Holocene deformation in the western end of the Tunka system of rift basins (Southwestern Baikal Rift)

被引：0
|
作者：
Arzhannikova, AV
Larroque, C
Arzhannikov, SG
机构：
[1] Russian Acad Sci, Inst Earth Crust, Irkutsk 664030, Russia
[2] CNRS, Geosci Res Assoc, F-6526 Valbonne, France
来源：
GEOLOGIYA I GEOFIZIKA | 2003年 / 44卷 / 04期
关键词：
tectonic deformation; fault kinematics; earthquake; strain field;
D O I：
暂无
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
We investigate the geometry and kinematics of Holocene active compressional structures in the Mondy basin and its surroundings (western termination of the Tunka system of rift basins) and continue the discussion on the M = 7 Mondy earthquake of 4 April 1950. The Holocene reverse-oblique motions along the W-E trending Mondy and Ikh-Uhgon faults are interpreted in the context of Late Cenozoic evolution of a flower structure, on the basis of deciphered digital SPOT (10 m resolution) and Landsat (30 m resolution) imagery and field geomorphological measurements.
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页码：373 / 379
页数：7
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