Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Amin, T.C., Kusnama, E. Rustandi & S. Gafoer (1993)- Geological map of the Manna and Enggano Sheet,
Sumatra, 1:250,000. Geol. Res. Dev. Centre, Bandung.
(Incl. fission track age of granite near Tanjungsakti of 9.53 +/- 0.55 Ma)
Amin, T.C., Sidarto, S. Santosa & W. Gunawan (1994)- Geology of the Kotaagung Quadrangle, Sumatra. Geol.
Res. Dev. Centre, Bandung, p.
Amir, V., R. Achdiat, M. Meirita & J. Guttormsen (2011)- Facies architecture and depositional relationship of
Baturaja carbonates in Letang, Rawa, and Tengah fields, Corridor Block, South Sumatra. Proc. 35 th Ann. Conv.
Indon. Petrol. Assoc., IPA11-G-090, p. 1-14.
(Letang, Rawa and Tengah eqarly 1990’s gas discoveries in Corridor Block E Miocene Baturaja Fm carbonate
buildups. Two main carbonate facies, muddy platform facies and coral-algal reefal buildup facies. Build-up
facies commonly developed above paleo-highs. Most porosity secondary vuggy and mouldic in leached coralalgal
framework. Carbonate platforms separated by deep NW-SE intra-platform channels. Karstification effect
related episodes predominantly developed in upper interval)
Amlan, M.H, Hendar S.M., Yarmanto & I.A. Muswar (2006)- Influence of strike-slip fault in structural
deformation of Asih and Asih North fields, Central Sumatra basin. Proc. 35th Ann. Conv. Indon. Assoc. Geol.
(IAGI), Pekanbaru, PITIAGI2006-048, 10p.
(Asih and Asih North two structural oil fields along N-S strike slip fault, about 30 km from Minas Field.
Remapping of Bekasap and Menggala Fm with 3D seismic. Left-stepping en echelon folds and faults represent
flower structure formed by NNW-SSE movement along older weak zone or ‘suture’ after SW-NE compression)
Anderson, B.L., J. Bon & H.E. Wahono (1993)- Reassessment of the Miocene stratigraphy, paleogeography and
petroleum geochemistry of the Langsa Block in the offshore North Sumatra Basin. Proc. 22nd Ann. Conv.
Indon. Petrol. Assoc. 1, p. 169-189.
(Langsa Block Miocene series of multicycles related to tectonic phases. Each multicycle several cycles: 4 in B,
5 in C. Multicycle A not penetrated, but interpreted on seismic. Paleogeographic reconstructions basis for
interpretation of source rock distribution. Two source rock types: (1) algal, probably lacustrine (initial A-
Multicycle) and (2) mixed marine algal/terrestrial (later A-Multicycle). Younger source rocks (B and C-
Multicycles) also identified but no oils typed to these. Oil generation started at beginning of Miocene in deepest
grabens and still continues on graben margin. Gas generation started in Late Miocene in most basinal areas)
Andi Mangga, S., Amiruddin, T. Suwarti, S. Gafoer & Sidarto (1994)- Geology of the Tanjungkarang
Quadrangle, Sumatra (1:250,000). Geol. Res. Dev. Centre, Bandung, p.
(SE Sumatra map sheet. With a.o. occurrence of Paleozoic? metamorphics (Gunung Kasih complex) and
Menanga Fm mid-Cretacous sediments with Orbitolina, interbedded with basalts and arc volcanics. Associated
amphibolite schist 125-108 Ma)
Andi Mangga, S., S. Gafoer & N. Suwarna (1987)- Hubungan geologi antara Kepulauan Mentawai dan dataran
Sumatra bagian Selatan.. Proc. 16th Ann. Conv. Indon. Assoc. Geol. (IAGI), p.
('Geological relationships between the Mentawai islands and S Sumatra')
Andi Mangga, S., Kusnama & Suryono (2006)- Stratigraphy and tectonic development of Mentawai island,
West Sumatra, based on plate tectonic theory. J. Sumberdaya Geol. (GRDC) 16, 3, p. 136-143.
Andi Mangga, S., K. Sutisna & Suminto (1996)- Karakteristik batuan klastika Formasi Peneta dan kaitannya
dengan indikasi minyak dan gas bumi. J. Geol. Sumberdaya Min. (GRDC) 6, 52, p. 1-11.
('Characteristics of the Peneta Fm clastics and its relation to oil and gas indications'. Late Jurassic- Early
Cretaceous, NW side of S Sumatra basin)
Andi Mangga, S., Suminto, Suyoko & K. Sutisna (1996)- Lingkungan tektonik formasi Mengkarang di daerah
Dusunbaru, Jambi. J. Geol. Sumberdaya Min. 6, 60, p. 16-20.
Bibliography of Indonesia Geology v. 4.1 8 www.vangorselslist.com July 2012