Magnetotelluric sounding study in the region of Zhongshan Station, East Antarctica

This paper deals with the results of the MT observations in the region of Zhongshan Station, Larsemann Hills area, East Antarctica and points out that the lithosphere thickness of the Larsemann Hills is 140 km and the crustal high conductivity layer is situated in 22 km.

Bibliographic Details
Main Authors: Xiangru, Kong, Jianjun, Zhang
Format: Article in Journal/Newspaper
Language:English
Published: Polar Research Institute of China - PRIC 1995
Subjects:
East Antarctica
Larsemann Hills
Zhongshan
Zhongshan Station
Advances in Polar Science
Antarc*
Antarctica
Polar Science
Online Access:http://library.arcticportal.org/2089/
http://library.arcticportal.org/2089/1/A501.002.pdf
id ftarcticportal:oai:generic.eprints.org:2089
record_format openpolar
spelling ftarcticportal:oai:generic.eprints.org:2089 2023-06-11T04:02:59+02:00 Magnetotelluric sounding study in the region of Zhongshan Station, East Antarctica Xiangru, Kong Jianjun, Zhang 1995-06 application/pdf http://library.arcticportal.org/2089/ http://library.arcticportal.org/2089/1/A501.002.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2089/1/A501.002.pdf Xiangru, Kong and Jianjun, Zhang (1995) Magnetotelluric sounding study in the region of Zhongshan Station, East Antarctica. Advances in Polar Science, 6 (1). pp. 24-29. Article PeerReviewed 1995 ftarcticportal 2023-04-19T22:52:31Z This paper deals with the results of the MT observations in the region of Zhongshan Station, Larsemann Hills area, East Antarctica and points out that the lithosphere thickness of the Larsemann Hills is 140 km and the crustal high conductivity layer is situated in 22 km. Article in Journal/Newspaper Advances in Polar Science Antarc* Antarctica East Antarctica Polar Science Polar Science Arctic Portal Library East Antarctica Larsemann Hills ENVELOPE(76.217,76.217,-69.400,-69.400) Zhongshan ENVELOPE(76.371,76.371,-69.373,-69.373) Zhongshan Station ENVELOPE(76.371,76.371,-69.373,-69.373)
institution Open Polar
collection Arctic Portal Library
op_collection_id ftarcticportal
language English
description This paper deals with the results of the MT observations in the region of Zhongshan Station, Larsemann Hills area, East Antarctica and points out that the lithosphere thickness of the Larsemann Hills is 140 km and the crustal high conductivity layer is situated in 22 km.
format Article in Journal/Newspaper
author Xiangru, Kong
Jianjun, Zhang
spellingShingle Xiangru, Kong
Jianjun, Zhang
Magnetotelluric sounding study in the region of Zhongshan Station, East Antarctica
author_facet Xiangru, Kong
Jianjun, Zhang
author_sort Xiangru, Kong
title Magnetotelluric sounding study in the region of Zhongshan Station, East Antarctica
title_short Magnetotelluric sounding study in the region of Zhongshan Station, East Antarctica
title_full Magnetotelluric sounding study in the region of Zhongshan Station, East Antarctica
title_fullStr Magnetotelluric sounding study in the region of Zhongshan Station, East Antarctica
title_full_unstemmed Magnetotelluric sounding study in the region of Zhongshan Station, East Antarctica
title_sort magnetotelluric sounding study in the region of zhongshan station, east antarctica
publisher Polar Research Institute of China - PRIC
publishDate 1995
url http://library.arcticportal.org/2089/
http://library.arcticportal.org/2089/1/A501.002.pdf
long_lat ENVELOPE(76.217,76.217,-69.400,-69.400)
ENVELOPE(76.371,76.371,-69.373,-69.373)
ENVELOPE(76.371,76.371,-69.373,-69.373)
geographic East Antarctica
Larsemann Hills
Zhongshan
Zhongshan Station
geographic_facet East Antarctica
Larsemann Hills
Zhongshan
Zhongshan Station
genre Advances in Polar Science
Antarc*
Antarctica
East Antarctica
Polar Science
Polar Science
genre_facet Advances in Polar Science
Antarc*
Antarctica
East Antarctica
Polar Science
Polar Science
op_relation http://library.arcticportal.org/2089/1/A501.002.pdf
Xiangru, Kong and Jianjun, Zhang (1995) Magnetotelluric sounding study in the region of Zhongshan Station, East Antarctica. Advances in Polar Science, 6 (1). pp. 24-29.
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