Paleogeography of the Seychelles Bank and the northwest Madagascar Shelf during the last glacio-eustatic regression (18,000 a B.P.)

D. D. Badyukov; E. L. Demidenko; P. A. Kaplin

doi:10.1007/BF02842661

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Paleogeography of the Seychelles Bank and the northwest Madagascar Shelf during the last glacio-eustatic regression (18,000 a B.P.)

OriginalPaper | Updated：2023-05-16

- Paleogeography of the Seychelles Bank and the northwest Madagascar Shelf during the last glacio-eustatic regression (18,000 a B.P.)
- Paleogeography of the Seychelles Bank and the northwest Madagascar Shelf during the last glacio-eustatic regression (18,000 a B.P.)
- 海洋湖沼学报（英文） 1989年7卷第1期页码：89-92
- Affiliations：
  
  Dept. of Geography
- Author bio：
- Funds：
- DOI：10.1007/BF02842661
  中图分类号：
- 纸质出版：1989
- Accepted：
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Paleogeography of the Seychelles Bank and the northwest Madagascar Shelf during the last glacio-eustatic regression (18,000 a B.P.)[J]. 海洋湖沼学报（英文）, 1989,7(1):89-92.

Badyukov, D.D., Demidenko, E.L. & Kaplin, P.A. Paleogeography of the Seychelles Bank and the northwest Madagascar Shelf during the last glacio-eustatic regression (18,000 a B.P.)., Chin. J. Ocean. Limnol. 7, 89–92 (1989). https://doi.org/10.1007/BF02842661
Paleogeography of the Seychelles Bank and the northwest Madagascar Shelf during the last glacio-eustatic regression (18,000 a B.P.)[J]. 海洋湖沼学报（英文）, 1989,7(1):89-92. DOI： 10.1007/BF02842661.

Badyukov, D.D., Demidenko, E.L. & Kaplin, P.A. Paleogeography of the Seychelles Bank and the northwest Madagascar Shelf during the last glacio-eustatic regression (18,000 a B.P.)., Chin. J. Ocean. Limnol. 7, 89–92 (1989). https://doi.org/10.1007/BF02842661 DOI：

摘要

Abstract

The Seychelles Bank and Madagascar Shelf in the western Indian Ocean were explored geologically during a cruise of the R/V “professor Shtokman” in 1986. Using the data of relief

sediment characteristics and their sequences of strata

paleogeographic maps (18

000 a B.P.) of these areas were produced. These maps show that the Bank and the Shelf are carbonate platforms with complicated topography. The data indicate an important role of sea level oscillation in relief development of this area.

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references

Kaplin, P. A., and F. A. Shcherbakov, 1986. Reconstruction of shelf environments during the Late Quaternary.Journal of Coastal Research (Special Issue)1: 95–98.

Pirazzoli, P. A., 1986. Late Quaternary evolution of Shelf areas in the Western Indian Ocean.Episodes 9(1): 30–31.

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