Research output: Contribution to journal › Article › peer-review
The Structure of the Tectonosphere in the Marginal Zones of the Kerguelen Plateau Based on Geological and Geophysical Data. / Dubinin, E. P.; Shaikhullina, A. A.; Bulychev, A. A.; Leitchenkov, G. L.; Maksimova, A. A.
In: Moscow University Geology Bulletin, Vol. 75, No. 4, 01.07.2020, p. 317-329.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - The Structure of the Tectonosphere in the Marginal Zones of the Kerguelen Plateau Based on Geological and Geophysical Data
AU - Dubinin, E. P.
AU - Shaikhullina, A. A.
AU - Bulychev, A. A.
AU - Leitchenkov, G. L.
AU - Maksimova, A. A.
N1 - Funding Information: This work was supported by the Russian Foundation for Basic Research (project no. 18-05-00127) and by the Russian Science Foundation (project no. 16-17-10139). Publisher Copyright: © 2020, Allerton Press, Inc. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2020/7/1
Y1 - 2020/7/1
N2 - Abstract: The Kerguelen Plateau is the largest submarine rise in the southern Indian Ocean. The heterogeneous structure of the crust, plume magmatic activity, and different ages of the adjacent basins indicate different structures of different marginal zones of the plateau. On the basis of geological and geophysical information, various morphodynamic types of margins of the Kerguelen Plateau are identified. Analysis of the bottom topography and potential field data, together with two-dimensional density modeling, allows us to specify the deep structure of the tectonosphere in the Kerguelen Plateau margins and take a fresh look at their nature.
AB - Abstract: The Kerguelen Plateau is the largest submarine rise in the southern Indian Ocean. The heterogeneous structure of the crust, plume magmatic activity, and different ages of the adjacent basins indicate different structures of different marginal zones of the plateau. On the basis of geological and geophysical information, various morphodynamic types of margins of the Kerguelen Plateau are identified. Analysis of the bottom topography and potential field data, together with two-dimensional density modeling, allows us to specify the deep structure of the tectonosphere in the Kerguelen Plateau margins and take a fresh look at their nature.
KW - crust
KW - Indian Ocean
KW - Kerguelen Plateau
KW - margins
KW - potential fields
UR - http://www.scopus.com/inward/record.url?scp=85092484511&partnerID=8YFLogxK
U2 - 10.3103/S0145875220040043
DO - 10.3103/S0145875220040043
M3 - Article
AN - SCOPUS:85092484511
VL - 75
SP - 317
EP - 329
JO - Moscow University Geology Bulletin
JF - Moscow University Geology Bulletin
SN - 0145-8752
IS - 4
ER -
ID: 70402082