Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Recent syn-orogenic megasequence, from main Barisan Mts uplift. Basin inversion intensity increases from
offshore to mountain belt. Fore-arc tectonically heterogeneous with potential for localised Paleogene and early
Neogene basins and hydrocarbons. Wells indicate mature source and migrated hydrocarbons, and contradict
assumption that heat flow in fore-arc areas is insufficient to allow expulsion and migration of hydrocarbons)
Hambali, H. & P. Dolan (1990)- Melibur Field: an integrated approach to reservoir development. Proc. 19 th
Ann. Conv. Indon. Petrol. Assoc., p. 141-154.
Hananto, N.D., S.C. Singh, M. Mukti & I. Deighton (2012)- Neotectonics of North Sumatra Forearc Proc. 36th
Ann.Conv. Indon. Petrol. Assoc. IPA, Jakarta, IPA12-G-100, p. 1-13.
Handayani, R.S.W., D. Setiawan & T. Afandi (2008)- Reservoir characterization of thin oil columns to improve
development drilling in a carbonate reservoir: case study of Gunung Kembang Field. Proc. 32 nd Ann. Conv.
Indon. Petrol. Assoc., IPA08-E-160, 15p.
(Medco Gunung Kembang field in anticlinal structure in E Miocene Baturaja platform carbonate on Musi
Platform, S Sumatra. Oil column 40', gas cap 120' thick. Cumulative oil production since 1988: 3.8 MMBO)
Hanus, V., A. Spicak & J. Vanek (1996)- Sumatran segment of the Indonesian subduction zone: morphology of
the Wadati-Benioff zone and seismotectonic pattern of the continental wedge. J. Southeast Asian Earth Sci. 13,
1, p. 39-60.
(Earthquake foci in Sumatra either in recent Benioff zone or in continental wedge. Intermediate-depth aseismic
gap in Wadati-Benioff zone associated with young calc-alkaline volcanism. Subduction process was correlated
with stratigraphy and geology. Duration of present cycle of subduction ~6-8 Ma. Oligocene volcanism and deep
earthquakes point to Tertiary subduction zone underlying present slab. Seismotectonic pattern of continental
wedge described by 11 seismically active fracture zones)
Hanzawa, S. (1947)- Note on some species of Pseudocyclammina from Sumatra. Japan J. Geol. Geogr. 20, 2-4,
p. 5-8.
(Fontaine et al. 1983: Upper Jurassic or Lower Cretaceous Pseudocyclammina from Gumai Mountains and
deep well in Kikim oilfield near Gumai Mts.)
Harahap, B.H. (2006)- Petrology of the Upper Miocene volcanic rocks on the western Barisan Mountain
Ranges, Lubuk Sikaping region, West Sumatera. Bul. Geologi (ITB) 38, 3, p. 81-108.
Harahap, B.H. (2007)- Petrologi batuan magmatis Neogen daerah Pangkalan Kotabaru Limapuluh kota,
Sumatera Barat. Jurn. Sumber daya Geol. (GRDC, Bandung) 17, 4, p. 207-217.
('Petrology of Neogene magmatic rocks in Pangkalan Kotabaru region, W Sumatra'. Andesites- dacites are
related to subduction)
Harahap, B.H. (2010)- Ciri geokimia batuan vulkaniklastika di daerah Tanjung Balit, Sumatra Barat: suatu
indikasi kegiatan magma pada Eosen. J. Geol. Indonesia 5, 2, p. 75-91.
(online at: http://www.bgl.esdm.go.id/publication/index.php/dir/article_detail/266)
('Geochemical characteristics of volcanoclastic rocks in the Tunjung Balit area, W Sumatra: some indications
of magmatic activity in the Eocene'. Chemistry of ?Eocene red mudstones overlying Permian Kuantan Fm in
Barisan Mts suggests altered volcanoclastic origin)
Harahap, B.H. (2011)- Magma genesis in Kabanjahe region continental margin arc of Sumatra. J. Geol.
Indonesia 6, 2, p. 105-127.
(Volcanic rocks in Kabanjahe area, N Sumatra Province, are products of old Toba Caldera, Sibayak Volcano,
and Sipiso-piso Volcano. Rhyolitic tuff most common, also basalt, andesite, dacitic, rhyolite. Rocks originated
from magma of continental origin formed at subduction zone environment)
Harahap, B.H. & Z.A. Abidin (2007)- Petrology of lava from Maninjau Lake, West Sumatera. Jurn. Sumber
daya Geol. (GRDC, Bandung) 16, 6, p. 359-370.
Bibliography of Indonesia Geology v. 4.1 38 www.vangorselslist.com July 2012