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Conodont faunas, age and correlation of the Alas Formation (Carboniferous), Sumatra

Published online by Cambridge University Press:  01 May 2009

I. Metcalfe
Affiliation:
Department of Geology, University of Malaya, Kuala Lumpur, 22–11, Malaysia

Abstract

Summary. The Alas Formation (shelf limestones) of Sumatra is reinterpreted to be of late Visean age, on the basis of conodonts and brachiopods, rather than of Permian age as previously thought. It is, therefore, the oldest dated formation in Sumatra. The Alas Formation probably underlies or is equivalent to the lower part of the Kluet Formation within the Tapanuli Group.

Type
Articles
Copyright
Copyright © Cambridge University Press 1983

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References

REFERENCES

Cameron, N. R., Clarke, M. C. G., Aldiss, D. T., Aspden, J. A. & Djunuddin, A. 1980. The geological evolution of northern Sumatra. Ninth Indonesia Petroleum Assoc. Convention, Jakarta. 53pp.Google Scholar
Higgins, A. C. 1975. Conodont zonation of the late Visean-early Westphalian strata of the south and central Pennines of northern England. Bull. Geol. Surv. G.B. no. 53, 190, 18 pls.Google Scholar
Metcalfe, I., Koike, T., Rafek, M. B. & Haile, N. S. 1979. Triassic conodonts from Sumatra. Palaeontology 22, 737–46, pl. 97.Google Scholar
Mitchell, A. H. G. 1977. Tectonic settings for emplacement of Southeast Asian tin granites. Bull. Geol. Soc. Malaysia, 9, 123–40.CrossRefGoogle Scholar
Mitchell, A. H. G. 1981. Phanerozoic plate boundaries in mainland S.E. Asia, the Himalayas and Tibet. J. geol. Soc. Lond. 138, 109–22.CrossRefGoogle Scholar
Ridd, M. F. 1980. Possible Palaeozoic drift of S.E. Asia and Triassic collision with China. J. geol. Soc. Lond. 137, 635–40.CrossRefGoogle Scholar
Silitonga, P. H. & Kastowo, 1975. Geological map of the Solok Quadrangle, Sumatra, 1:250000 scale. Geological Survey of Indonesia, Bandung.Google Scholar
Stauffer, P. H. 1974. Malaya and Southeast Asia in the pattern of continental drift. Bull. Geol. Soc. Malaysia, 7, 83138.Google Scholar
Stauffer, P. H. 1983. Unraveling the mosiac of Palaeozoic crustal blocks in Southeast Asia. Geologische Rundschau (in press).CrossRefGoogle Scholar
Stauffer, P. H. & Mantajit, J. 1981. Late Palaeozoic tilloids of Malaya, Thailand and Burma. In Earth's Pre-Pleistocene Glacial Record (ed. Hambrey, M. J. and Harland, W. B.), pp. 331–7. Cambridge University Press.Google Scholar
Waterhouse, J. B. 1976. World correlations for marine Permian faunas. Pap. Dep. Geol. Univ. Queensland 7, 232 pp.Google Scholar