Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Groothoff, C.T. (1916)- Eenige merkwaardige gesteenten van Billiton. Verhand. Nederl. Geol.-Mijnbouwk.
Gen. Nederl. Kol., Geol. Ser. 3 (Molengraaf Volume), p. 89-106.
('Some remarkable rocks from Belitung'. Includes descriptions of granite with primary cassiterite, granite with
fluorite, topaze-bearing rocks, tourmaline greisen, etc.)
Haile, N.S. (1971)- Quaternary shorelines in West Malaysia and adjacent parts of the Sunda Shelf. Quaternaria
15, p. 333-343.
Haile, N.S. (1973)- The geomorphology and geology of the northern part of the Sunda shelf and its place in the
Sunda mountain system. Pacific Geol. 1973, 6, p. 73-89.
Hamzah, Y. (1995)- Tin placer deposits off the Rebo area, East coast of Bangka Island, Indonesia. In: J. Ringis
(ed.) Proc. 31st Sess. Comm. Co-ord. Joint Prospecting Min. Res. Asian Offshore Areas (CCOP), Kuala
Lumpur 1994, 2, p. 79-89.
Hamzah, Y. (1998)- Geophysical survey of tin placer deposits in West Singkep offshore, Riau Archipelago,
Indonesia. In: J.L. Rau (ed.) Proc. 34th Sess. Sess. Co-ord. Comm. Coastal Offshore Geosc. Programs E and SE
Asia (CCOP), Taejon, Korea 1997, 2, Techn. Repts, p. 55-63.
(Geophysical survey W of Singkep, NW of Bangka, to map cassiterite-bearing channels on biotite granite
basement surface)
Hanebuth, T.J.J. & K. Stattegger (2003)- The stratigraphic evolution of the Sunda Shelf during the past fifty
thousand years. In: F.H. Sidi, D. Nummedal et al. (eds.) Deltas of Southeast Asia and vicinity-sedimentology,
stratigraphy and petroleum geology, SEPM Spec. Publ. 76, p. 189-200.
(Sunda shelf extensively exposed during last glaciation, with soil formation and sediment bypass. Subsequent
sea level rise caused stepwise drowning)
Hanebuth, T.J.J. & K. Stattegger (2004)- Depositional sequences on a late Pleistocene-Holocene tropical
siliciclastic shelf (Sunda Shelf, Southeast Asia). J. Asian Earth Sci. 23, p.113-126.
(Sunda Shelf tropical siliciclastic shelf with low gradient, extreme width, huge paleo-valley systems, high
sediment input due to large catchment area. Four systems tracts during last glacial sea-level fall and
subsequent deglacial rise: (a) wide, partly detached deltaic clinoforms indicate forced regression; (b) shoreline
deposits and soil formation of lowstand systems tract; (c) backstepping coastline deposits form confined
transgressive systems tract and mainly restricted to paleo-valley system; (d) thin marine mud cover as
condensed section over whole shelf (base of HST))
Hanebuth, T.J.J., K. Stattegger & A. Bojanowski (2009)- Termination of the Last Glacial Maximum sea-level
lowstand: the Sunda-Shelf data revisited. Global Planet. Change 66, p. 76-84.
(Sunda Shelf Late Pleistocene paleo-coastal relict forms indicating older lowstand 5 m deeper than sea level
during Last Glacial Maximum (LGM; 21-19 ka BP). Sunda shelf LGM sea level recalculated to 123 ± 2 m
below modern water depth)
Hanebuth, T.J.J., K. Stattegger & P.M. Grootes (2000)- Rapid flooding of the Sunda Shelf- a late-glacial sealevel
record. Science 288, p.1033-1035.
(Sea level rise after last glacial maximum at ~20 ka derived from siliciclastic shoreline facies. Record generally
confirms reconstructions from coral reefs (~ -115m at 20 ka). Rise of sea level during meltwater pulse 1A was
16 m in 300 years between 14.6 to 14.3 ka)
Hanebuth, T.J.J., K. Stattegger & Y. Saito (2002)- The stratigraphic architecture of the central Sunda Shelf (SE
Asia) recorded by shallow-seismic surveying. Geo-Marine Lett. 22, p. 86-94.
(Shallow seismic identified units and surfaces of last three 100 ka Pleistocene sea-level cycles)
Bibliography of Indonesia Geology v. 4.1 130 www.vangorselslist.com July 2012