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- W2022650277 abstract "Limited geologic and petrographic data and rather extensive chemical data are presented for several of the alkalic and associated masses of Tuva. The alkalic rocks and middle Paleozoic granites of the Syutkhol' intrusive complex were genetically related as well as nearly contemporaneous. It is concluded that the alkalic rocks are differentiates of a granitic magma during the late stages of middle Paleozoic igneous activity. The differentiation proceeded most likely at the periphery of multichambered magmatic centers or isolated reservoirs within Precambrian structural zones. A relatively stable tectonic regimen is believed to be a prerequisite for alkalic rocks. Periodically active faults provided vents for a rising alkalic magma and promoted its further differentiation as a result of the changing magmatic gas regimens. The effect on the enclosing rocks undersaturated in silica was a possible factor in the emergence of alkalic magma. --R. V. Dietrich." @default.
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- W2022650277 date "1963-10-01" @default.
- W2022650277 modified "2023-09-25" @default.
- W2022650277 title "ALKALIC INTRUSIONS IN THE NORTHEAST OF TUVA" @default.
- W2022650277 doi "https://doi.org/10.1080/00206816309473873" @default.
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