Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
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MacGregor, D.S. & A.S. MacKenzie (1986)- Quantification <strong>of</strong> oil generation and migration in the Malacca<br />
Strait region Central <strong>Sumatra</strong>. Proc. 15th Ann. Conv. Indon. Petrol. Assoc., p. 303-320.<br />
Machali Muchsin, A., C.C. Johnson, M.J. Crow, A. Djumsari & Sumartono (1997)- Geochemical atlas <strong>of</strong><br />
Southern <strong>Sumatra</strong>. Regional geochemical atlas series <strong>of</strong> <strong>Indonesia</strong> 2, Direct. Miner. Res., Bandung, 63 p.<br />
(Distributions <strong>of</strong> 15 metals/ elements in 13,187 stream sediments from <strong>Sumatra</strong> S <strong>of</strong> the Equator)<br />
Madon, M. B. & M.B.Ahmad, (1999)- Basins in the Straits <strong>of</strong> Melaka. In: The Petroleum <strong>Geology</strong> and<br />
Resources <strong>of</strong> Malaysia, Petronas, Kuala Lumpur, p. 235-250.<br />
Maliki, M.A. & S. Soenarwi (1991)- South Lho Sukon-D1 discovery, North <strong>Sumatra</strong>. Proc. 20 th Ann. Conv.<br />
Indon. Petrol. Assoc., 1, p. 235-254.<br />
Malod, J. & B.M. Kemal (1996)- The <strong>Sumatra</strong> margin: oblique subduction and lateral displacement <strong>of</strong> the<br />
accretionary prism. In: R. Hall & D.J. Blundell (eds.) Tectonic Evolution <strong>of</strong> SE Asia. Geol. Soc. London, Spec.<br />
Publ. 106, p. 19-28.<br />
(Oblique convergence in <strong>Sumatra</strong> forearc partitioned into trench- perpendicular convergence and strike-slip<br />
parallel to trench. Strike-slip along two major faults, <strong>Sumatra</strong> and Mentawai FZ. Mentawai fault attenuated at<br />
N end, terminates in accretionary prism. It is relayed and connected to <strong>Sumatra</strong> fault. Pattern can be explained<br />
with two sliver plates, Mentawai and Aceh, on top <strong>of</strong> which forearc basin developed. Accretionary prism<br />
moving NW along Mentawai fault. No extension within Mentawai plate, suggesting uniform motion along<br />
<strong>Sumatra</strong> fault S <strong>of</strong> 3°N. Strike-slip along Mentawai fault explained by better coupling between subducting slab<br />
and upper plate beneath accretionary prism compared to forearc)<br />
Malod, J.A., B. M. Kemal, M.O. Beslier, C. Deplus, M. Diament et al. (1993)- Deformations du bassin davantarc<br />
au Nord-Ouest de <strong>Sumatra</strong>: une reponse a la subduction oblique. C. R. Acad. Sci. Paris 316, p. 791-797.<br />
(‘Deformation <strong>of</strong> the fore-arc basin NW <strong>of</strong> <strong>Sumatra</strong>; a response to oblique subduction’. NW <strong>Sumatra</strong> example<br />
<strong>of</strong> oblique convergence, expressed by two major strike-slip fault zones: <strong>Sumatra</strong> and Mentawai faults.<br />
Mentawai fault zone continues N-ward, and fore-arc basin segmented by strike-slip or compressional features)<br />
Manaf, N.A. & N. Mujahidin (1993)- Evaluasi migrasi hidrokarbon di sub cekungan Jambi berdasar<br />
pemelajaran biomarker dan sejarah tektoniknya. Proc 22nd Ann Conv Indon Assoc. Geol. (IAGI) 2, p. 736-746.<br />
(Evaluation <strong>of</strong> hydrocarbon migration in Jambi sub-basin, C <strong>Sumatra</strong>, using biomarkers)<br />
Mandre, D. (2000)- Coal geology <strong>of</strong> the Bengkulu Block. In: Proc. Southeast Coal <strong>Geology</strong> Conference,<br />
Directorate General <strong>of</strong> <strong>Geology</strong> and Mineral Res. <strong>Indonesia</strong>, Bandung, p.<br />
Mangold, K.M., Erlina & E.B. Hamzah (1992)- Critical aspects <strong>of</strong> 3-D seismic surveys for field development in<br />
Central <strong>Sumatra</strong>. Proc. 21st Ann. Conv. Indon. Petrol. Assoc.,1, p. 257-286.<br />
Mangunkusumo, R.I. (1982)- Infill drilling in old fields. In: SPE Offshore South East Asia Conf, Singapore<br />
1982, 16p.<br />
(On infill drilling program by Stanvac in Raja and Abab old oil fields, onshore S <strong>Sumatra</strong>, to identify and<br />
recover remaining oil not drained by existing wells. Original development on 80-acre spacing did not define all<br />
hydrocarbon bearing zones nor establish all drainage points in complex Talang Akar sandstone reservoirs)<br />
Mannhardt, F.G. (1921)- Verslag over de resultaten van geologisch- mijnbouwkundig onderzoek der Tandjoeng<br />
kolenvelden (Res. Palembang). Jaarboek Mijnwezen Nederl. Indie 47 (1918), Verh. 2, p. 67-107.<br />
(Investigation <strong>of</strong> S <strong>Sumatra</strong> Tanjung coal fields (including Bukit Asam), 13 km S <strong>of</strong> Muara Enim. Coal beds in<br />
700-800m thick Middle Palembang Fm. Coal grade locally improved by andesite intrusives)<br />
Manuyama, J.M.B., Nazirman & Haryoto (2004)- Characterization <strong>of</strong> reservoir carbonate and hydrocarbon<br />
potential Baturaja Formation on Nova structure, South <strong>Sumatra</strong>. Proc. 33 rd Ann. Conv. Indon. Assoc. Geol.<br />
(IAGI), p. 172-180.<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 61 www.vangorselslist.com July 2012