapan batubara di Bukit Asam, <strong>Sumatra</strong> Selatan. Bul. Dep.<br />

Geologi Inst. Tekn. Bandung 1, p. 11-33.<br />

(‘<strong>Geology</strong> <strong>of</strong> Bukit Asam coal deposits, S <strong>Sumatra</strong>')<br />

Matchette-Downes, C.J., A.E. Fallick, Karmajaya & S. Rowland (1994)- A maturity and paleoenvironmental<br />

assessment <strong>of</strong> condensates and oils from the North <strong>Sumatra</strong> Basin, <strong>Indonesia</strong>. In: A.C. Scott & A.J. Fleet (eds.)<br />

Coal and coal-bearing strata as oil-prone source rocks?, Geol. Soc., London, Spec. Publ. 77, p. 139-148.<br />

(Five light oils-condensates from wells in N <strong>Sumatra</strong> Basin. Source facies dominantly lacustrine with<br />

subordinate ombrogenous raised peat bog palaeoenvironments. Oils and condensates mature to extremely<br />

mature. Some oils mixtures <strong>of</strong> different maturities and discrete terrestrial sources)<br />

Matson, R.G. & G.F. Moore (1992)- Structural influences on Neogene subsidence in the Central <strong>Sumatra</strong> forearc<br />

basin. In: J.S. Watkins et al. (eds.) <strong>Geology</strong> and geophysics <strong>of</strong> continental margins. AAPG Mem. 53, p. 157-<br />

181.<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 63 www.vangorselslist.com July 2012

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