Variolites of the Paleoproterozoic Hekpoort Formation (Transvaal sub-basin, Kaapvaal craton): Multistage undercooling textures?

Author:

Humbert Fabien,Elburg Marlina A.,Ossa Frantz Ossa,de Kock Michiel O.,Robion Philippe

Funder

South African Department of Science and Technology

National Research Foundation (DST-NRF)–funded Centre of Excellence for Integrated Mineral and Energy Resource Analysis

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference55 articles.

1. Dacitic ocelli in mafic lavas, 3.8–3.7 Ga Isua Greenstone Belt, West Greenland: geochemical evidence for partial melting of oceanic crust and magma mixing;Appel;Chem. Geol.,2009

2. White globules in the Makuyamalava dome, Hakone volcano, central Japan;Arima;Sci. Rep. Yokohama Natl. Univ.,1988

3. Radiometric age determinations on rocks from southern Africa up to the end of 1971;Burger;Bull. Geol. Soc. South Africa,1973

4. A Regional Study of the Stratigraphy and Development of the Transvaal Basin in the Eastern and North-eastern Transvaal;Button,1973

5. Possible liquid immiscibility textures in high magnesia basalts from the Ventersdorp Supergroup, South Africa;Cawthorn;J. Geol.,1979

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