Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sitanggang, J.M. (1983)- The use of alkali elements as a guide to tin mineralization in some granite rocks in the
island of Bangka. Proc. 12th Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 163-167.
Sitanggang, J.M. (1986)- Distribution of major and some trace elements of some granites from Bangka,
Indonesia. In: G.H. Teh & S. Paramananthan (eds.) Proc. GEOSEA V Conf., Kuala Lumpur 1984, 2, Geol. Soc.
Malaysia Bull. 20, p. 401-422.
Sitha, K., L.D. Setijadji, K. Sanematsu, T. Ikuno, A. Imai, A. Dimara & K. Watanabe (2009)- REE in monzogranites
in Bangka Island, Indonesia. Proc. 2nd Reg. Conf. Interdisc. Res. Natural Resources and Materials
Engineering, Yogyakarta 2009, p.
Slik, JW.F., S. Aiba, M. Bastian, F.Q. Brearley, C.H. Cannon, K.A.O. Eichhorng, G. Fredriksson et al. (2011)-
Soils on exposed Sunda shelf shaped biogeographic patterns in the equatorial forests of Southeast Asia. Proc.
Nat. Acad. Sci. USA 108, 30, p. 12343-12347.
(Marked present-day biogeographic difference between W (Malay Peninsula, Sumatra) and E Sundaland
(Borneo) surprising as these areas formed single landmass for long time in Pleistocene. Dry savanna corridor
dispersal barrier during glacial maxima proposed to explain this, but short duration of dry savanna conditions
make it an unlikely sole cause. Analysis of tree inventories suggest exposed sandy sea-bed soils acted as
dispersal barrier; no confirmation of savanna corridor)
Smit Sibinga, G.L. (1949)- Pleistocene eustasy and glacial chronology in Java and Sumatra. Verhand. Nederl.
Geol.-Mijnbouwk. Gen., Geol. Ser. 15, p. 1-31.
Soeria-Atmadja, R., D. Darda & D. Hasanuddin (1986)- Some aspects of southern granitoid complex and tin
mineralization in the northern part of Bangka, Indonesia. In: G.H. Teh & S. Paramananthan (eds.) Proc.
GEOSEA V Conf., Kuala Lumpur 1984, 1, Geol. Soc. Malaysia Bull. 19, p. 349-367.
(Petrographic details of S-type granitoids of Bangka. Tin mineralization mostly along WNW, NNE and N-S
directions, seem related to Late Triassic deformation)
Stattegger, K., W. Kuhnt, H.K. Wong, C. Buhring, C. Haft, T. Hanebuth et al. (1997)- Sequence stratigraphy,
Late Pleistocene- Holocene sea level fluctuations and high resolution record of the Post-Pleistocene
transgression on the Sunda Shelf. Cruise Report Sonne 115, Sundaflut, Univ. Kiel, Geol.-Pal. Institut, Reports
86, 211p.
Steinke, S., T.J.J. Hanebuth, C. Vogt & K. Stattegger (2008)- Sea level induced variations in clay mineral
composition in the southwestern South China Sea over the past 17,000 yr. Marine Geol. 250, p. 199-210.
(Variations in clay mineral composition of Sunda Shelf margin and slope cores over past 17,000 yrs. Deglacial
sea level rise principal factor driving changes. Late Glacial high kaolinite reflect higher contribution of clays
from soils formed on exposed Sunda Shelf. After coastline retreated close to present-day position in mid-
Holocene stronger influence of illite-rich sources (e.g. Borneo))
Steinke, S., M. Kienast & T. Hanebuth (2003)- On the significance of sea-level variations and shelf paleomorphology
in governing sedimentation in the southern South China Sea during the last deglaciation. Marine
Geol. 201, p. 179-206.
(Quaternary deglacial sedimentation on outer Sunda Shelf, shelf margin and slope controlled by shelf paleophysiography
and changes in sea level and sediment supply. Five sites along transect across outer shelf and
continental slope document four intervals of significant depositional changes in last 20 000 years: drowning of
lower course of North Sunda (Molengraaff) River (16.5-14.5 ka), rapid rise in sea level with flooding of middle
part of paleo-valley at 14.5-14 ka and flooding of surrounding plains of river valley (14-8.5 ka). Coastline
reached modern position between ca. 8.5- 6 ka)
Strimple, H.L. & T.E. Yancey (1976)- Moscovicrinus preserved in magnetite from Selumar, Belitung Island,
Indonesia. J. Paleontology 50, 6 p. 1195-1202.
Bibliography of Indonesia Geology v. 4.1 137 www.vangorselslist.com July 2012