3.07-2.97 Ga greenstone belt formation in the northeastern Kaapvaal Craton; implications for the origin of the Witwatersrand Basin

Abstract

Other| December 01, 1996 3.07-2.97 Ga greenstone belt formation in the northeastern Kaapvaal Craton; implications for the origin of the Witwatersrand Basin Marc Poujol; Marc Poujol Universite Montpellier II, Montpellier, France Search for other works by this author on: GSW Google Scholar Laurence J. Robb; Laurence J. Robb Search for other works by this author on: GSW Google Scholar Jean-Patrick Respaut; Jean-Patrick Respaut Search for other works by this author on: GSW Google Scholar Carl R. Anhaeusser Carl R. Anhaeusser Search for other works by this author on: GSW Google Scholar Author and Article Information Marc Poujol Universite Montpellier II, Montpellier, France Laurence J. Robb Jean-Patrick Respaut Carl R. Anhaeusser Publisher: Society of Economic Geologists First Online: 02 Mar 2017 Online ISSN: 1554-0774 Print ISSN: 0361-0128 GeoRef, Copyright 2004, American Geological Institute. Economic Geology (1996) 91 (8): 1455–1461. https://doi.org/10.2113/gsecongeo.91.8.1455 Article history First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Marc Poujol, Laurence J. Robb, Jean-Patrick Respaut, Carl R. Anhaeusser; 3.07-2.97 Ga greenstone belt formation in the northeastern Kaapvaal Craton; implications for the origin of the Witwatersrand Basin. Economic Geology 1996;; 91 (8): 1455–1461. doi: https://doi.org/10.2113/gsecongeo.91.8.1455 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyEconomic Geology Search Advanced Search This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.