Implications of palaeogeotherms for the thermal history of the Witwatersrand Basin, South Africa

M. Jones

doi:10.3997/2214-4609-pdb.154.014

Implications of palaeogeotherms for the thermal history of the Witwatersrand Basin, South Africa
By M. Jones
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 9th SAGA Biennial Technical Meeting and Exhibition, Sep 2005, cp-154-00022
DOI: https://doi.org/10.3997/2214-4609-pdb.154.014

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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2005-09-14

2024-04-20

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Implications of palaeogeotherms for the thermal history of the Witwatersrand Basin, South Africa

Abstract

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Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture