Original Research
Regional microthermometric data base for the Proterozoic rocks of the Northwestern Cape Province
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
Submitted: 08 July 1990 | Published: 08 July 1990
About the author(s)
A. E. Schoch,, South AfricaE. Klatt,, South Africa
D. Elsmere,, South Africa
Full Text:
PDF (741KB)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
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