Abstract
The ancient crystalline base is found to be intricately wrench-faulted, with considerable movement of its blocks up, down, and sideways, along the principal and subsidiary fractures. There is a very good correspondence between the tectonic structure of the base and structures of its sedimentary overburden. A connection between tectonic structure of the base and kimberlitic magmatism is definitely indicated. -- V.P. Sokoloff
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