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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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(online at: http://www.iagi.or.id/fosi/bs20-sumatra.html. Ombilin Basin E Miocene intertidal beach sediments<br />

<strong>of</strong> Sawahlunto Fm with tracks <strong>of</strong> two different types <strong>of</strong> shorebirds. Represent first discovery <strong>of</strong> bird footprint<br />

fossils in <strong>Indonesia</strong>)<br />

Zeliff, C.W. & D. Bastian (2000)- New play in a mature basin: prospecting for gas. AAPG Int. Conf and Exhib.,<br />

Bali 2000, AAPG Bull. 84, 9 (Abstract only)<br />

(Dayung-1 1991 wildcat well, S <strong>Sumatra</strong> tested gas in fractured pre-Tertiary granite wash and granite. Since<br />

Dayung, Gulf discovered 8 gas fields where basement rocks represent primary reservoir)<br />

Zeliff, C.W., S.W. Trollope & E. Maulana (1985)- Exploration cycles in the Corridor Block, South <strong>Sumatra</strong>.<br />

Proc. 14th Ann. Conv. Indon. Petrol. Assoc., 1, p. 379-400.<br />

(Corridor area in S <strong>Sumatra</strong> several cycles <strong>of</strong> petroleum exploration. Exploration by BPM (Shell) in early<br />

1890's, resulted in several small, shallow oil fields. Second cycle concentrating on deep Talang Akar prospects<br />

through 1930's terminated by World War II. Low level <strong>of</strong> activity post World War II through late 1960's.<br />

Modern exploration cycle initiated by Stanvac in 1971 and Asamera after 1980, with Tanjung Laban and<br />

Ramba fields discoveries in 1982).<br />

Zen, M.T. (1970)- Origin <strong>of</strong> Lake Singkarak in the Padang Highlands (Central <strong>Sumatra</strong>). Inst. Tekn. Bandung<br />

J. Science 5, 1, p. 1-8.<br />

(Lake Singkarak in Padang Highlands previously interpreted as volcanic caldera, but Singkarak Trough is<br />

fault-bounded depression, and part <strong>of</strong> <strong>Sumatra</strong> Rift zone, stretching for 1650 km from <strong>Sumatra</strong>’s N tip to<br />

Semangko valley in SE, and already identified by Westerveld (1952), Katili (1967), etc.)<br />

Zen, M.T. (1983)- Krakatau and the tectonic importance <strong>of</strong> <strong>Sunda</strong> Strait. Bull. Jurusan Geol., 12, p. 9-22.<br />

Zen, M.T. (1989)- Seismicity <strong>of</strong> the <strong>Sumatra</strong> fault zones. In: B. Situmorang (ed.) Proc. 6th Reg. Conf. <strong>Geology</strong><br />

Mineral Hydrocarbon Res. Southeast Asia, Jakarta 1987, IAGI, p. 197-205.<br />

(Earthquakes in W <strong>Sumatra</strong> either shallow and related to subduction or related to right-lateral <strong>Sumatra</strong> Fault)<br />

Zen, M.T. (1993)- Deformation de l'avant-arc en reponse a une subduction a convergence oblique. Exemple de<br />

<strong>Sumatra</strong>. Doct. Thesis, Univ. Paris VII, Institut de Physique du Globe, p.<br />

('Deformation <strong>of</strong> the fore-arc in response to oblique convergence- example <strong>of</strong> <strong>Sumatra</strong>')<br />

Ziegler, K.G.J. (1921)- Verslag over de resultaten van geologisch- mijnbouwkundig onderzoek van het Kendi-<br />

Ringin kolenveld (Res. Palembang). Jaarboek Mijnwezen Nederl. Indie 47 (1918), Verh. 2, p. 141-189.<br />

('Report on the results <strong>of</strong> geological-mining investigation <strong>of</strong> the Kendi-Ringin coal field (Res. Palembang)'.<br />

Coal field with 12 coalbeds in Middle Palembang Fm. Coal grade improved by andesite intrusives)<br />

Ziegler, K.G.J. (1922)- Verslag over het onderzoek der asfalt-terreinen by Tandjoeng Laoet (Res. Palembang).<br />

Jaarboek Mijnwezen Nederl. Indie 47 (1920), Verh. 1, p. 33-69.<br />

('Investigation <strong>of</strong> asphalt deposits near Tanjung Laut (Res. Palembang)'. Six surface asphalt deposits 50 km<br />

WNW <strong>of</strong> Palembang, S <strong>Sumatra</strong>, which are large, degraded oil seeps in outcropping ?Pliocene clastics)<br />

Zonneveld, J. P., Y. Zaim, Y. Rizal, R.L. Ciochon, E.A. Bettis, Aswan & G.F. Gunnell (2011)- Oligocene<br />

shorebird footprints, Kandi, Ombilin Basin, <strong>Sumatra</strong>. Ichnos 18, 4, p. 221-227.<br />

(Two types <strong>of</strong> bird footprints in intertidal sand flat fine sandstone <strong>of</strong> Oligocene Sawahlunto Fm in outcrop near<br />

Kandi Ombilin Mine. Referable to ichnogenus Aquatilavipes and similar to small modern shorebirds)<br />

Zonneveld, J.P., Y. Zaim, Y. Rizal, R.L. Ciochon, E.A. Bettis, Aswan & G.F. Gunnell (2012)- Ichnological<br />

constraints on the depositional environment <strong>of</strong> the Sawahlunto Formation, Kandi, northwest Ombilin Basin,<br />

west <strong>Sumatra</strong>, <strong>Indonesia</strong>. J. Asian Earth Sci. 45, 2, p. 106-113.<br />

(Low diversity trace fossil assemblage from Oligocene Sawahlunto Fm near Kandi, NW Ombilin Basin, W<br />

<strong>Sumatra</strong>. Traces and mud-draped and bidirectional ripples imply tidally-influenced marine setting. Bird<br />

footprints (Aquatilavipes) imply periodic subaerial exposure)<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 123 www.vangorselslist.com July 2012

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