Post-Doctoral Associate
Yale University
Department of Geology and Geophysics
PO Box 208109
New Haven, CT 06511
tel: (203) 436 4049
e-mail: michiel.dekock@yale.edu
Last updated: January 2008
Research
Publications and Reprints
Abstracts
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I am currently doing a postdoc at Yale University, where my research is focused on the paleomagnetism of the Ghaap Group. It is a Late Archean to Early Proterozoic carbonate/banded-iron formation succession from the Kaapvaal Craton in South Africa. This study is part of the Agouron-Griqualand Paleoproterozoic Drilling Project.
Of particular interest is the correlation of the Ghaap Group with a similar succession from the Pilbara Craton in Western Australia. Were the two cratons ever amalgamated to form the hypothetical Vaalbara? When did Vaalbara exists, and when did it break up? How did global tectonics influence paleoclimate, the biosphere and the atmosphere? Was the geomagnetic field to the first order always dipolar? This is the so-called GAD hypothesis. Presently we have a limited set of paleoclimatic indicators with which to test the GAD hypothesis. We use paleoclimatic indicators to test GAD through time, but how sensitive are they? Are there others indicators we could use, for example stromatolites in Archean and Paleoproterozoic aged rocks?
These are some of the questions I am interested in. My work also includes economic aspects such as the large iron ore deposits of South Africa, Western Australia and India and their place within a global tectonic reference frame.
Articles in preparation
Gutzmer, J., Beukes, N.J., De Kock, M.O. and Netshiozi, S., (2005). Origin of high-grade iron ores at the Thabazimbi deposit, South Africa, in Conference Proceedings Iron Ore 2005, Aus IMM, Publication Series 8, pp.99-110. AusIMM, Melbourne, Australia.
De Kock, M.O., Evans, D.A.D., Kirschvink, J.L., Beukes, N.J., Rose, E. and Hilburn, I. (in review), Paleomagnetism of a Neoarchean-Paleoproterozoic carbonate ramp and carbonate platform succession (Transvaal Supergroup) from surface outcrop and drill core, Griqualand West region, South Africa. Precambrian Research
2006
De Kock, M.O., Evans, D.A.D., Dorland, H.C., Beukes, N.J. and Gutzmer, J. (2006). Paleomagnetism of the lower two unconformity-bounded sequences of the Waterberg Group South Africa: Towards a better defined apparent polar wander path for the Paleoproterozoic Kaapvaal Craton. South African Journal of Geology, 109, pp. 157-182.
2005
Ward, P.D., Botha, J., Buick, R, De Kock, M.O., Erwin, D.H., Garrison, G.H., Kirschvink, J.L., and Smith, R. (2005). Abrupt and gradual extinction among Late Permian land vertebrates in the Karoo Basin, South Africa. Science, 307, pp. 709-714.
2004
De Kock, M.O., and Kirschvink, J.L. (2004). Paleomagnetic Constraints on the Permian-Triassic boundary in Terrestrial strata of the Karoo Supergroup, South Africa: Implications for causes of the End-Permian extinction event. Gondwana Research, 7(1), pp. 175-183.