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The Madai-Baturong Limestone Member of the Chert-Spilite Formation, North Borneo

Published online by Cambridge University Press:  01 May 2009

C. G. Adams  and
H. J. C. Kirk
C. G. Adams
Affiliation:
British Museum (Nat. Hist.), London, S. W. 7.
H. J. C. Kirk
Affiliation:
Geological Survey Department, British Territories in Borneo, Jesselton, North Borneo.
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Abstract

Pelagic Foraminifera found in the marginal parts of the limestone at Mount Madai in south-eastern North Borneo indicate that it is of Upper Cretaceous age. Much of the limestone at Mount Madai and Mount Baturong does, however, contain algae and other microfossils characteristic of Lower Cretaceous rocks in other parts of the world.

The limestone is provisionally classified as the Madai–Baturong Limestone Member of the Chert-Spilite Formation. Revision of the stratigraphy has clarified the regional structure, and it is postulated that the Chert-Spilite Formation has been uplifted against Neogene sediments along a major zone of thrust faulting.

Type
Articles
Information
Geological Magazine , Volume 99 , Issue 4 , August 1962 , pp. 289 - 303
Copyright
Copyright © Cambridge University Press 1962

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References

REFERENCES

Bolli, H. M., 1957. The genera Praeglobotruncana, Rotalipora, Globotruncana, and Abathomphalus in the Upper Cretaceous of Trinidad, B.W.I. In Loeblich et al., Studies in Foraminifera. Bull. U.S. nat. Mus., 215, 1–323.Google Scholar
Cushman, J. A., 1938. Cretaceous species of Gümbelina and related genera. Contr. Cush. Lab. Foram. Res., 14, 2–28.Google Scholar
Dalbiez, F., 1955. The genus Globotruncana in Tunisia. Micropaleontology, 1, 161–171.CrossRefGoogle Scholar
Davis, A. G., 1955. In Wilford G. E. The Geology and Mineral Resources of the Kuching-Lundu Area, West Sarawak, including the Bau Mining Area. Brt. Borneo Geol. Survey Mem. 3.Google Scholar
Elliott, G. F., 1958. Algal debris-facies in the Cretaceous of the Middle East. Palaeontology, 1, 254–9.Google Scholar
Elliott, G. F., 1960 a. Fossil calcareous algal floras from the Middle East with a note on a Cretaceous problematicum. Hensonella cylindrica gen. et. sp. nov. Quart. J. geol. Soc. Lond., 115, 217–232.CrossRefGoogle Scholar
Elliott, G. F., 1960 b. In KirkH. J. C. Progress Report on the Semporna Peninsula Survey. Brit. Borneo Geol. Survey Ann. Rpt. for 1959, 182–195.Google Scholar
Fitch, F. H., 1955. The geology and mineral resources of part of the Segama Valley and Darvel Bay area, North Borneo. Brt. Borneo Geol. Survey Mem. 4.Google Scholar
Kirk, H. J. C., 1959. Geology and Mineral Resources of the Semporna Peninsula. Brt. Borneo Geol. Survey Ann. Rpt. for 1958, 191–206.Google Scholar
Kirk, H. J. C., 1960. Progress report on the Semporna Peninsula Survey. Brt. Borneo Geol. Survey Ann. Rpt. for 1959, 182–195.Google Scholar
Reinhard, M., and Wenk, E., 1951. The Geology of the Colony of North Borneo. Brt. Borneo Geol. Survey Bull. 1.Google Scholar
Vogler, J., 1941. Ober-Jura und Kreide von Misol (Nienderländisch Ostindien), 243–293. In Boehm, G., and Wanner, J.. Beiträge zur Geologie von Niederländisch-Indian. Palaeontographica, Stuttgart, Suppl. Bd. 4, Lief 4, Abschnitt 4.Google Scholar
Wanner, J., 1921. Beiträge zur geologie und geographie von Nordost-Borneo. Neues Jb. Min. Geol. Paläont., Beilage Bd. 45, 149–213.Google Scholar