Original Research

Regional microthermometric data base for the Proterozoic rocks of the Northwestern Cape Province

A. E. Schoch, E. Klatt, D. Elsmere
Suid-Afrikaanse Tydskrif vir Natuurwetenskap en Tegnologie | Vol 9, No 4 | a471 | DOI: https://doi.org/10.4102/satnt.v9i4.471 | © 1990 A. E. Schoch, E. Klatt, D. Elsmere | This work is licensed under CC Attribution 4.0
Submitted: 08 July 1990 | Published: 08 July 1990

About the author(s)

A. E. Schoch,, South Africa
E. Klatt,, South Africa
D. Elsmere,, South Africa

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Abstract

First results from fluid inclusion studies of the Proterozoic rocks of the Northwestern Cape, indicate unique characteristics for the fugitive constituents connected to the most important late to post-tectonic geological processes in the Namaqua mobile belt. A broad fluid consanguinity is present in different structural terranes, in spite of possibly contrasting early PT histories.

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Crossref Citations

1. The Grenvillian Namaqua fold belt adjacent to the western Kaapvaal Craton: 2. Archaean Craton and supercontinent connections
W.P. Colliston, A.E. Schoch, J. Cole
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doi: 10.1016/j.precamres.2017.07.032