Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Schlueter, H.U., C. Gaedicke, H.A. Roeser, B. Schreckenberger, H. Meyer, C. Reichert et al. (2002)- Tectonic
features of the Sumatra-Java forearc of Indonesia. Tectonics 21, 5, p. 1047-1062.
(Sunda Arc off S. Sumatra-E Java two accretionary wedges: inner wedge I Late Oligocene tectonic flakes and
Neogene-Recent outer wedge II. Wedge I forms outer arc high and backstop for outer wedge II. Missing outer
arc high of S Sunda Strait explained by Neogene transtension due to clockwise rotation of Sumatra and arcparallel
strike-slip movements. Rotation created pull-apart basins along W Sunda Strait (Semangka Graben)
and transpression and inversion on E Sunda Strait in Krakatau Basin. Sumatra FZ probably attached to Java
Cimandiri-Pelabuhan Ratu strike-slip fault prior to Sumatra rotation)
Schmidt, C. (1901)- Observations geologiques a Sumatra et a Borneo. Bull. Soc. Geol. France IV, 1, p. 260-
267.
(‘Geological observations on Sumatra and Borneo’. Summary description of Sumatra and Borneo geology, with
cross sections through Bangka and south Sumatra)
Schouten, C. (1928)- Mineragrafisch onderzoek van goudertsen van Lebong Bahroe en Tandaiberg
(Mijnbouwmaatschappij Simau, Sumatra). Verhand. Geol. Mijnbouwk. Gen. Nederl. Kol., Mijnbouwk. Ser. 2,
4, p. 161-233.
(Minerographic study of gold ores from Lebong Baru and Tandaiberg (Mining company Simau, Sumatra)'.
Miscroscopic study of gold, silver and copper minerals from hydrothermal veins associated with andesites from
Lebong Baru and Lebong Tandai, complex, NE of Bengkulu, C Sumatra)
Schurmann, H.M.E. (1922)- Over de Neogene synclinaal van Zuid Sumatra en het ontstaan van bruinkool. De
Mijningenieur 3, 5, p. 67-70. en 6, p. 77-81.
(‘On the Neogene syncline of South Sumatra and the development of lignites’)
Schurmann, H.M.E. (1923)- Uber die Neogene Geosynclinale von Sud-Sumatra und das Erstehen der
Braunkohle. Geol. Rundschau 14, p. 239-252.
(‘On the Neogene syncline of South Sumatra and the development of lignite’. German version of 1922 Dutch
paper)
Schurmann, H.M.E. (1929)- Ofiolieten en abyssieten in Noord Sumatra. De Mijningenieur 10, 11, p. 235-237.
(‘Ophiolites and abyssal rocks in North Sumatra’. In Barisan Mts area between Tangse and Geumpang, Aceh.
Ocean crust assemblage of serpentinites and gabbro associated with red siliceous shales and radiolarites)
Schurmann, H.M.E. (1930)- Geologische notities uit de Batak landen, Noord Sumatra. De Mijningenieur 11, 10,
p. 197-200.
(‘Geologic notes from the Batak territories, N Sumatra’. Paleogene outcrops in several areas. Pre-Eocene
rocks in Wilhelmina mountains)
Schwartz, M.O. & Surjono (1990)- Sungai Isahan- a new primary tin occurrence in Sumatra. Bull. Geol. Soc.
Malaysia 26, p. 181-188.
(New primary tin occurrence at Sg Isahan has cassiterite mineralization in hydrothermally altered muscovite
granite. Radiometric age (193, 197 Ma= earliest Jurassic; HvG) and tectonic position suggests correlation
with Main Range of Peninsular Malaysia)
Sebrier M., S. Pramumijoyo & O. Bellier (1993)- Miocene to Recent kinematic evolution around the Sunda
Strait and southern end of the great Sumatra Fault: microtectonic approach. 10th Ann. French Indonesian
Cooperation in Oceanography, Jakarta, p. 37-40.
Setiawan, H., P.S. Widiantoro, Hendarman & M. Primaryanta (2012)- Success story with low resistivity sand in
an exploration block, western edge of Central Sumatran Basin. Proc. 36th Ann.Conv. Indon. Petrol. Assoc.,
Jakarta, IPA12-G-095, p.1-8.
Bibliography of Indonesia Geology v. 4.1 88 www.vangorselslist.com July 2012