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Kinematics of the Tanbour Metamorphic Complex (SE Iran): Implications for Cenozoic Metamorphism and Deformation in the Northeastern Margin of the Afro-Arabian Plate
New petrofabric studies joined with kinematic vorticity and finite strain analyses allowed to recognize the deformation characteristics of the mid-crustal rocks exposed in the the Tanbour Metamorphic Complex (Iran). Different scale sense of shear criteria in the Tanbour Metamorphic Complex reveal an...
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Published in: | Geotectonics 2023-04, Vol.57 (2), p.213-229 |
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creator | Mansouri, S. M. Keshavarz, S. Shahpasandzadeh, M. Faghih, A. |
description | New petrofabric studies joined with kinematic vorticity and finite strain analyses allowed to recognize the deformation characteristics of the mid-crustal rocks exposed in the the Tanbour Metamorphic Complex (Iran). Different scale sense of shear criteria in the Tanbour Metamorphic Complex reveal an unequivocal top-to-the-SE sense of shear within this part of the Sanandaj–Sirjan metamorphic belt. Well-developed quartz
c
-axis within selected mylonitic samples was utilized to estimate bulk kinematic vorticity. W
k
values ranging from 0.65 to 0.86, thus indicating non-coaxial shear deformation with contemporaneous pure and simple shear components. Integration of microstructure- and petrofabric-based geothermometers indicates temperature of mylonitization ranges between ~450‒650°C corresponding from upper greenschist to amphibolites facies metamorphism. Data obtained support interpretations suggesting occurrence of transpressive deformation during ongoing continental collision of the Afro‒Arabian and Iranian plates. |
doi_str_mv | 10.1134/S001685212302005X |
format | article |
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c
-axis within selected mylonitic samples was utilized to estimate bulk kinematic vorticity. W
k
values ranging from 0.65 to 0.86, thus indicating non-coaxial shear deformation with contemporaneous pure and simple shear components. Integration of microstructure- and petrofabric-based geothermometers indicates temperature of mylonitization ranges between ~450‒650°C corresponding from upper greenschist to amphibolites facies metamorphism. Data obtained support interpretations suggesting occurrence of transpressive deformation during ongoing continental collision of the Afro‒Arabian and Iranian plates.</description><identifier>ISSN: 0016-8521</identifier><identifier>EISSN: 1556-1976</identifier><identifier>DOI: 10.1134/S001685212302005X</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Amphibolites ; Cenozoic ; Deformation ; Earth and Environmental Science ; Earth Sciences ; Kinematics ; Metamorphism ; Microstructure ; Plates ; Shear ; Shear deformation ; Strain analysis ; Structural Geology ; Vorticity</subject><ispartof>Geotectonics, 2023-04, Vol.57 (2), p.213-229</ispartof><rights>Pleiades Publishing, Inc. 2023. ISSN 0016-8521, Geotectonics, 2023, Vol. 57, No. 2, pp. 213–229. © Pleiades Publishing, Inc., 2023. ISSN 0016-8521, Geotectonics, 2023. © Pleiades Publishing, Inc., 2023.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-e4110d0d6448c4e88a5fda2e29335f46a3f4ed04a51fba3cf32cfbb15f75076d3</citedby><cites>FETCH-LOGICAL-a339t-e4110d0d6448c4e88a5fda2e29335f46a3f4ed04a51fba3cf32cfbb15f75076d3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,27905,27906</link.rule.ids></links><search><creatorcontrib>Mansouri, S. M.</creatorcontrib><creatorcontrib>Keshavarz, S.</creatorcontrib><creatorcontrib>Shahpasandzadeh, M.</creatorcontrib><creatorcontrib>Faghih, A.</creatorcontrib><title>Kinematics of the Tanbour Metamorphic Complex (SE Iran): Implications for Cenozoic Metamorphism and Deformation in the Northeastern Margin of the Afro-Arabian Plate</title><title>Geotectonics</title><addtitle>Geotecton</addtitle><description>New petrofabric studies joined with kinematic vorticity and finite strain analyses allowed to recognize the deformation characteristics of the mid-crustal rocks exposed in the the Tanbour Metamorphic Complex (Iran). Different scale sense of shear criteria in the Tanbour Metamorphic Complex reveal an unequivocal top-to-the-SE sense of shear within this part of the Sanandaj–Sirjan metamorphic belt. Well-developed quartz
c
-axis within selected mylonitic samples was utilized to estimate bulk kinematic vorticity. W
k
values ranging from 0.65 to 0.86, thus indicating non-coaxial shear deformation with contemporaneous pure and simple shear components. Integration of microstructure- and petrofabric-based geothermometers indicates temperature of mylonitization ranges between ~450‒650°C corresponding from upper greenschist to amphibolites facies metamorphism. Data obtained support interpretations suggesting occurrence of transpressive deformation during ongoing continental collision of the Afro‒Arabian and Iranian plates.</description><subject>Amphibolites</subject><subject>Cenozoic</subject><subject>Deformation</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Kinematics</subject><subject>Metamorphism</subject><subject>Microstructure</subject><subject>Plates</subject><subject>Shear</subject><subject>Shear deformation</subject><subject>Strain analysis</subject><subject>Structural Geology</subject><subject>Vorticity</subject><issn>0016-8521</issn><issn>1556-1976</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp1kc1Kw0AUhQdRsFYfwN2AG11E5yeTJu5KrFpsVWgFd-EmmWlTmpk4k4L6PD6o0x_oQlxduOc758C9CJ1Tck0pD28mhNAoFowyThgh4v0AdagQUUCTXnSIOms5WOvH6MS5BSGceLWDfp4qLWtoq8Jho3A7l3gKOjcri8eyhdrYZl4VODV1s5Sf-HIywEML-uoWD_2mKrzTaIeVsTiV2nwbD--NrsagS3wnvV5vUFzpTcmzsX6Aa6XVeAx25ve7_r6yJuhbyCvQ-HUJrTxFRwqWTp7tZhe93Q-m6WMwenkYpv1RAJwnbSBDSklJyigM4yKUcQxClcAkSzgXKoyAq1CWJARBVQ68UJwVKs-pUD1BelHJu-him9tY87GSrs0W_hDaV2YsZjFPEh_tKbqlCmucs1Jlja1qsF8ZJdn6GdmfZ3gP23qcZ_VM2n3y_6Zfj_WNsA</recordid><startdate>20230401</startdate><enddate>20230401</enddate><creator>Mansouri, S. M.</creator><creator>Keshavarz, S.</creator><creator>Shahpasandzadeh, M.</creator><creator>Faghih, A.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20230401</creationdate><title>Kinematics of the Tanbour Metamorphic Complex (SE Iran): Implications for Cenozoic Metamorphism and Deformation in the Northeastern Margin of the Afro-Arabian Plate</title><author>Mansouri, S. M. ; Keshavarz, S. ; Shahpasandzadeh, M. ; Faghih, A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-e4110d0d6448c4e88a5fda2e29335f46a3f4ed04a51fba3cf32cfbb15f75076d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Amphibolites</topic><topic>Cenozoic</topic><topic>Deformation</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Kinematics</topic><topic>Metamorphism</topic><topic>Microstructure</topic><topic>Plates</topic><topic>Shear</topic><topic>Shear deformation</topic><topic>Strain analysis</topic><topic>Structural Geology</topic><topic>Vorticity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Mansouri, S. M.</creatorcontrib><creatorcontrib>Keshavarz, S.</creatorcontrib><creatorcontrib>Shahpasandzadeh, M.</creatorcontrib><creatorcontrib>Faghih, A.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geotectonics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Mansouri, S. M.</au><au>Keshavarz, S.</au><au>Shahpasandzadeh, M.</au><au>Faghih, A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Kinematics of the Tanbour Metamorphic Complex (SE Iran): Implications for Cenozoic Metamorphism and Deformation in the Northeastern Margin of the Afro-Arabian Plate</atitle><jtitle>Geotectonics</jtitle><stitle>Geotecton</stitle><date>2023-04-01</date><risdate>2023</risdate><volume>57</volume><issue>2</issue><spage>213</spage><epage>229</epage><pages>213-229</pages><issn>0016-8521</issn><eissn>1556-1976</eissn><abstract>New petrofabric studies joined with kinematic vorticity and finite strain analyses allowed to recognize the deformation characteristics of the mid-crustal rocks exposed in the the Tanbour Metamorphic Complex (Iran). Different scale sense of shear criteria in the Tanbour Metamorphic Complex reveal an unequivocal top-to-the-SE sense of shear within this part of the Sanandaj–Sirjan metamorphic belt. Well-developed quartz
c
-axis within selected mylonitic samples was utilized to estimate bulk kinematic vorticity. W
k
values ranging from 0.65 to 0.86, thus indicating non-coaxial shear deformation with contemporaneous pure and simple shear components. Integration of microstructure- and petrofabric-based geothermometers indicates temperature of mylonitization ranges between ~450‒650°C corresponding from upper greenschist to amphibolites facies metamorphism. Data obtained support interpretations suggesting occurrence of transpressive deformation during ongoing continental collision of the Afro‒Arabian and Iranian plates.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S001685212302005X</doi><tpages>17</tpages></addata></record> |
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subjects | Amphibolites Cenozoic Deformation Earth and Environmental Science Earth Sciences Kinematics Metamorphism Microstructure Plates Shear Shear deformation Strain analysis Structural Geology Vorticity |
title | Kinematics of the Tanbour Metamorphic Complex (SE Iran): Implications for Cenozoic Metamorphism and Deformation in the Northeastern Margin of the Afro-Arabian Plate |
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