Tectonic Structure and Evolution of the Lithosphere in the Near-Antarctic Part of the South Atlantic

被引：1
作者：
Dubinin, E. P. [1 ]
Kokhan, A. V. [2 ]
Suschevskaya, N. M. [3 ]
机构：
[1] Moscow MV Lomonosov State Univ, Earth Sci Museum, Moscow, Russia
[2] Russian Acad Sci, Geol Inst, Moscow, Russia
[3] Russian Acad Sci, Vernadsky Inst Geochem & Analyt Chem, Moscow, Russia
来源：
OCEANOLOGY | 2024年 / 64卷 / 01期
基金：
俄罗斯科学基金会;
关键词：
relief; morphostructures; tectonics; crust structure; evolution; South Atlantic; MOZAMBIQUE RIDGE; AGULHAS PLATEAU; INDIAN-OCEAN; EAST ANTARCTICA; NATAL VALLEY; AFRICA; MANTLE; MODEL; RECONSTRUCTIONS; KINEMATICS;
D O I：
10.1134/S0001437024010053
中图分类号：
P7 [海洋学];
学科分类号：
0707 ;
摘要：
Based on an analysis of global digital models, the distribution of fracture zones of the oceanic crust, global and regional models of evolution, and published geological and geophysical data, the structural features of the ocean floor in the junction area of the Indian and Atlantic oceans are considered. Tectonic zoning of the region's crust has been carried out. Heterogeneous blocks of the lithosphere with crust formed on different spreading ridges, separated by structural boundaries, which are pseudofaults, fixing traces of propagating rift zones, jumping and cessation of spreading ridges are identified. The main stages in the evolution of the lithosphere associated with the activation of plume magmatism and kinematic reorganizations of plate boundaries are identified.
引用
收藏
页码：81 / 95
页数：15
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