Camptonites of Southern Dzungaria and questions of their genesis
Abstract
In recent years, on the southern slopes of the Dzungarian Alatau discovered and studied peculiar vein alkaline-basaltoid rocks, which correspond to the totality of geological and petrographic-mineralogical features of camptonites. A characteristic feature of these rocks is the abundance of various clastic inclusions, mostly of deep origin. The study of these inclusions is of undoubted interest in connection with the problem of genesis of lamprophyres and the structure of deep horizons of the Earth's crust and upper mantle.
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(Archived) Without section
References
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