The tectonic evolution of the Colbeck Archipelago, MacRobertson Land, East Antarctica
The high-grade metamorphic rocks of the Colbeck Archipelago comprise granulite facies metasedimentary gneisses and chamockitic gneisses of three ages. A suite of rocks previously mapped as the Colbeck Gneiss is shown to be composite in age and origin, consisting of metasedimentary and orthogneiss th...
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Format: | Thesis |
Language: | English |
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The University of Sydney
1993
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Online Access: | https://hdl.handle.net/2123/26733 |