The significance of 3000 Ma granulite-facies mafic dikes in the central zone of the Limpopo belt, southern Africa-Reference-Cited by-同舟云学术

The significance of 3000 Ma granulite-facies mafic dikes in the central zone of the Limpopo belt, southern Africa

Published:1990-10 Issue:3 Volume:48 Page:299-308
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Barton J.M.,van Reenen D.D.,Roering C.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference26 articles.

1. The chemical composition, Rb-Sr isotopic systematics and tectonic setting of certain post-kinematic mafic igneous rocks, Limpopo mobile belt, southern Africa;Barton;Precambrian Res.,1979

2. Our understanding of the Limpopo belt;Barton;Spec. Publ. Geol. Soc. S. Afr.,1983

3. Pb-isotopic evidence for the age of the Messina layered intrusion, central zone, Limpopo mobile belt;Barton;Spec. Publ. Geol. Soc. S. Afr.,1983

4. Geochronologic studies in the southern marginal zone of the Limpopo mobile belt, southern Africa;Barton;Spec. Publ. Geol. Soc. S. Afr.,1983

5. Rb-Sr ages and chemical composition of some deformed Archaean mafic dykes, central zone, Limpopo mobile belt, southern Africa;Barton;Spec. Publ. Geol. Soc. S. Afr.,1983

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