Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Harsa, A.E. & A. Kohar (1976)- Distribution of carbonate build-ups in Stanvacs South Sumatra Area. Proc.
Carbonate Seminar, Indonesian Petrol. Assoc., Spec. Vol., p. 116. (Abstract only)
Harsono, D. G.J. Manchester & R. Hanschitz (1989)- Arun field reservoir management, Sumatra. Proc. 18th
Ann. Conv. Indon. Petrol. Assoc. 2, p. 67-90.
Harting, A. (1930)- Verslag van een mijnbouwkundig-geologisch onderzoek in de omstreken van Tambang
Sawah in de jaran 1924-1927. Jaarboek Mijnwezen Nederl. Oost-Indie 58 (1929), Verhand., p. 229-264.
('Report of mining-geological survey in the region of Tambang Sawah in the years 1924-1927'. Investigation of
additional gold-silver prospects in Bengkulu region, but no prospective localities found. Area with presumably
Mesozoic granites, overlain by M-U Mioceneshales and sands, Late Miocene or Pliocene vlcanic breccias with
some coal and younger andesite-liparite volcanics. With 1:20,000 geologic map)
Hartanto, K., E. Widianto & Safrizal (1991)- Hydrocarbon prospect related to the local unconformities of the
Kuang Area, South Sumatra Basin. Proc. 20th Ann. Conv. Indon. Petrol. Assoc., 1, p. 17-35.
(Kuang area one of most stable parts of S Sumatra Basin. Three local unconformities: (1) vadose zone on top
Baturaja Fm, (2) turbidite sediments during sea level drop when Gumai Fm was deposited; (3) local
unconformity within Air Benakat Fm)
Hartmann, E. (1917)- Over de geologie van de Lampongsche Distrikten en het zuidelijk deel der residentie
Palembang, Zuid Sumatra. Jaarboek Mijnwezen Nederl. Oost-Indie 44 (1915), Verhand. 2, p. 90- 132.
(‘On the geology of the Lampung Districts and the southern part of the Palembang Residency, S Sumatra’
Results of 1915 reconnaissance. Pretertiary metamorphics and granites, overlain by folded ‘Eocene’ quartz
sandstones with coal, Oligocene Baturaja Limestone (few 100m thick; should be E Miocene age; HvG), 500m
or more marine Telisa/ Gumai clays, tuffs and limestones, 1000m of Miocene-Pliocene L-M Palembang clayssandstones
(rel. little coal in this area) and 500m Upper Palembang Fm quartz-rich tuffs. Overlain by unfolded
Quaternary conglomerates and volcanics)
Hartmann, E. (1921)- Geologisch rapport over het kolenvoorkomen in de mijnconcessies 'Soekamarinda' en
'Boenian' en het tusschen deze beide gelegen kolenveld 'Ajer Serillo', gelegen in de onderafdeeling Lematang
Oeloe, Residentie Palembang. Jaarboek Mijnwezen Nederl. Oost-Indie 47 (1918), Verhand. 2, p. 108- 140.
(Detailed study of Middle Palembang Fm coals in 3 mining concessions in Lematang Ulu area, Palembang
Residency, S Sumatra)
Hartanto, K., R. Djaafar & I. Yuswar (1990)- Evaluasi cekungan dengan metode restorasi dalam hubungannya
dengan akumulasi hidrokarbon di Tinggian Kuang, Sumatra Selatan. Proc. 19th Ann. Conv. Indon. Assoc. Geol.
(IAGI), 1, p. 264-291.
('Basin evaluation with restoration methods in relation with hydrocarbon accumulation in Tinggian Kuang, S
Sumatra')
Hartono, U. (2002)- Permian magmatism in Sumatra: their tectonic setting and magmatic source. J. Geol.
Sumberdaya Min. 12, 129, p.
Hartono, U., S. Andi Mangga & A. Achdan (1996)- Geochemical results of the Permian and Silungkang
volcanics, southern Sumatra. J. Geol. Sumberdaya Min. (GRDC Bandung), 5, 56, p. 18-24
Hasan, M.A., Kamal & F.B. Langitan (1977)- The discovery and development of the Minas Field. Proc. First
Ann. Conf. ASEAN Council on Petroleum, p. 323-345. (also in Oil and Gas J., 22 May 1978, p. 168-177)
Hasan, M.A., Kamal & F.B. Langitan (1978)- Discovery and development of the Minas Field. SEAPEX Proc.
4, Singapore 1977/78, p. 138-157.
Bibliography of Indonesia Geology v. 4.1 40 www.vangorselslist.com July 2012