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Amphibolite facies metamorphism in the Schapenburg schist belt: A record of the mid-crustal response to ~3.23 Ga terrane accretion in the Barberton greenstone belt

Stevens, Gary; Droop, G T R; Armstrong, Richard; Anhaeusser, C.R.


The Schapenburg Schist Belt is one of several large greenstone remnants exposed in the granitoid-dominated terrane to the south of the Barberton greenstone belt and is unique in that it contains a well-developed metasedimetary sequence in addition to the

CollectionsANU Research Publications
Date published: 2002
Type: Journal article
Source: South African Journal of Geology


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