Discontinuites sismiques et sedimentaires dans la serie de remplissage du fosse du Tanganyika, Rift Est-africain

J. J. Tiercelin; C. A. Scholz; A. Mondeguer; B. R. Rosendahl; C. Ravenne

Discontinuites sismiques et sedimentaires dans la serie de remplissage du fosse du Tanganyika, Rift Est-africain

Translated title of the contribution: Seismic and sedimentary discontinuities in the Lake Tanganyika Trough, East African Rift

J. J. Tiercelin, C. A. Scholz, A. Mondeguer, B. R. Rosendahl, C. Ravenne

Research output: Contribution to journal › Article › peer-review

16 Scopus citations

Abstract

Reveals a thick sedimentary fill partitioned by six seismic and sedimentary discontinuities which are either gaps in the sedimentary record or marked changes in lithology. Dated between the Mesozoic and the upper Pleistocene, they can be interpreted in terms of lake level variations caused by tectonic or climatic events. There is an abridged English version. -English summary

Translated title of the contribution	Seismic and sedimentary discontinuities in the Lake Tanganyika Trough, East African Rift
Original language	French
Pages (from-to)	1599-1606
Number of pages	8
Journal	Comptes Rendus - Academie des Sciences, Serie II
Volume	309
Issue number	16
State	Published - 1989
Externally published	Yes

ASJC Scopus subject areas

General Environmental Science
General Engineering
General Earth and Planetary Sciences

Cite this

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AU - Tiercelin, J. J.

AU - Scholz, C. A.

AU - Mondeguer, A.

AU - Rosendahl, B. R.

AU - Ravenne, C.

PY - 1989

Y1 - 1989

N2 - Reveals a thick sedimentary fill partitioned by six seismic and sedimentary discontinuities which are either gaps in the sedimentary record or marked changes in lithology. Dated between the Mesozoic and the upper Pleistocene, they can be interpreted in terms of lake level variations caused by tectonic or climatic events. There is an abridged English version. -English summary

AB - Reveals a thick sedimentary fill partitioned by six seismic and sedimentary discontinuities which are either gaps in the sedimentary record or marked changes in lithology. Dated between the Mesozoic and the upper Pleistocene, they can be interpreted in terms of lake level variations caused by tectonic or climatic events. There is an abridged English version. -English summary

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Discontinuites sismiques et sedimentaires dans la serie de remplissage du fosse du Tanganyika, Rift Est-africain

Abstract

ASJC Scopus subject areas

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