Hostname: page-component-cd9895bd7-gxg78 Total loading time: 0 Render date: 2024-12-26T07:06:34.609Z Has data issue: false hasContentIssue false

Sedimentation in an intracratonic extensional basin: the Karoo of the Central Morondava Basin, Madagascar

Published online by Cambridge University Press:  01 May 2009

G. J. Nichols
Affiliation:
Department of Geological Sciences, University College London, Gower Street, London WC1E 6BT, U.K.
M. C. Daly
Affiliation:
B.P. Petroleum Development Ltd, Britannic House, Moor Lane, London EC2 9BU, U.K.

Abstract

The late Carboniferous to Triassic Karoo Supergroup of Madagascar is a sequence of predominantly continental clastic sediments deposited during a long period of regional crustal extension. In the Morondava Basin of western Madagascar the lower two divisions of the Karoo sediments – the Sakoa and the Sakamena – are deposits of fluvial and lacustrine sedimentation systems supplied from the Precambrian metamorphic basement terrain to the east. East–west crustal extension produced a series of graben and half-graben structures after the Sakoa period which were reactivated after the Sakamena. The position and orientation of these half graben, which were marginal to a larger rift system to the west, were partly controlled by the steep NNE–SSW mylonitic fabric in the metamorphic basement. Palaeocurrents in the braided river deposits of the Sakoa and Lower Sakamena indicate flow to the southwest and west in both sequences. The rivers followed a regional palaeoslope to the southwest/west and were apparently not significantly influenced by the local structural trends which were oriented perpendicular to this slope. The absence of local structural control is attributed to extensive erosional events which followed each tectonic episode and preceded the onset of further sedimentation which took place on an essentially peneplained surface. The tectonic episodes brought about changes in base level which caused this part of the basin to fluctuate between erosion and deposition.

Type
Articles
Copyright
Copyright © Cambridge University Press 1989

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Allen, J. R. L. 1966. On bedforms and palaeocurrents. Sedimentology 6, 153–90.CrossRefGoogle Scholar
Besairie, H. 1972. Géologie de Madagascar I. Les terrains sédimentaires. Tananarive: Malagasy Imprimerie National. Annales Géologiques de Madagascar no. 35, 463 pp.Google Scholar
Boast, J. & Nairn, A. E. M. 1982. An outline of the geology of Madagascar. In The Ocean Basins and Margins, Vol. 6. The Indian Ocean (eds Nairn, A. E. M. and Stehli, F. G.), pp. 649–96. Plenum Press.CrossRefGoogle Scholar
Cant, D. J. 1978. Development of a facies model for sandy braided river sedimentation: comparison of the S. Saskatchewan River and the Battery Point Formation. In Fluvial Sedimentology (ed. Miall, A. D.), pp. 627–39. Canadian Society of Petroleum Geologists Memoir no. 5.Google Scholar
Cant, D. J. & Walker, R. G. 1976. Development of a braided-fluvial facies model for the Devonian Battery Point Formation Sandstone, Quebec. Canadian Journal of Earth Sciences 13, 102–19.CrossRefGoogle Scholar
Cliquet, P. L. 1957. La tectonique profonde du sud du bassin Morondava. Commission for Technical Cooperation in Africa South of Sahara. East-Central and South Regional Committee Geological Meeting 2, Tananarive, pp. 199217.Google Scholar
Coffin, M. F. & Rabinowitz, P. D. 1987. Reconstruction of Madagascar and Africa: evidence from the Davie Fracture Zone and Western Somali Basin. Journal of Geophysical Research 92, 9385–406.CrossRefGoogle Scholar
Crowell, J. C. & Frakes, L. A. 1975. The Late Palaeozoic Glaciation. In Gondwana Geology: papers from the 3rd Gondwana Symposium (ed. Campbell, K. S. W.), pp. 313–31. Canberra: Australian National University Press.Google Scholar
Dewey, J. F. 1982. Plate tectonics and the evolution of the British Isles. Journal of the Geological Society of London 139, 371412.Google Scholar
Dixey, F. 1960. The geology and geomorphology of Madagascar and a comparison with eastern Africa. Quarterly Journal of the Geological Society of London 116, 255–68.CrossRefGoogle Scholar
Friend, P. F., Hirst, J. P. P. & Nichols, G. J. 1986. Sandstone-body structure and river processes in the Ebro Basin of Aragon, Spain. Cuadernos de Geologia (Fluvial Sedimentation in Spain) 10, 930.Google Scholar
Friend, P. F., Slater, M. J. & Williams, R. C. 1979. Vertical and lateral building of river sandstone bodies, Ebro Basin, Spain. Journal of the Geological Society of London 136, 946.CrossRefGoogle Scholar
Frostick, L. E. & Reid, I. 1987. Tectonic control of desert sediments in rift basins ancient and modern. In Desert Sediments, Ancient and Modern (eds Frostick, L. E. and Reid, I.), pp. 5368. Special Publication of the Geological Society of London no. 35.Google Scholar
Hobday, D. K. 1982. The southeast African margin. In The Ocean Basins and Margins, Vol. 6. The Indian Ocean (eds Nairn, A. E. M. and Stehli, F. G.), pp. 149184. Plenum Press.Google Scholar
Kent, P. E. 1974. Continental margin of East Africa – a region of vertical movements. In Geology of the Continental Margins (eds Burk, C. A. and Drake, C.), pp. 313–20. Springer-Verlag, 1009 pp.CrossRefGoogle Scholar
Kent, P. E. 1982. The Somali Ocean Basins and the continental margin of east Africa. In The Ocean Basins and Margins, Vol. 6. The Indian Ocean (eds Nairn, A. E. M. and Stehli, F. G.), pp. 185204. Plenum Press.CrossRefGoogle Scholar
McElhinny, M. W. 1970. Formation of the Indian Ocean. Nature 228, 977–9.Google Scholar
Miall, A. D. 1974. Palaeocurrent analysis of alluvial sediments; a discussion of directional variance and vector magnitude. Journal of Sedimentary Petrology 44, 1174–85.Google Scholar
Miall, A. D. 1981. Alluvial sedimentary basins: tectonic setting and basin architecture. In Sedimentation and Tectonics in Alluvial Basins (ed. Miall, A. D.), pp. 133. Geological Association of Canadian Special Paper no. 23.Google Scholar
Nairn, A. E. M. 1978. Northern and eastern Africa. In The Phanerozoic Geology of the World, Vol. II: The Mesozoic A (eds Moullard, A. and Nairn, A. E. M.), pp. 329–70. Elsevier.Google Scholar
Norton, I. O. & Sclater, J. G. 1979. A model for the evolution of the Indian ocean and the breakup of Gondwanaland. Journal of Geophysical Research 84, 6803–30.Google Scholar
Picard, M. D. & High, L. R. 1972. Criteria for recognising lacustrine rocks. In Recognition of Ancient Sedimentary Environments (eds Rigby, J. K. and Hamblin, W. K.), pp. 108–16. Society of Economic Paleontologists and Mineralogists Special Publication no. 16.Google Scholar
Rabinowitz, P. D., Coffin, M. F. & Falvey, D. 1983. The separation of Madagascar and Africa. Science 220, 67–9.Google Scholar
Radelli, L. 1975. Geology and oil of the Sakamena Basin, Malagasy Republic (Madagascar). American Association of Petroleum Geologists Bulletin 59, 97114.Google Scholar
Rust, B. R. 1978. Depositional models for braided alluvium. In Fluvial Sedimentology (ed. Miall, A. D.), pp. 605–26. Canadian Society of Petroleum Geologists Memoir no. 5.Google Scholar
Smith, A. G. & Hallam, A. 1970. The fit of the southern continents. Nature 225, 139–44.Google Scholar
Watts, A. B. 1982. Tectonic subsidence, flexure and global changes in sea level. Nature 297, 469–74.CrossRefGoogle Scholar
White, N. & McKenzie, D. 1988. Formation of the ‘steer's head’ geometry of sedimentary basins by different stretching of the crust and mantle. Geology 16, 250–3.2.3.CO;2>CrossRefGoogle Scholar