The present-day deformation of the central Zagros from GPS measurements
In 1997 and in 2000, we measured the distances between 14 geodetic benchmarks across the central Zagros mountain belt. The results show that about 10 mm/yr of shortening in the central Zagros is distributed across the mountain belt. This shortening corresponds to roughly 50% of the total convergence...
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| Veröffentlicht in: | Geophysical research letters 2002-10, Vol.29 (19), p.33-1-33-4 |
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| container_title | Geophysical research letters |
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| creator | Tatar, Mohammad Hatzfeld, Denis Martinod, Joseph Walpersdorf, Andrea Ghafori-Ashtiany, Mohsen Chéry, Jean |
| description | In 1997 and in 2000, we measured the distances between 14 geodetic benchmarks across the central Zagros mountain belt. The results show that about 10 mm/yr of shortening in the central Zagros is distributed across the mountain belt. This shortening corresponds to roughly 50% of the total convergence between Arabia and Eurasia and is consistent in direction. The Persian Gulf does not deform significantly. The Main Zagros Reverse Fault is not an active kinematic boundary. The internal deformation of the folded belt is rather homogeneous, at the scale of our survey, which does not allow us to detect any individual active blind fault. However, the strain pattern suggests that N‐S dextral strike slip faults may accommodate part of the deformation. |
| doi_str_mv | 10.1029/2002GL015427 |
| format | Article |
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The results show that about 10 mm/yr of shortening in the central Zagros is distributed across the mountain belt. This shortening corresponds to roughly 50% of the total convergence between Arabia and Eurasia and is consistent in direction. The Persian Gulf does not deform significantly. The Main Zagros Reverse Fault is not an active kinematic boundary. The internal deformation of the folded belt is rather homogeneous, at the scale of our survey, which does not allow us to detect any individual active blind fault. 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However, the strain pattern suggests that N‐S dextral strike slip faults may accommodate part of the deformation.</description><subject>Arabia</subject><subject>Belts</subject><subject>Boundaries</subject><subject>Convergence</subject><subject>Deformation</subject><subject>Earth Sciences</subject><subject>Faults</subject><subject>Geophysics</subject><subject>Mountains</subject><subject>Physics</subject><subject>Sciences of the Universe</subject><subject>Strikes</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNp90ctO3DAUBmCrAomBsuMBsqpAatrjS3xZIkRDpXAHIXVjeZLjkpJMBjtTmLevR6kQK1a2_H-_ZfkQckDhGwVmvjMAVlZAC8HUJzKjRohcA6gtMgMwac-U3CG7Mf4BAA6czkh594jZMmDExZg3bp016IfQu7EdFtngszHFdcqC67Jf7ncYYubD0Gfl1W3Wo4urgH2K42ey7V0Xcf__ukfuf5zenZzl1WX58-S4yl0huM6NdBRqP3eeNgyVlIIL77XUkqk5NCAahQJqXShTAPWNEZoBciUZEzhHyvfI0XTvo-vsMrS9C2s7uNaeHVd2cwZAwRit_27sl8kuw_C8wjjavo01dp1b4LCKliklC2pkgocfQlpwCpQzwxP9OtE6fUUM6N8eQcFuhmDfDyFxNvGXtsP1h9aWNxWVwHQq5VOpjSO-vpVceLJScVXYh4vSngt-La7Nrb3h_wBDUZRD</recordid><startdate>200210</startdate><enddate>200210</enddate><creator>Tatar, Mohammad</creator><creator>Hatzfeld, Denis</creator><creator>Martinod, Joseph</creator><creator>Walpersdorf, Andrea</creator><creator>Ghafori-Ashtiany, Mohsen</creator><creator>Chéry, Jean</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope><scope>1XC</scope><scope>VOOES</scope></search><sort><creationdate>200210</creationdate><title>The present-day deformation of the central Zagros from GPS measurements</title><author>Tatar, Mohammad ; Hatzfeld, Denis ; Martinod, Joseph ; Walpersdorf, Andrea ; Ghafori-Ashtiany, Mohsen ; Chéry, Jean</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5438-96a10cfbaf1d2e766434ff868627b0d04d7e40c8579501fd94820e376224ebe13</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>Arabia</topic><topic>Belts</topic><topic>Boundaries</topic><topic>Convergence</topic><topic>Deformation</topic><topic>Earth Sciences</topic><topic>Faults</topic><topic>Geophysics</topic><topic>Mountains</topic><topic>Physics</topic><topic>Sciences of the Universe</topic><topic>Strikes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Tatar, Mohammad</creatorcontrib><creatorcontrib>Hatzfeld, Denis</creatorcontrib><creatorcontrib>Martinod, Joseph</creatorcontrib><creatorcontrib>Walpersdorf, Andrea</creatorcontrib><creatorcontrib>Ghafori-Ashtiany, Mohsen</creatorcontrib><creatorcontrib>Chéry, Jean</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Tatar, Mohammad</au><au>Hatzfeld, Denis</au><au>Martinod, Joseph</au><au>Walpersdorf, Andrea</au><au>Ghafori-Ashtiany, Mohsen</au><au>Chéry, Jean</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The present-day deformation of the central Zagros from GPS measurements</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2002-10</date><risdate>2002</risdate><volume>29</volume><issue>19</issue><spage>33-1</spage><epage>33-4</epage><pages>33-1-33-4</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>In 1997 and in 2000, we measured the distances between 14 geodetic benchmarks across the central Zagros mountain belt. The results show that about 10 mm/yr of shortening in the central Zagros is distributed across the mountain belt. This shortening corresponds to roughly 50% of the total convergence between Arabia and Eurasia and is consistent in direction. The Persian Gulf does not deform significantly. The Main Zagros Reverse Fault is not an active kinematic boundary. The internal deformation of the folded belt is rather homogeneous, at the scale of our survey, which does not allow us to detect any individual active blind fault. 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| source | Wiley Free Content; Wiley-Blackwell AGU Digital Library; EZB-FREE-00999 freely available EZB journals; Wiley Online Library All Journals |
| subjects | Arabia Belts Boundaries Convergence Deformation Earth Sciences Faults Geophysics Mountains Physics Sciences of the Universe Strikes |
| title | The present-day deformation of the central Zagros from GPS measurements |
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