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Abstract

Magnetotelluric (MT) results from three diverse tectonic settings exhibit strong correlations between increased electrical conductivity and expected depths of enhanced crustal strain. The environments are a young caldera complex and the Basin and Range (BR) Province, both in North America, and the transpressional Southern Alps of New Zealand. Conductivity patterns at >10 Ian beneath the Valles caldera are strongly congruent with isotherms projected from geothermal drill holes up to 4.5 Ian deep.

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/content/papers/10.3997/2214-4609-pdb.299.237
1997-11-07
2021-12-05
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.299.237
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