The Paleo-Orientations of Northwestern Borneo and Adjacent South China Sea Basins
DOI:
https://doi.org/10.17014/ijog.7.2.67-76Keywords:
paleomagnetism, counter-clockwise rotation, reconstruction rotation of Borneo, South China SeaAbstract
Limited paleomagnetic data from West Kalimantan and southwestern Sarawak appear to indicate counter-clockwise (CCW) rotation of over 50 degrees during Cenozoic. On the other hand, similar studies from Sabah show conflicting results in terms of paleo-positions. This CCW information and other plate tectonic considerations have formed the base of Southeast Asia’s plate reconstructions that have seen print in a number of updated versions. The existing publications on extensive field and exploration data, including geological stress fields from wellbore breakouts, on northwestern Borneo and basins of South China Sea have not been taken into account. The latter wealth of information already established that the region under discussion consists of a mosaic-like assemblage of diverse tectono-stratigraphic terranes, each with separate tectonic development. Stress fields changed in different ways in the different terranes indicating definitively that regional, progressive CCW rotation of Borneo is not possible.
References
Darman, H. and Hasan Sidi, F. 2000. An Outline of The Geology of Indonesia, Ikatan Ahli Geologi Indonesia, 5, p.69-90.
Fuller, M., Ali, J. R., Moss, S.J., Frost, G.M., Richter, B., and Mahfi, A. 1999. Paleomagnetism in Borneo. Journal Asian Earth Sciences, 17 (1-2), p.3-24. doi:10.1016/S0743-9547(98)00057-9
Haile, N.S., 1961. The Geology and Mineral Resources of the Suai-Baram Area, North Sarawak. Geological Survey Department, British Territories in Borneo, Memoir 13, map scale 1 : 250 000.
Hall, R., Clements, B., and Smyth, H.R., 2009. Sundaland basement character, structure and plate tectonic development.
Proceedings, 33rd Indonesian Petroleum Association Annual Convention & Exhibition. IPA09-G-134.
Hon, V. and Lam, S.K., 1992. Geological Map of Sarawak, second edition, scale 1:500 000. Geological Survey of Malaysia.
James, D.M.D. (ed.), 1984. The Geology and Hydrocarbon Resources of Negara Brunei Darussalam. Muzium Brunei; Seria, Special publication, 169pp. doi:10.1017/S0016756800031551
Kirk, H.J.C., 1957. The Geology and Mineral Resources of the Upper Rajang and Adjacent Areas, Sarawak. Geological Survey Department, British Territories in Borneo, Memoir 8, map scale 1 : 250 000.
Liechti, P., Roe, F.W., and Haile, N.S., 1960. The Geology of Sarawak, Brunei and the Western Part of North Borneo. Geological Survey Department, British Territories in Borneo, Bulletin 3 (1), 360pp.
Lim, P.S., 1985. Geological Map of Sabah, third edition, scale 1 : 500 000. Geological Survey of Malaysia. Petronas, K.M. Leong, ed., 1999. The Petroleum Geology and Resources of Malaysia, Petronas, Kuala Lumpur, 685pp.
Pieters, P. E., Trail, D.S., and Supriatna, S., 1987. Correlation of pre-Tertiary rocks across Kalimantan. Proceedings, Indonesian Petroleum Association 16th Annual Convention, 1.
Sabins Jr., F.F., 1983. Space radar images of Indonesia. Proceedings,12th Indonesian Petroleum Association Annual Convention, 127, p.142.
Sandal, S.T., 1996. The Geology and Hydrocarbon Resources of Negara Brunei Darussalam, Brunei Shell Petroleum Company Sendirian Berhad.
Schmidtke, E.A., Fuller, M.D., and Haston, R.B., 1990. Paleomagnetic data from Sarawak, Malaysia (Borneo) and the Late Mesozoic and Cretaceus tectonics of Sundaland. Tectonics, 9(1), p.123-140. doi:10.1029/TC009i001p00123
Tate, R.B., compiler, 2001. The Geology of Borneo Island. Geological Society of Malaysia, CD issue.
Taylor, B. and Hayes, D.E., 1983. Origin and history of the South China Sea basin. American Geophysical Union, Geophysical Monograph, 27, p.23-56. doi:10.1029/GM027p0023
Tjia, H.D., 1967. Sense of fault displacements. Geologie en Mijnbouw, 46, p.392-396.
Tjia, H.D. and Idrus Ismail, M.,1994. Tectonic implications of well-bore breakouts in Malaysian basins. Geological Society of Malaysia, Bulletin, 36, p.175-186.
Tjia, H.D., 1988. Accretion tectonics in Sabah: Kinabalu Suture Zone and East Sabah terrane. Geological Society of Malaysia, Bulletin, 22, p.237-251.
Tjia, H.D., 2003. Northwest Sabah Overthrust System. Geological Society of Malaysia, Bulletin, 46, p.5-10.