Paleoarchean (3.6–3.2 Ga) Mineral Systems in the Context of Continental Crust Building and the Role of Mantle Plumes-Reference-Cited by-同舟云学术

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Paleoarchean (3.6–3.2 Ga) Mineral Systems in the Context of Continental Crust Building and the Role of Mantle Plumes

Published:2019 Issue: Volume: Page:187-209
ISSN:
Container-title:Earth's Oldest Rocks
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Author:

Pirajno Franco,Huston David L.

Publisher

Elsevier

Reference197 articles.

1. The intensity, occurrence and duration of superplume events and eras over geological time;Abbott;Journal of Geodynamics,2002

2. Trace element zoning of sulfides and quartz at Sheba and Fairview gold mines: clues to Mesoarchean mineralisation in the Barberton greenstone belt, South Africa;Agangi;Ore Geology Reviews,2014

3. Radiogenic isotopes: the case for crustal recycling on a near-steady-state no-continental growth earth;Armstrong;Philosophical Transactions of the Royal Society of London Series A,1981

4. Supercontinent cycles and the distribution of metal deposits through time;Barley;Geology,1992

5. Late Archean to early proterozoic global tectonics, environmental change and the rise of atmospheric oxygen;Barley;Earth and Planetary Science Letters,2005

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1. The evolution from plate margin to intraplate mineral systems in the Capricorn Orogen, links to prospectivity;Ore Geology Reviews;2020-12

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