Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

II.3. Natuna, Anambas
Adrian, H., L. Andria & A. Sudarsana (2005)- Horizontal well placements using V shale and facies geomodel:
an example from Belanak Field, South Natuna Sea, Indonesia. Proc. 30 th Ann. Conv. Indon. Petrol. Assoc., 1, p.
145-162.
(Main reservoirs in Belanak Field, S Natuna Sea Block ‘B’ are U Oligocene Gabus Massive Sand and Gabus
Zone-3. Massive Sand gas with thin oil rim, deposited in a fluvial channel environment. Multi-storied channel
sands. Porosity ranges similar throughout field, but permeabilities are variable)
Alyadrus, M.A. & R.L. Coates (1990)- Successful marginal feld development, Ikan Pari Field, Natuna Sea.
Proc. 19th Ann. Conv. Indon. Petrol. Assoc., p. 345-351.
(Ikan Pari Field, discovered in 1983, 50 miles NE of Udang Field. Developed with four seafloor completions)
Bachtel, S.L., R.D. Kissling, D. Martono, S.P. Rahardjanto, P. Dunn & B.A. MacDonald (2004)- Seismic
stratigraphic evolution of the Miocene-Pliocene Segitiga platform, East Natuna Sea, Indonesia: the origin,
growth, and demise of an isolated carbonate platform. In: G. Eberli et al. (eds.) Seismic imaging of carbonate
reservoirs and systems, AAPG Mem. 81, p. 309-328.
(High-res 2D seismic survey over Segitiga Platform (1400 km2), E Natuna-Sarawak Sea. Terumbu Fm
carbonate up to 1800 m thick, subdivided into 12 seismic sequences, showing (1) initial isolation; (2)
progradation /coalescence; (3) backstepping; (4) terminal drowning. Platform originated as 3 smaller
platforms on highs, separated by deep intraplatform seaways. Three platforms merged into composite platform
in M-U Miocene. Rapid end Miocene sea level riset caused major backstepping of carbonate margins (and
drowning of Natuna field carbonate platform to E) resulting in smaller platform in Lower Pliocene. Rapid
subsidence at end of E Pliocene, caused terminal drowning)
Ben-Brahmin, L. et al. (1999)- Characterization of seismic anomalies using converted waves: a case of history
from East Natuna Basin. Proc. 27th Ann. Conv. Indon. Petrol. Assoc., p. 295-302.
Bennett, M. (1999)- Intra-Muda shallow gas in Cumi-Cumi PSC, Natuna Sea- a driller's nightmare becomes a
geophysicist's dream. Proc. 27th Ann. Conv. Indon. Petrol. Assoc., p. 303-321.
(M Miocene age Intra-Muda Fm. sandstones draped over inversion feature. Strong seismic amplitude anomaly
over crest, with 'flatspots' around flanks of structure and gas-charged in Tenggiri 1 and Mako 1 wells)
Bhikuningputra, D. (1986)- Seismic stratigraphic study to evaluate reservoirs and seals of the Natuna area. In:
Seismic Stratigraphy I, Proc. Joint ASCOPE/ CCOP Workshop, Jakarta 1986.CCOP Tech. Publ. 17, p. 157-180.
Bothe, A.C. (1928)- Geologische verkenningen in den Riouw-Lingga archipel en de eilandengroep der Poelau
Toedjoeh (Anambas- en Natoena-eilanden). Jaarboek Mijnwezen Nederl. Oost-Indie 54 (1925), Verh. 2, p. 101-
152.
(Geological reconnaissance surveys of Riau Archipelago (common granites), Anambas Islands (mainly
granites) and Natuna islands (metamorphic rocks, possibly Jurassic radiolarian chert, serpentinites, granites))
Budiyono (2002)- Forel field reservoir characterization and field assessment, West Natuna Basin Indonesia.
M.Sc. Thesis Univ. Texas, Austin, p. (Unpublished)
Burton, D. & L.J. Wood (2010)- Seismic geomorphology and tectonostratigraphic fill of half grabens, West
Natuna Basin, Indonesia. AAPG Bull. 94, 11, p. 1695-1712.
(Study of Eo-Oligocene synrift architectures of Cenozoic grabens in W Natuna Basin (WNB) from Gabus and
Belanak 3D seismic surveys. Five facies: fluvial, deltaic, alluvial fan, shallow lacustrine and deep lacustrine.
Synrift stratigraphy shows strong tectonic control. Hydrocarbon in basin restricted to upper synrift- postrift
reservoirs in M Miocene inversion anticlines, but synrift may have potential)
Bibliography of Indonesia Geology v. 4.1 143 www.vangorselslist.com July 2012