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Title: RELATION BETWEEN BASIC AND ACID MAGMATISM IN TIN-BEARING AREAS OF EASTERN YAKUTIA
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RELATION BETWEEN BASIC AND ACID MAGMATISM IN TIN-BEARING AREAS OF EASTERN YAKUTIA
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1314-2704
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English
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18
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1.1
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The article concentrates on relation of mineralization, granitoid magmatism and dikes in ore fields of the Eastern Yakutia with cassiterite-sulfide mineralization. It is shown that, the main ore bodies are confined to places of intensive development of dikes and do not significantly concur with the time of granitoid formation. The melts that formed dikes and generated into metasomatised mantle, was the main source of tin and accompanying elements. When centers of granitoid and dike eruption are the same, these melts were additional sources of heat and volatile components, that provided duration of granite system evolution and additional mobilization of ore material.
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conference
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18th International Multidisciplinary Scientific GeoConference SGEM 2018
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18th International Multidisciplinary Scientific GeoConference SGEM 2018, 02-08 July, 2018
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Proceedings Paper
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STEF92 Technology
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International Multidisciplinary Scientific GeoConference-SGEM
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Bulgarian Acad Sci; Acad Sci Czech Republ; Latvian Acad Sci; Polish Acad Sci; Russian Acad Sci; Serbian Acad Sci & Arts; Slovak Acad Sci; Natl Acad Sci Ukraine; Natl Acad Sci Armenia; Sci Council Japan; World Acad Sci; European Acad Sci, Arts & Letters; Ac
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577-588
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02-08 July, 2018
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website
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cdrom
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73
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granitoids; mantle magmatism; sources of ore elements
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