Recent developments of the Middle East catalog
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. Accordi...
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| Veröffentlicht in: | Journal of seismology 2014-10, Vol.18 (4), p.749-772 |
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| creator | Zare, Mehdi Amini, Hamideh Yazdi, Pouye Sesetyan, Karin Demircioglu, Mine Betul Kalafat, Dogan Erdik, Mustafa Giardini, Domenico Khan, M. Asif Tsereteli, Nino |
| description | 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 30° 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 30° E), and Saudi Arabia is about 9 km. |
| doi_str_mv | 10.1007/s10950-014-9444-1 |
| format | Article |
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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 30° E), and Saudi Arabia is about 9 km.</description><identifier>ISSN: 1383-4649</identifier><identifier>EISSN: 1573-157X</identifier><identifier>DOI: 10.1007/s10950-014-9444-1</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Arabia ; Earth and Environmental Science ; Earth models ; Earth Sciences ; Earth, ocean, space ; Earthquakes ; Earthquakes, seismology ; Engineering and environment geology. Geothermics ; Exact sciences and technology ; Geophysics ; Geophysics/Geodesy ; Geotechnical Engineering & Applied Earth Sciences ; Hydrogeology ; Internal geophysics ; Natural hazards: prediction, damages, etc ; Original Article ; Plate tectonics ; Reproduction ; Seismic activity ; Seismic phenomena ; Seismicity ; Seismology ; Structural Geology ; Tectonics ; Tectonics. Structural geology. Plate tectonics</subject><ispartof>Journal of seismology, 2014-10, Vol.18 (4), p.749-772</ispartof><rights>Springer Science+Business Media Dordrecht 2014</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c412t-3f2838c629848f7221a2716bfb825a02dbfc02bc742f0f5b9b2e847ccb721bf93</citedby><cites>FETCH-LOGICAL-c412t-3f2838c629848f7221a2716bfb825a02dbfc02bc742f0f5b9b2e847ccb721bf93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10950-014-9444-1$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10950-014-9444-1$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=28800830$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Zare, Mehdi</creatorcontrib><creatorcontrib>Amini, Hamideh</creatorcontrib><creatorcontrib>Yazdi, Pouye</creatorcontrib><creatorcontrib>Sesetyan, Karin</creatorcontrib><creatorcontrib>Demircioglu, Mine Betul</creatorcontrib><creatorcontrib>Kalafat, Dogan</creatorcontrib><creatorcontrib>Erdik, Mustafa</creatorcontrib><creatorcontrib>Giardini, Domenico</creatorcontrib><creatorcontrib>Khan, M. Asif</creatorcontrib><creatorcontrib>Tsereteli, Nino</creatorcontrib><title>Recent developments of the Middle East catalog</title><title>Journal of seismology</title><addtitle>J Seismol</addtitle><description>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 30° 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 30° E), and Saudi Arabia is about 9 km.</description><subject>Arabia</subject><subject>Earth and Environmental Science</subject><subject>Earth models</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Earthquakes</subject><subject>Earthquakes, seismology</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Exact sciences and technology</subject><subject>Geophysics</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Hydrogeology</subject><subject>Internal geophysics</subject><subject>Natural hazards: prediction, damages, etc</subject><subject>Original Article</subject><subject>Plate tectonics</subject><subject>Reproduction</subject><subject>Seismic activity</subject><subject>Seismic phenomena</subject><subject>Seismicity</subject><subject>Seismology</subject><subject>Structural Geology</subject><subject>Tectonics</subject><subject>Tectonics. Structural geology. 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Geothermics</topic><topic>Exact sciences and technology</topic><topic>Geophysics</topic><topic>Geophysics/Geodesy</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Hydrogeology</topic><topic>Internal geophysics</topic><topic>Natural hazards: prediction, damages, etc</topic><topic>Original Article</topic><topic>Plate tectonics</topic><topic>Reproduction</topic><topic>Seismic activity</topic><topic>Seismic phenomena</topic><topic>Seismicity</topic><topic>Seismology</topic><topic>Structural Geology</topic><topic>Tectonics</topic><topic>Tectonics. Structural geology. 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Asif</au><au>Tsereteli, Nino</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Recent developments of the Middle East catalog</atitle><jtitle>Journal of seismology</jtitle><stitle>J Seismol</stitle><date>2014-10-01</date><risdate>2014</risdate><volume>18</volume><issue>4</issue><spage>749</spage><epage>772</epage><pages>749-772</pages><issn>1383-4649</issn><eissn>1573-157X</eissn><abstract>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 30° 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 30° E), and Saudi Arabia is about 9 km.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s10950-014-9444-1</doi><tpages>24</tpages></addata></record> |
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| subjects | Arabia Earth and Environmental Science Earth models Earth Sciences Earth, ocean, space Earthquakes Earthquakes, seismology Engineering and environment geology. Geothermics Exact sciences and technology Geophysics Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Hydrogeology Internal geophysics Natural hazards: prediction, damages, etc Original Article Plate tectonics Reproduction Seismic activity Seismic phenomena Seismicity Seismology Structural Geology Tectonics Tectonics. Structural geology. Plate tectonics |
| title | Recent developments of the Middle East catalog |
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