MID-CRETACEOUS EPISODIC MAGMATISM AND TIN MINERALIZATION IN KHINGAN-OKHOTSK VOLCANO-PLUTONIC BELT, FAR EAST RUSSIA

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dc.contributor.author Vrublevsky A.A.
dc.contributor.author Rodionov S.M.
dc.contributor.author Romanovsky N.P.
dc.contributor.author Nedachi M.
dc.contributor.author Sato K.
dc.date.accessioned 2021-06-07T12:43:25Z
dc.date.available 2021-06-07T12:43:25Z
dc.date.issued 2002
dc.identifier https://elibrary.ru/item.asp?id=13393098
dc.identifier.citation Resource Geology, 2002, 52, 1, 1-14
dc.identifier.issn 1344-1698
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/28867
dc.description.abstract Age of magmatism and tin mineralization in the Khingan-Okhotsk volcano–plutonic belt, including the Khingan, Badzhal and Komsomolsk tin fields, were reviewed in terms of tectonic history of the continental margin of East Asia. This belt consists mainly of felsic volcanic rocks and granitoids of the reduced type, being free of remarkable geomagnetic anomaly, in contrast with the northern Sikhote-Alin volcano–plutonic belt dominated by oxidized-type rocks and gold mineralization. The northern end of the Khingan-Okhotsk belt near the Sea of Okhotsk, accompanied by positive geomagnetic anomalies, may have been overprinted by magmatism of the Sikhote-Alin belt.
dc.subject Cretaceous granitoid magmatism
dc.subject Far East Russia
dc.subject Khingan
dc.subject Badzhal
dc.subject Komsomolsk
dc.subject tin mineralization
dc.subject Khingan-Okhotsk volcano-plutonic belt
dc.subject Kiselevka-Manoma accretionary complex
dc.subject Sikhote-Alin
dc.subject marginal basin
dc.title MID-CRETACEOUS EPISODIC MAGMATISM AND TIN MINERALIZATION IN KHINGAN-OKHOTSK VOLCANO-PLUTONIC BELT, FAR EAST RUSSIA
dc.type Статья
dc.subject.age Mesozoic::Cretaceous
dc.subject.age Мезозой::Меловая ru


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