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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Heryanto, R. (2007)- Kemungkinan keterdapatan hidrokarbon di Cekungan Bengkulu. Jurnal Geol. <strong>Indonesia</strong>,<br />
2, 3, p. 119-131.<br />
('Hydrocarbon potential <strong>of</strong> the Bengkulu basin')<br />
Heryanto, R. & H. Hermiyanto (2006)- Potensi batuan sumber (source rock) hidrokarbon di Pegunungan<br />
Tigapuluh, Sumatera Tengah. Jurnal Geol. <strong>Indonesia</strong> 1, 1, p. 37-48.<br />
('Hydrocarbon source rock potential in the Tigapuluh Mts, C <strong>Sumatra</strong>'. Source rocks S <strong>of</strong> C <strong>Sumatra</strong> Basin<br />
margin fine grained clastics in Late Eocene Kelesa and Oligocene Lakat Fms. Kelesa Fm TOC 2.3-9.6%, Lakat<br />
Fm TOC 0.7-3.5%, Thermal maturation <strong>of</strong> Kelesa Fm late immature- early mature, kerogen types I and II,<br />
Lakat Fm late immature, kerogen types I, II, and III)<br />
Heryanto, R. & K.D. Kusamah (2001)- Sedimentasi batuan pembawa-batubara Formasi Talang Akar di daerah<br />
Lubuk Madrasah, sub-cekungan Jambi. In: Geologi formasi pembawa batubara di beberapa Cekungan Tersier<br />
<strong>Indonesia</strong>, Geol. Res. Dev. Centre, Bandung, Spec. Publ. 26, p. 99-114.<br />
(On the E Miocene fluvio-deltaic coal-bearing Talang Akar Fm in W part Jambi basin)<br />
Heryanto, R. & H. Panggabean (2006)- The Tertiary source rock potential <strong>of</strong> the Bengkulu Basin. Proc. Jakarta<br />
2006 Int. Geosc. Conf. Exhib., Indon. Petrol. Assoc., Jakarta06-PG-26, 4p.<br />
(Bengkulu forearc basin in SW <strong>Sumatra</strong> intiated in Eocene-Oligocene with deposition <strong>of</strong> Lahat equivalent Fm,<br />
unconformably overlain by Oligo Miocene Hulusimpang Fm volcanics, E-M Miocene Seblat Fm siliciclastics<br />
and carbonates, M-L Miocene Lemau Fm, etc. Geochemical analysis <strong>of</strong> outcrop, well samples and oil seeps<br />
identified organic matter <strong>of</strong> terrestrial origin. Best potential source rocks in Lemau Fm, although these are<br />
immature and oil seeps were derived from a mature source rock)<br />
Heryanto, R., N. Suwarna, & H. Panggabean (2001)- The Lakat Formation in the Northeastern flank <strong>of</strong> the<br />
Tigapuluh Mountains and its possibilities as a source rock. Proc. 30 th Ann. Conv. Indon. Assoc. Geol. (IAGI)<br />
and 10th GEOSEA Reg. Congr., p.<br />
Heryanto, R., N. Suwarna & H. Panggabean (2004)- Hydrocarbon source rock potential <strong>of</strong> the Eocene-<br />
Oligocene Keruh Formation in the Southwestern margin <strong>of</strong> the Central Sumatera Basin. J. Sumber Daya Geol.<br />
(J. Geol. Resources) 14, 3, p. 118-133.<br />
Heryanto, R. & Suyoko (2007)- Karakteristik batubara di Cekungan Bengkulu. Jurnal Geol. <strong>Indonesia</strong> 2, 4, p.<br />
247-259. (Online at http://www.bgl.esdm.go.id/dmdocuments/jurnal20070405.pdf)<br />
('Characteristics <strong>of</strong> coal in the Bengkulu Basin')<br />
Hestu S.N., Joan C.T., F. Asrul, E. Wijayati, S. Pujiastuti & T. Iswachyono (2010)- Tight carbonate platform: a<br />
new opportunity reservoir in Musi Platform a case study <strong>of</strong> Naya F4 well. Proc. 39th Conv. Indon. Assoc. Geol.<br />
(IAGI), Lombok, PIT-IAGI-2010-172, 7p.<br />
(On oil-bearing, but tight platform carbonate in 2008 Naya F4 well at NE flank <strong>of</strong> 'Naya field' buildup, SW<br />
<strong>Sumatra</strong> basin (probably not real field name; map looks like Soka field; HvG))<br />
Heyde, I., M. Block, Y.S. Djajadihardja, J.P. Hutagaol, H. Lelgemann, H.A. Roeser & B. Schreckenberger<br />
(2001)- Gravimetric measurements and their interpretation on the active convergence zone between the East<br />
Eurasian and Indo-Australian plates along <strong>Indonesia</strong>. In: Proc. CCOP 37th Ann. Sess. Bangkok 2000, 2, Techn.<br />
Repts., p. 12-26.<br />
(Free air gravity anomaly maps <strong>of</strong> forearc <strong>of</strong> SW <strong>Sumatra</strong>- W Java and <strong>Sunda</strong> Straits and comparison with<br />
satellite gravity. Marine gravity data higher resolution than satellite data)<br />
Hickman, R.G., P.F. Dobson, M. van Gerven, B.D. Sagala & R.P. Gunderson (2004)- Tectonic and stratigraphic<br />
evolution <strong>of</strong> the Sarulla graben geothermal area, North <strong>Sumatra</strong>, <strong>Indonesia</strong>. J. Asian Earth Sci. 23, p. 435-448.<br />
(Sarulla graben Plio-Pleistocene basin along <strong>Sumatra</strong> fault, where fault coincides with volcanic arc. Offset <strong>of</strong><br />
0.27 Ma rhyodacite dome by strand <strong>of</strong> <strong>Sumatra</strong> fault indicates ~9 mm/y slip, lower than previous estimates <strong>of</strong><br />
~25-30 mm/y for Holocene slip on <strong>Sumatra</strong> fault determined from stream <strong>of</strong>fsets. Discrepancy may be due to (1)<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 44 www.vangorselslist.com July 2012