Salvador, P., W.R. Morris, R.J. Morley, M. Gunarto, R. Adhyaksawan & M. Challis (2008)- Managing reservoir uncertainty at the North Belut Field, Offshore <strong>Indonesia</strong>, <strong>Natuna</strong> Sea: an integrated analysis <strong>of</strong> biostratigraphy, core, wireline and seismic data. Proc. 32 nd Ann. Conv. Indon. Petrol. Assoc., IPA08-G-205, 14p. (Reservoir study <strong>of</strong> North Belut gas field in Udang and Gabus sands. 1500 ft section <strong>of</strong> thin, stacked lacustrine and deltaic sands with significant variation in vertical and lateral reservoir development) Sangree, J.B. (1981)- Use <strong>of</strong> seismic stratigraphy in carbonate rocks, <strong>Natuna</strong> D-Alpha Block Example. Proc. 10th Ann. Conv. Indon. Petrol. Assoc., p. 135-152. (<strong>Natuna</strong> D-Alpha "L" structure large Late Miocene reef complex, 5,250’ gas column, 67%- 82%CO2. Arang Fm considered source <strong>of</strong> methane; CO2 believed to be from deep igneous activity. E-M Miocene Arang and Barat-Gabus shale widespread and uniform thickness, suggesting stable nonmarine-shallow marine shelf conditions. Post-Arang normal faulting resulted in rotation and faulting <strong>of</strong> "L" structure and Terumbu (U Miocene) carbonate development Further downfaulting in Lt Miocene- E Pliocene resulted in widespread carbonate deposits with local reef development on W shelf area and local buildups on crest <strong>of</strong> 'L' structure) Satriawan, R.W., T. Read & H. Baskara (2005)- Applying seismic attribute analysis and inversion techniques to understand the trapping mechanism in the Gajah Abu Abu Field, West <strong>Natuna</strong> Offshore. Proc. 30 th Ann. Conv. Indon. Petrol. Assoc., 1, p. 135- 144. (Gajah Abu Abu field in W <strong>Natuna</strong> Basin 1992 discovery in faulted Late Miocene inversion anticline. Significant stratigraphic component in Gajah Abu Abu trap) Subono, S, Siswoyo & A. Firman (1995)- Heat flow in border areas <strong>of</strong> <strong>Indonesia</strong>, Malaysia and Vietnam. In: J. Ringis (ed.) Proc. 31st Sess. Comm. Co ord. Joint Prospecting Min. Res. Asian Offshore Areas (CCOP), Kuala Lumpur 1994, 2, p. 59-75. (Mainly on heatflow from 46 wells in West and 24 wells in East <strong>Natuna</strong> basins. Av. T gradient 39.7 °C/km) Sugihardjo, S.S. Aprilian, A. Yusuf & S Sumardan (2000)- Investigations <strong>of</strong> the storage efficiency <strong>of</strong> CO2 in carbonate aquifers. Proc. 27th Ann. Conv. Indon. Petrol. Assoc., 2, p. 79-93. Suryono, N. (1997)- Analisa struktur P. Laut dan P. Sekatung, Kepulauan <strong>Natuna</strong> besar. J. Geol. Sumberdaya Min. 7, 74, p. 2-24. ('Analysis <strong>of</strong> the structure <strong>of</strong> the Laut and Sekatung islands, <strong>Natuna</strong> Besar island group') Sutoto, A. (1991)- Reservoir geology <strong>of</strong> the Belida Field South <strong>Natuna</strong> Sea, Block B. Proc. 20th Ann. Conv. Indon. Petrol. Assoc., 1, p. 453-478. (1989 Conoco Belida oil field with 187 MBO and 130 BCF gas. Trap four-way closure, a structural inversion <strong>of</strong> half-graben during E Miocene (later?; HvG) regional compression. Age <strong>of</strong> sediments over Cretaceous granite Oligocene- Holocene. Oil reservoirs Oligocene Udang and E Miocene Lower Arang Sands, gas in E Miocene Arang Fm. Udang Fm sands stacked fluvial channels, Lower Arang sands distributary mouth bars in progadational lacustrine delta. Good vertical and lateral reservoir continuity. Sands ~30% porosity) Thamrin, M., Prayitno, S. Tiwar & Solichin (1983)- Heatflow investigation in the Tertiary basins <strong>of</strong> <strong>Natuna</strong> Sea. Proc. 19 th Sess. CCOP, Tokyo 1982, 2, Techn. Repts., p. 153-166. (Heatflow data from 29 wells in <strong>Indonesia</strong>n sector <strong>of</strong> <strong>Natuna</strong> Sea. Heatflow in W area <strong>of</strong> <strong>Natuna</strong> Arch (av. 2.03 HFU, T gradient av. 3.45 248 °C/100m) higher than in E (av. 1.59 HFU, T gradient av. 3.36 °C/100m)) Tjia, H.D. (1997)- Regional northwest to west-northwest lineaments in the southern part <strong>of</strong> the South China Sea Basin. Warta Geologi, Geol. Soc. Malaysia Newsl. 23, 5, p. 297-302. Van Mechelen, G., J. Meyer & R. Gir (1998)- Correlation mapping technique, a powerful tool to minimize risk and to guide future development plans. Proc. 26th Ann. Conv. Indon. Petrol. Assoc., p. 175-196. (Geophysical study over two gas fields in W <strong>Natuna</strong> Basin) <strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 151 www.vangorselslist.com July 2012
Wagimin, N. & E.A. Sentani (2009)- Opportunities (II), East <strong>Natuna</strong> area. Inameta J. 7, p. 24-27. (online at: www.patranusa.com) (Brief overview <strong>of</strong> E <strong>Natuna</strong> Basin, in conjunction with tender round <strong>of</strong>fering) Wirojudo, G.K. & A. Wongsosantiko (1985)- Tertiary tectonic evolution and related hydrocarbon potential in the <strong>Natuna</strong> area. Energy 10, 3/4, p. 433-455. Wongkosantiko, A. & P. Prijosoesilo (1995)- Geologic summary <strong>of</strong> the <strong>Natuna</strong> Sea. In: Seismic Atlas <strong>of</strong> <strong>Indonesia</strong>n Oil and Gas Fields, II: Java, Kalimantan, <strong>Natuna</strong>, Irian Jaya, Indon. Petrol. Assoc., Jakarta, 6p. Wongkosantiko, A. & G.K. Wirojudo (1984)- Tertiary tectonic evolution and related hydrocarbon potential in the <strong>Natuna</strong> area. Proc. 13 th Ann. Conv. Indon. Petrol. Assoc., p. 161-183. (W and E <strong>Natuna</strong> Basins separated by N-S trending <strong>Natuna</strong> basement Arch. W <strong>Natuna</strong> Basin started in E Oligocene by rifting/ pull-apart, producing SW-NE half-grabens filled with non-marine sediments. Extension in W <strong>Natuna</strong> little effect on E <strong>Natuna</strong> Basin, where Oligocene sediments more uniform thickness. Compressive forces started in W <strong>Natuna</strong> in E Miocene, resulting in inversions <strong>of</strong> former half grabens) <strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 152 www.vangorselslist.com July 2012
- Page 1 and 2:
BIBLIOGRAPHY OF THE GEOLOGY OF INDO
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A widespread Plio-Pleistocene compr
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II.3. Natuna The Natuna area forms
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(Broad Oligo-Miocene paleogeographi
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Amin, T.C., Kusnama, E. Rustandi &
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(Pertamina operates 55 mature oil f
- Page 13 and 14:
Barber, A.J. & M.J. Crow (2008)- Th
- Page 15 and 16:
Beauvais, L. (1985)- Donnees nouvel
- Page 17 and 18:
Berglar, K., C. Gaedicke, R. Lutz,
- Page 19 and 20:
('Contribution to the geology of th
- Page 21 and 22:
Sumatra volcanic arc activity, with
- Page 23 and 24:
Clarke, M.C.G., S.A. Ghazali, H. Ha
- Page 25 and 26:
(Heat flow in Central Sumatra basin
- Page 27 and 28:
De Neve, G.A. (1961)- Mesozoic orog
- Page 29 and 30:
Durham, J.W. (1940)- Triassic fossi
- Page 31 and 32:
Feriyanto, F. Kamil, Y. Kusnandar &
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(Middle Permian of Padang Highlands
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Triassic tin-granites on Bangka-Bel
- Page 37 and 38:
Guntoro, A. & Y.S. Djajadiharja (20
- Page 39 and 40:
Recent syn-orogenic megasequence, f
- Page 41 and 42:
Harsa, A.E. & A. Kohar (1976)- Dist
- Page 43 and 44:
egional dextral wrenching; F3- M Mi
- Page 45 and 46:
Heryanto, R. (2007)- Kemungkinan ke
- Page 47 and 48:
Hopper, R.H. (1976)- The discovery
- Page 49 and 50:
(‘On Tertiary and Quaternary depo
- Page 51 and 52:
Kadir, W.G.A., S. Sukmono, M.T. Zen
- Page 53 and 54:
(Radiometric age dates from Sumatra
- Page 55 and 56:
Kingston, J. (1978)- Oil and gas ge
- Page 57 and 58:
trench slope break defines landward
- Page 59 and 60:
Lambrecht, K. (1931)- Protoplotus b
- Page 61 and 62:
Lismawaty, K. Simanjuntak & A. Bach
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(Nova field in Baturaja Limestone i
- Page 65 and 66:
(C Sumatra fore-arc Singkel and Pin
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Mertosono, S. & G.A.S. Nayoan (1974
- Page 69 and 70:
Moore, G.F. & J.R. Curray (1980)- S
- Page 71 and 72:
(M Miocene (N13-N14) sandstone in m
- Page 73 and 74:
('Critical notes on the origin and
- Page 75 and 76:
Nishimura, S., J. Nishida, T. Yokoy
- Page 77 and 78:
along SFS. Sumatran magmatic arc co
- Page 79 and 80:
Philippi, H. (1923)- Contributions
- Page 81 and 82:
Pudjowalujo, H. (1990)- Cenozoic te
- Page 83 and 84:
groups: marine, lacustrine, deltaic
- Page 85 and 86:
(Petapahan 1971 oil discovery 60km
- Page 87 and 88:
Samuel, M.A. (1994)- The structural
- Page 89 and 90:
Schlueter, H.U., C. Gaedicke, H.A.
- Page 91 and 92:
('Revision of Pre-Tertiary foramini
- Page 93 and 94:
Situmorang, B., B. Yulihanto, S. So
- Page 95 and 96:
(Structure and stratigraphy of tren
- Page 97 and 98:
Sukanta, U., Yarmanto, A. Susianto
- Page 99 and 100:
Suryono & M.C.G. Clarke (1982)- Pri
- Page 101 and 102: Suwarna, N. (2006)- Permian Mengkar
- Page 103 and 104: Tan Sin Hok (1936)- Bemerkungen ube
- Page 105 and 106: Thompson, M. L. (1936)- The fusulin
- Page 107 and 108: Tobler, A. (1922)- Djambi verslag.
- Page 109 and 110: Deposition in semi-enclosed valleys
- Page 111 and 112: Van Dijk, P. (1875)- Zwartkolen in
- Page 113 and 114: Van Waveren I. M., F. Hasibuan, Suy
- Page 115 and 116: Verbeek, R.D.M., O. Boettger & K. v
- Page 117 and 118: Vozenin-Serra, C. (1989)- Lower Per
- Page 119 and 120: Whitten, A.J., S.J. Damanik, J. Anw
- Page 121 and 122: Wisnu, A. & Nazirman (1997)- Statis
- Page 123 and 124: Yulihanto, B., B. Situmorang, A. Nu
- Page 125 and 126: Zulkarnain, I. (2007)- Variasi geok
- Page 127 and 128: II.2. Sunda Shelf (incl. 'Tin islan
- Page 129 and 130: Bothe, A.C.D. (1925)- Het voorkomen
- Page 131 and 132: Groothoff, C.T. (1916)- Eenige merk
- Page 133 and 134: Houtz, R.E. & D.E. Hayes (1984)- Se
- Page 135 and 136: Lehmann, B. & Harmanto (1990)- Larg
- Page 137 and 138: Ronojudo, A. (1972)- Offshore explo
- Page 139 and 140: (Rare, probably Early Permian age c
- Page 141 and 142: Van Overeem, A.J.A. (1960)- The geo
- Page 143 and 144: Wisoko (1983)- Pengaruh kipas aluvi
- Page 145 and 146: Burton, D. & L.J. Wood (2010)- Inte
- Page 147 and 148: elatively small, 1-2 km in Cumi-Cum
- Page 149 and 150: Maubeuge, F. & I. Lerche (1994)- Ge
- Page 151: (W Natuna Tertiary 3-4 megasequence