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SOURCE GEOMETRY AND MECHANISM OF 1978 TABS, IRAN, EARTHQUAKE FROM WELL LOCATED AFTRERSHOCK
Aftershock of the September 16, 1978 Tabas earthquake located from close-in observations madeduring a four-week fielding of temporary stations have been analyzed for the purpose of delineating detailed source geometry of ...
SEISMICITY OF THE IRANIAN PLATEAU AND BORDERING REGIONS
Seismicity of the Iranian Plateau and bordering regions during the past 22½ yr
from 1 July 1957 through December 1979 is investigated in four successive time
intervals by analyzing close to 4000 earthquakes ...
Seismic dissipation in deep seismic zones from spectral ratio of sP/P
Observed variation of amplitude ratios of sP and P phases with frequency is used for a study of inelastic properties of upper mantle in the region of deep focus earthquakes. Results are compared with those derived from ...
Seismicity of Iranian plateau and Hindu Kush region based on 20 years of seismic activity.
All reported earthquakes of magnitude 4 and above which occurred between 20 and 40 1\\orth Latitude and between 40 and 75 1 East Longitude during the 20 years period ended on June 30,1977 are analysed. On the basis of ...