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Deep electrical conductivity structure in the Great Wall Station area, Fildes Peninsula, West Antarctica

Xiangru, Kong and Jianjun, Zhang (1994) Deep electrical conductivity structure in the Great Wall Station area, Fildes Peninsula, West Antarctica. Advances in Polar Science, 5 (1). pp. 11-20.

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Abstract

MT measured in Great Wall Station area shows that the electrical conductivity major axis of the Wind Valley Fault is 110° NE and the crustal thickness in the Fildes Peninsula is about 22.3 km. The crust contains four main resistivity layers with their thickness being 1.3km, 6.7km, 1.2km and 13.1km respectively. The upper crustal thickness is 9.2,m and the lower crustal thickness is 13.1km.

Item Type: Article
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    Date Deposited: 11 Apr 2023 14:09
    URI: http://library.arcticportal.org/id/eprint/2071

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