The Neoarchaean Limpopo Orogeny: Exhumation and Regional-Scale Gravitational Crustal Overturn Driven by a Granulite Diapir-Reference-Cited by-同舟云学术

The Neoarchaean Limpopo Orogeny: Exhumation and Regional-Scale Gravitational Crustal Overturn Driven by a Granulite Diapir

Published:2019 Issue: Volume: Page:185-224
ISSN:2364-6438
Container-title:Regional Geology Reviews
language:
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Author:

van Reenen Dirk D.,Smit C. Andre,Perchuk Alexei L.,Huizenga Jan M.,Safonov Oleg G.,Gerya Taras V.

Publisher

Springer International Publishing

Link

http://link.springer.com/content/pdf/10.1007/978-3-319-78652-0_8

Reference127 articles.

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2. Aranovich LY, Newton RC (1999) Experimental determination of CO2–H2O activity-composition relations at 600–1000 °C and 6–14 kbar by reversed decarbonation and dehydration reactions. Am Mineral 84:1319–1332

3. Armstrong RA, Wilson AH (2000) SHRIMP U-Pb study of zircons from the layered sequence of the Great Dyke, Zimbabwe, and a granitoid anatectic dyke. Earth Planet Sci Lett 180:1–12

4. Bahnemann KP (1972) A review of the structure, the stratigraphy and the metamorphism of the basement rocks of the Messina District, Northern Transvaal. Dissertation, University of Pretoria

5. Baker J, van Reenen DD, Van Schalkwyk JF, Newton RC (1992) Constraints on the composition of fluids involved in retrograde anthophyllite formation in the Limpopo Belt, South Africa. Precambr Res 55:327–336

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