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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Maubeuge, F. & I. Lerche (1994)- Geopressure evolution and hydrocarbon generation in a North <strong>Indonesia</strong>n<br />
basin: two dimensional quantitave modelling. Marine Petrol. Geol. 11, 1, p. 105-115.<br />
(Unnamed basin = ?)<br />
May, J.A. & D.R. Eyles (1985)- Well log and seismic character <strong>of</strong> Tertiary Terumbu carbonate, South China<br />
Sea, <strong>Indonesia</strong>. AAPG Bull. 69, 9, p. 1339-1358.<br />
Maynard, K. & I. Murray (2003)- One million years from the Upper Arang Formation, West <strong>Natuna</strong> Basin,<br />
Implications for reservoir distribution and facies variation in fluvial deltaic deposits. Proc. 29th Ann. Conv.<br />
Indon. Petrol. Assoc., 1, p. 270-276.<br />
(M Miocene Upper Arang Fm important reservoir, comprising fluvial deltaic deposits with gas sourced from<br />
interbedded coals. Periodic marine flooding events provide intra-formational seals. Series <strong>of</strong> horizon slices<br />
over a 1 million year time interval, at ~4,800’ illustrate major changes in reservoir distribution and facies.<br />
Lateral and vertical complexity <strong>of</strong> these reservoir not resolved by limited well penetrations)<br />
Maynard, K., W. Prabowo, J. Gunawan, C. Ways & R. Brotherton (2003)- Maximising the value <strong>of</strong> a mature<br />
asset, the Belida Field, West <strong>Natuna</strong>- can a detailed subsurface re-evaluation really add value late in field life?<br />
Proc. 29th Ann. Conv. Indon. Petrol. Assoc. 2, p. 291-305.<br />
(Belida Field 1989 discovery, EUR ~350 MMBO developed in 1992, with peak oil production <strong>of</strong> 135,000 bopd<br />
in 1994 from two fluvial deltaic sandstone reservoirs,E Miocene Lower Arang Fm and Oligocene Udang Fm)<br />
Maynard, K., P. Siregar & L. Andria (2002)- Seismic stratigraphic interpretation <strong>of</strong> a major 3D, the Gabus Subbasin,<br />
Blocks B and Tobong, West <strong>Natuna</strong> Sea, <strong>Indonesia</strong>: getting the geology back into seismic. Proc. 28th<br />
Ann. Conv. Indon. Petrol. Assoc. 1, p. 87-104.<br />
(Conoco 2000 large regional 3D survey in Gabus Sub-Basin, W <strong>Natuna</strong>. Interpretation focused on stratigraphy.<br />
Source rock distribution re-interpreted based on seismic facies)<br />
Meirita, M.F. (2003)- Structural and depositional evolution, KH Field, West <strong>Natuna</strong> Basin, Offshore <strong>Indonesia</strong>.<br />
M.Sc. Thesis Texas A&M University, 56p. (online at http://txspace.tamu.edu/..)<br />
(3D seismic study. KH structure formed by N-S trending Eo-Oligocene rifting, reactivated by E-M Miocene<br />
inversion)<br />
Michael, E. & H. Adrian (1996)- The petroleum systems <strong>of</strong> West Block B PSC, South <strong>Natuna</strong> Sea, <strong>Indonesia</strong>.<br />
Proc. 25 th Ann. Conv. Indon. Petrol. Assoc., p. 465-479.<br />
(Two petroleum systems in Conoco West Block 'B': (1) coals and coaly shales <strong>of</strong> Arang and Gabus Fms and (2)<br />
lacustrine synrift Belut/Gabus Fms. Synrift organic facies divided into "deep" lacustrine and shallow lacustrine.<br />
Early synrift sections expel as early as 29-19 Ma, shallower; more gas prone synrift sections expel from 26-12<br />
Ma and 23-0 Ma. Coals and coaly shales in Arang and Gabus expulsion below 7,500’ (0.7% Ro) suggesting<br />
charging from 8 Ma- present. Late formed traps (
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