1887

Abstract

The Midland Valley of Scotland is associated with strong anomalies in the gravity and magnetic domains and a distinct velocity structure. Exposed Lower Carboniferous alkali-olivine basalts have a mean volume susceptibility of about 0.06 SI; approximately twice that for Devonian andesitic lavas.

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/content/papers/10.3997/2214-4609.201409311
1995-05-29
2020-11-23
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409311
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