Specific features of the seismic regime in the lithosphere: Manifestations of the deep aqueous fluid action

被引：0

作者：

B. V. Levin

M. V. Rodkin

E. V. Sasorova

机构：

[1] Russian Academy of Sciences,Institute of Marine Geology and Geophysics, Far East Division

[2] Russian Academy of Sciences,Geophysical Center

[3] Russian Academy of Sciences,Shirshov Institute of Oceanology

来源：

Izvestiya, Physics of the Solid Earth | 2010年 / 46卷

关键词：

Lithosphere; Solid Earth; Seismic Moment; Depth Interval; Rock Interaction;

D O I：

暂无

中图分类号：

学科分类号：

摘要：

We considered the seismic regime in the upper 70–100 km of the lithosphere and identified the layers (at depths of about 10, 20–30, and 60–80 km) characterized by relatively reduced effective strength and increased seismicity. The existence of such layers is related to changes in the regime of fluid-rock interaction, namely, to the characteristic depths of a jump-like decrease in the effective permeability of rocks and an increase in the spatial homogeneity of a fluid-rock system.

引用

页码：451 / 459

页数：8

共 9 条

[1] Specific Features of the Seismic Regime in the Lithosphere: Manifestations of the Deep Aqueous Fluid Action
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IZVESTIYA-PHYSICS OF THE SOLID EARTH, 2010, 46 (05) : 451 - 459
[2] Specific features of the seismic regime in an area of minor earthquakes in the central Hellenic arc
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[9] Specific features of the fluid regime during the formation of systems with copper-molybdenum-gold and copper-tin mineralizations (Iskra-Soboliny knot, Kavalerovo ore district, Primorye)
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