Mineralogy of lacustrine sediments in the Schirmacher Range Area, Eastern Antarctica

A mineralogical study of the lacustrine sediment cores from lakes and varve deposits of the lake shore in the Schirmacher Range of East Antarctica is presented. Field observations and laboratory analysis indicate quartz and feldspar as principal allogenic phases derived from local crystalline rocks...

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Main Authors: Sinha, Rajiv, Chatterjee, A.
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of India 2000
Subjects:
Online Access:http://repository.ias.ac.in/120244/
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spelling ftindianacasci:oai:repository.ias.ac.in:120244 2023-05-15T13:53:35+02:00 Mineralogy of lacustrine sediments in the Schirmacher Range Area, Eastern Antarctica Sinha, Rajiv Chatterjee, A. 2000 http://repository.ias.ac.in/120244/ unknown Geological Society of India Sinha, Rajiv Chatterjee, A. (2000) Mineralogy of lacustrine sediments in the Schirmacher Range Area, Eastern Antarctica Journal of the Geological Society of India, 56 (1). pp. 39-45. ISSN 0016-7622 QE Geology Article PeerReviewed 2000 ftindianacasci 2021-07-11T18:26:52Z A mineralogical study of the lacustrine sediment cores from lakes and varve deposits of the lake shore in the Schirmacher Range of East Antarctica is presented. Field observations and laboratory analysis indicate quartz and feldspar as principal allogenic phases derived from local crystalline rocks surrounding the lake basin. Illite, chlorite and minor amount of mixed-layered minerals in the lacustrine sediments are interpreted to be products of weathering in the lake catchment. In general, the clay mineralogy of sediment cores and varve sediments is indicative of low-hydrolyzing depositional environment under high latitudes and subtle weathering. Article in Journal/Newspaper Antarc* Antarctica Antarctica Journal East Antarctica Indian Academy of Sciences: Publication of Fellows East Antarctica
institution Open Polar
collection Indian Academy of Sciences: Publication of Fellows
op_collection_id ftindianacasci
language unknown
topic QE Geology
spellingShingle QE Geology
Sinha, Rajiv
Chatterjee, A.
Mineralogy of lacustrine sediments in the Schirmacher Range Area, Eastern Antarctica
topic_facet QE Geology
description A mineralogical study of the lacustrine sediment cores from lakes and varve deposits of the lake shore in the Schirmacher Range of East Antarctica is presented. Field observations and laboratory analysis indicate quartz and feldspar as principal allogenic phases derived from local crystalline rocks surrounding the lake basin. Illite, chlorite and minor amount of mixed-layered minerals in the lacustrine sediments are interpreted to be products of weathering in the lake catchment. In general, the clay mineralogy of sediment cores and varve sediments is indicative of low-hydrolyzing depositional environment under high latitudes and subtle weathering.
format Article in Journal/Newspaper
author Sinha, Rajiv
Chatterjee, A.
author_facet Sinha, Rajiv
Chatterjee, A.
author_sort Sinha, Rajiv
title Mineralogy of lacustrine sediments in the Schirmacher Range Area, Eastern Antarctica
title_short Mineralogy of lacustrine sediments in the Schirmacher Range Area, Eastern Antarctica
title_full Mineralogy of lacustrine sediments in the Schirmacher Range Area, Eastern Antarctica
title_fullStr Mineralogy of lacustrine sediments in the Schirmacher Range Area, Eastern Antarctica
title_full_unstemmed Mineralogy of lacustrine sediments in the Schirmacher Range Area, Eastern Antarctica
title_sort mineralogy of lacustrine sediments in the schirmacher range area, eastern antarctica
publisher Geological Society of India
publishDate 2000
url http://repository.ias.ac.in/120244/
geographic East Antarctica
geographic_facet East Antarctica
genre Antarc*
Antarctica
Antarctica Journal
East Antarctica
genre_facet Antarc*
Antarctica
Antarctica Journal
East Antarctica
op_relation Sinha, Rajiv
Chatterjee, A. (2000) Mineralogy of lacustrine sediments in the Schirmacher Range Area, Eastern Antarctica Journal of the Geological Society of India, 56 (1). pp. 39-45. ISSN 0016-7622
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