The structure of tungsten deposits in Kukulbei and its environments
Authors:
Abstract
The geological structure of the Kukulbey Ridge and its environs includes metamorphic rocks of the Paleozoic, sandstone-conglomerate-shale deposits of the marine Jurassic (I1 - I2), ancient cataclastic coarse-grained granites and rocks of the Middle Cimmerian intrusive complex, represented by quartz diorites, granodiorites and granites. Young igneous rocks originated from a single magmatic reservoir. Between granodiorite and leucocratic granite there are numerous transitional rocks, connecting them into a single complex of a consistently developing intrusive process.
Область исследования:
Geology
Funding:
None
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