Magmatic Complexes of the Vetlovaya Marginal Sea Paleobasin (Kamchatka): Composition and Geodynamic Setting
- Authors: Tsukanov N.V.1, Saveliev D.P.2, Kovalenko D.V.3
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Affiliations:
- Shirshov Institute of Oceanology
- Institute of Seismology and Volcanology, Far East Branch
- Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry
- Issue: Vol 58, No 1 (2018)
- Pages: 92-106
- Section: Marine Geology
- URL: https://bakhtiniada.ru/0001-4370/article/view/149613
- DOI: https://doi.org/10.1134/S0001437018010162
- ID: 149613
Cite item
Abstract
This study presents new geochemical and isotope data on igneous rocks of the Vetlovaya marginal sea paleobasin (part of the Late Mesozoic–Cenozoic margin of the northwestern Pacific). The results show that the rock complexes of this marginal sea basin comprise igneous rocks with geochemical compositions similar to those of normal oceanic tholeiites, enriched transitional tholeiites, and ocean island and back-arc basin basalts. Island-arc tholeiitic basalts are present only rarely. The specific geochemical signatures of these rocks are interpreted as being related to mantle heterogeneity and the geodynamic conditions in the basin.
About the authors
N. V. Tsukanov
Shirshov Institute of Oceanology
Author for correspondence.
Email: nvts_ov@rambler.ru
Russian Federation, Moscow
D. P. Saveliev
Institute of Seismology and Volcanology, Far East Branch
Email: nvts_ov@rambler.ru
Russian Federation, Petropavlovsk–Kamchatsky
D. V. Kovalenko
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry
Email: nvts_ov@rambler.ru
Russian Federation, Moscow
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