NEW DATA ON THE STRUCTURE AND COMPOSITION OF GABBROIDS AND PLAGIOGRANITES FROM THE LATE CRETACEOUS OPHIOLITIC COMPLEX OF THE KAMCHATSKY MYS PENINSULA (EASTERN KAMCHATKA)
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dc.contributor.author | Tsukanov N.V. | |
dc.contributor.author | Luchitskaya M.V. | |
dc.contributor.author | Skolotnev S.G. | |
dc.contributor.author | Kramer W. | |
dc.contributor.author | Seifert W. | |
dc.date.accessioned | 2022-08-03T05:21:02Z | |
dc.date.available | 2022-08-03T05:21:02Z | |
dc.date.issued | 2004 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13467740 | |
dc.identifier.citation | Doklady Earth Sciences, 2004, 397, 5, 632-635 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/38481 | |
dc.description.abstract | The complex petro-, geochemical and mineralogical investigation of gabbroides and associating with them plagiogranites permits to conclude that formation of the gabbroic pluton, which fragments are mapped in 1-ya Olchovaya river headwater, proceeded under per-subduction conditions within the island arc system. Apparently gabbroides and plagiogranites are derivatives of the island-arc toleite melts. The conducted study confirms the validity of uniting gabbroides and plagiogranites in the integral ophiolite complex with highly depleted peridotites of Soldatskaya mountain massif and island-arc toleitic basalts and boninites of Tarchov suite. Gabbro-plagiogranite pluton is a fragment of the bedding of upper-Cretaceous Kronot early island arc. | |
dc.subject | Cretaceous | |
dc.title | NEW DATA ON THE STRUCTURE AND COMPOSITION OF GABBROIDS AND PLAGIOGRANITES FROM THE LATE CRETACEOUS OPHIOLITIC COMPLEX OF THE KAMCHATSKY MYS PENINSULA (EASTERN KAMCHATKA) | |
dc.type | Статья | |
dc.subject.age | Mesozoic::Cretaceous | |
dc.subject.age | Мезозой::Меловая | ru |
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