Faults and Source Parameters of Earthquakes in the Baikal Rift Zone: Dip Angles of Fault Planes

被引：1
|
作者：
Dem'yanovich, V. M. [1 ]
Klyuchevskii, A. V. [1 ]
机构：
[1] Russian Acad Sci, Inst Earths Crust, Siberian Branch, Irkutsk 664033, Russia
来源：
DOKLADY EARTH SCIENCES | 2018年 / 479卷 / 02期
基金：
俄罗斯基础研究基金会;
关键词：
The work was supported in part by the Russian Foundation for Basic Research; project nos. 14–45– 04011-r_Sibir’_a and 14–05–00308_a;
D O I：
10.1134/S1028334X18040128
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
Analysis of gentle, intermediate, and steep dip angles of fault planes in earthquake sources of the Baikal region is carried out with the slips in seismic sources being taken into account. The areas where normal faulting slips at steep, intermediate, and gentle angles took place are distinguished, and this can be interpreted as transformation of a steep dip to gentle one. It is found that the increase in energy class is accompanied by the number of earthquakes with steep dip angles, whereas the proportion of earthquakes with intermediate angles decreases, and the fraction of earthquakes with gentle angles remains quasi-stable and small.
引用
收藏
页码：433 / 438
页数：6
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