Field, geochemical and U-Pb isotopic constraints from hypabyssal felsic intrusions within the Barberton greenstone belt, South Africa: Implications for tectonics and the timing of gold mineralization-Reference-Cited by-同舟云学术

Field, geochemical and U-Pb isotopic constraints from hypabyssal felsic intrusions within the Barberton greenstone belt, South Africa: Implications for tectonics and the timing of gold mineralization

Published:1991-02 Issue:3-4 Volume:49 Page:261-280
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

de Ronde C.E.J.,Kamo S.,Davis D.W.,de Wit M.J.,Spooner E.T.C.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference39 articles.

1. Strontium isotopic studies of the mafic and felsic rocks of the Onverwacht Group of the Swaziland sequence;Allsopp;Geol. Rundsch.,1973

2. Facets of the granitic assemblages on the northwest flank of the Barberton Mountain Land;Anhaeusser,1966

3. Archean gold mineralization in the Barberton Mountain Land;Anhaeusser,1986

4. Notes on the provisional geological map of the Barberton Greenstone Belt and surrounding granitic terrane, Eastern Transvaal and Swaziland (1: 250,000 color map);Anhaeusser;Geol. Soc. S. Afr. Spec. Publ.,1983

5. The stratigraphy of the 3.5-3.2 Ga Barberton greenstone belt revisited: a single zircon ion microprobe study;Armstrong;Earth Planet. Sci. Lett.,1990

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