The Detailed Hypocenter Distribution around the Active Fault
نویسندگان
چکیده
منابع مشابه
Active tectonic evidences related to the Main Recent Fault in the Sarvabad region, NW Iran
-Introduction The Main Recent Fault (MRF) is a seismic structure on the northwestern boundary of the Zagros belt and southern border of the Sanandaj-Sirjan belt. This fault as a major strike-slip fault consists of several segments in the Zagros collision zone. The seismic activity of the southwestern segments is greater than the northwestern segments. Several earthquake events have occurred al...
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ژورنال
عنوان ژورنال: Zisin (Journal of the Seismological Society of Japan. 2nd ser.)
سال: 2008
ISSN: 0037-1114,1883-9029,2186-599X
DOI: 10.4294/zisin.61.1_1