Archaean megacrystic plagioclase units and the tectonic setting of greenstones
Large (up to 20 cm), equidimensional, commonly euhedral, plagioclase megacrysts of highly calcic composition (An sub 80-90) occur commonly in all Archean cratons in one or more of three distinct associations: (1) as cumulate crystal segregations of anorthosite or as megacrysts in basaltic dikes, sil...
Main Authors: | , , |
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Format: | Other/Unknown Material |
Language: | unknown |
Published: |
1986
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Online Access: | http://hdl.handle.net/2060/19860013651 |