SURFACE FAULT TRACES AND FAULT PLANE SOLUTIONS OF THE MAY-JUNE 1978 MAJOR SHOCKS IN THE THESSALONIKI AREA, GREECE

被引：79

作者：

PAPAZACHOS, B

MOUNTRAKIS, D

PSILOVIKOS, A

LEVENTAKIS, G

机构：

[1] ARISTOTELIAN UNIV SALONIKA,GEOL LAB,SALONIKA,GREECE

[2] ARISTOTELIAN UNIV SALONIKA,LAB PHYS GEOL,SALONIKA,GREECE

来源：

TECTONOPHYSICS | 1979年 / 53卷 / 3-4期

关键词：

D O I：

10.1016/0040-1951(79)90061-1

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

It is shown that the foci of the recent earthquakes in the Thessaloniki area of northern Greece are located in an arcuate seismic zone which is associated with the Serbomacedonian geologic zone. Three main lines of fracture have been observed in the epicentral area after the May-June 1978 earthquakes. Field and macroseismic observations as well as fault plane solutions for the main shock and for the largest foreshock show that both earthquakes are due to a strike slip sinistral motion with a small reverse component on a steeply dipping and trending southeast-northwest fault. © 1979.

引用

页码：171 / 183

页数：13