Radon activity of faults (western Baikal and southern Angara areas)

被引：28

作者：

Seminsky, K. Zh. ^{[1
]}

Bobrov, A. A. ^{[1
]}

机构：

[1] RAS, Siberian Branch, Inst Earths Crust, Irkutsk 664033, Russia

来源：

RUSSIAN GEOLOGY AND GEOPHYSICS | 2009年 / 50卷 / 08期

基金：

俄罗斯基础研究基金会;

关键词：

radon; fault; tectonic activity; Baikal rift; Siberian craton; SOIL-GAS RADON; ANOMALIES; PART;

D O I：

10.1016/j.rgg.2008.12.010

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

We report results of transect radon surveys on twenty six large and small faults of different geometries in the western Baikal and southern Angara (southern Siberian craton) areas. The studied faults show up in the radon field as broad zones of high radon activity concentration, with their widths 1.4 times the widths of faulting-related deformation zones. Other things being equal, radon emanation depends on the size and slip geometry of faults and on their activity in the Cenozoic. Relative radon activity is higher in rift faults than in cratonic ones, in normal relative to strike-slip faults, and in larger and more active faults, the latter factor being the basic geodynamic control of radon emanation. (C) 2009, IGM, Siberian Branch of the RAS. Published by Elsevier B. V. All rights reserved.

引用

页码：682 / 692

页数：11

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