1887

Abstract

The Vredefort dome exhibits unique geological and geophysical features compared with other known impact<br>craters, and one of these is a negative magnetic anomaly over the basement rocks near the centre of the crater. In<br>this study we conducted a magnetic survey across the amphibolite-granulite transition.

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/content/papers/10.3997/2214-4609-pdb.154.011
2005-09-14
2021-03-08
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.154.011
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