1887

Abstract

Regional greenschist facies metamorphism (350±50°C, ca 2.5 kbar) of sediments in the Witwatersrand Basin<br>implies that crustal temperatures were significantly elevated at some time in the Late Archaean and<br>Palaeoproterozoic relative to present day temperatures.

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/content/papers/10.3997/2214-4609-pdb.154.014
2005-09-14
2021-01-22
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.154.014
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