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Journal of Geophysical Research | Vol.59, Issue.2 | | Pages 223-232

The permanent magnetisation of horizontal volcanic sheets

T. Hatherton

Abstract

The magnetisation of igneous rocks is often largely due to thermoremanent components. Several horizontal sheets of acid tuffs in New Zealand exhibit similar magnetisation patterns. Each sheet has a basic minimum Q

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The permanent magnetisation of horizontal volcanic sheets

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Keywords

magnetisation of minimum

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T. Hatherton,.The permanent magnetisation of horizontal volcanic sheets. 59 (2),223-232.

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