Fault mechanisms of Fennoscandian earthquakes and regional crustal stresses
作者:
Ragnar Slunga,
期刊:
Geologiska Föreningen i Stockholm Förhandlingar
(Taylor Available online 1981)
卷期:
Volume 103,
issue 1
页码: 27-31
ISSN:0016-786X
年代: 1981
DOI:10.1080/11035898109455200
出版商: Taylor & Francis Group
关键词: Earthquakes;crust;stress;mechanism;strike-slip faults;southeastern Norway;west central Norway;south central Sweden;western Estonia;Fennoscandia;N5921 N6649 E2321 E1043
数据来源: Taylor
摘要:
The eleven currently available (May 1980) source mechanisms of Fennoscandian earthquakes are analysed. The orientations of the horizontal stresses involved in the faulting are estimated from the fault solutions. The NW-SE orientation of the largest horizontal compression found in a large number of various investigations in continental Europe north of the Alps, is confirmed by the eleven source mechanisms. This result is shown to be statistically significant. The dominating type of faulting is strike-slip on close to vertical fault planes. The agreement between these earthquakes and the European regional stress field strongly suggests that the Fennoscandian earthquakes are related to tectonic forces.
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