Recent developments of the Middle East catalog

被引:116
作者
Zare, Mehdi [1 ]
Amini, Hamideh [1 ]
Yazdi, Pouye [1 ]
Sesetyan, Karin [2 ,3 ]
Demircioglu, Mine Betul [2 ,3 ]
Kalafat, Dogan [2 ,3 ]
Erdik, Mustafa [2 ,3 ]
Giardini, Domenico [4 ]
Khan, M. Asif [5 ]
Tsereteli, Nino [6 ]
机构
[1] IIEES, Tehran, Iran
[2] Bogazici Univ, Kandili Observ, Istanbul, Turkey
[3] Bogazici Univ, Earthquake Res Inst, Istanbul, Turkey
[4] ETH, Inst Geophys, CH-8093 Zurich, Switzerland
[5] Univ Peshawar, Natl Ctr Excellence Geol, Peshawar, Pakistan
[6] Georgian Acad Sci, Inst Geophys, Dept Seismol & Expt Geophys, Tbilisi, Georgia
关键词
Seismicity; Catalog; Middle East; Depth; Historical; Instrumental; Magnitude; EFFECTIVE ELASTIC THICKNESS; DAY CRUSTAL DEFORMATION; SOURCE PARAMETERS; PLATE KINEMATICS; FOCAL DEPTHS; EARTHQUAKES; CONSTRAINTS; CALIFORNIA; TECTONICS; BENEATH;
D O I
10.1007/s10950-014-9444-1
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
This article summarizes a recent study in the framework of the Global Earth model (GEM) and the Earthquake Model of the Middle East (EMME) project to establish the new catalog of seismicity for the Middle East, using all historical (pre-1900), early and modern instrumental events up to 2006. According to different seismicity, which depends on geophysical, geological, tectonic, and seismicity data, this region is subdivided to nine subregions, consisting of Alborz-Azerbaijan, Afghanistan-Pakistan, Saudi Arabia, Caucasus, Central Iran, Kopeh-Dagh, Makran, Zagros, and Turkey (Eastern Anatolia; after 30A degrees E). After omitting the duplicate events, aftershocks, and foreshocks by using the Gruenthal method, and uniform all magnitude to Mw scale, 28,244 main events remain for the new catalog of Middle East from 1250 B.C. through 2006. The magnitude of completeness (Mc) was determined as 4.9 for five out of nine subregions, where the least values of Mc were found to be 4.2. The threshold of Mc is around 5.5, 5.0, 4.5, and 4.0, for the time after 1950, 1963, 1975, and 2000, respectively. The average of teleseismic depths in all regions is less than 15 km. Totally, majority of depth for Kopeh-Dagh and Central Iran, Zagros, and Alborz-Azerbaijan, approximately, is 15, 13, and 11 km and for Afghanistan-Pakistan, Caucasus, Makran, Turkey (after 30A degrees E), and Saudi Arabia is about 9 km.
引用
收藏
页码:749 / 772
页数:24
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