Glacial Sedimentology of Schirmacher Oasis, East Antarctica

Author:

Srivastava Ashok Kumar1,Khare Neloy2

Affiliation:

1. SGB Amravati University, India

2. Ministry of Earth Sciences, India

Abstract

Schirmacher Oasis, East Antarctica is under investigation for the last four decades by Indian scientists of various disciplines, of which geological studies constitute a significant aspect. The present attempt is a review of sedimentological studies carried out in the area. A few of the current chapter's elements are sediment characteristics, mode, and pattern of sediment deposition, source rock, provenance, paleoclimate, and weathering condition through clay mineral studies, grain surface studies, etc., with specific aspects more data on the number of samples. Simultaneously, the Oasis also offers good scope for various other significant investigations like paleoclimatic reconstruction, source of glacial sediments, silicates weathering, etc. Globally, they are a front-line work area and recommended.

Publisher

IGI Global

Reference85 articles.

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2. Bardin, V. I. (1982). Composition of East Antarctic moraines and some problems of Cenozoic history. In C. Craddock (Ed.), Antarctic Geoscience (pp. 1069-1076). Univ. Wisconsin Press.

3. Clay minerals in unconsolidated deposits of the Prince Charles Mountains.;V. I.Bardin;Inf. Bull. Sov. Antarct. Exped.,1979

4. Late Holocene palaeo-winds and climatic changes in Eastern Antarctica as indicated by long-distance transported pollen-spores and local microbiota in polar lake core sediments.;S. K.Bera;Current Science,2004

5. Mineralogy and Sedimentation of Recent Deep-Sea Clay in the Atlantic Ocean and Adjacent Seas and Oceans

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