Submeridional boundary zone in Asia: seismicity, lithosphere structure, and the distribution of convective flows in the upper mantle
The study is focused on the submeridional transregional boundary that stretches as a wide band along 105°E in Central Asia. In modern seismic models, it is traceable to a depth of ~600 km. In the continental area to the west of this boundary, seismic activity is increased. Following the study of the...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2018-10-01
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Series: | Геодинамика и тектонофизика |
Subjects: | |
Online Access: | https://www.gt-crust.ru/jour/article/view/635 |