Loading…

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...

Full description

Saved in:
Bibliographic Details
Published in:Geotectonics 2023-04, Vol.57 (2), p.213-229
Main Authors: Mansouri, S. M., Keshavarz, S., Shahpasandzadeh, M., Faghih, A.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-a339t-e4110d0d6448c4e88a5fda2e29335f46a3f4ed04a51fba3cf32cfbb15f75076d3
cites cdi_FETCH-LOGICAL-a339t-e4110d0d6448c4e88a5fda2e29335f46a3f4ed04a51fba3cf32cfbb15f75076d3
container_end_page 229
container_issue 2
container_start_page 213
container_title Geotectonics
container_volume 57
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
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2828399644</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2828399644</sourcerecordid><originalsourceid>FETCH-LOGICAL-a339t-e4110d0d6448c4e88a5fda2e29335f46a3f4ed04a51fba3cf32cfbb15f75076d3</originalsourceid><addsrcrecordid>eNp1kc1Kw0AUhQdRsFYfwN2AG11E5yeTJu5KrFpsVWgFd-EmmWlTmpk4k4L6PD6o0x_oQlxduOc758C9CJ1Tck0pD28mhNAoFowyThgh4v0AdagQUUCTXnSIOms5WOvH6MS5BSGceLWDfp4qLWtoq8Jho3A7l3gKOjcri8eyhdrYZl4VODV1s5Sf-HIywEML-uoWD_2mKrzTaIeVsTiV2nwbD--NrsagS3wnvV5vUFzpTcmzsX6Aa6XVeAx25ve7_r6yJuhbyCvQ-HUJrTxFRwqWTp7tZhe93Q-m6WMwenkYpv1RAJwnbSBDSklJyigM4yKUcQxClcAkSzgXKoyAq1CWJARBVQ68UJwVKs-pUD1BelHJu-him9tY87GSrs0W_hDaV2YsZjFPEh_tKbqlCmucs1Jlja1qsF8ZJdn6GdmfZ3gP23qcZ_VM2n3y_6Zfj_WNsA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2828399644</pqid></control><display><type>article</type><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><source>Springer Nature</source><creator>Mansouri, S. M. ; Keshavarz, S. ; Shahpasandzadeh, M. ; Faghih, A.</creator><creatorcontrib>Mansouri, S. M. ; Keshavarz, S. ; Shahpasandzadeh, M. ; Faghih, A.</creatorcontrib><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><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 &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; 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>
fulltext fulltext
identifier ISSN: 0016-8521
ispartof Geotectonics, 2023-04, Vol.57 (2), p.213-229
issn 0016-8521
1556-1976
language eng
recordid cdi_proquest_journals_2828399644
source Springer Nature
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
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-19T00%3A45%3A28IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Kinematics%20of%20the%20Tanbour%20Metamorphic%20Complex%20(SE%20Iran):%20Implications%20for%20Cenozoic%20Metamorphism%20and%20Deformation%20in%20the%20Northeastern%20Margin%20of%20the%20Afro-Arabian%20Plate&rft.jtitle=Geotectonics&rft.au=Mansouri,%20S.%20M.&rft.date=2023-04-01&rft.volume=57&rft.issue=2&rft.spage=213&rft.epage=229&rft.pages=213-229&rft.issn=0016-8521&rft.eissn=1556-1976&rft_id=info:doi/10.1134/S001685212302005X&rft_dat=%3Cproquest_cross%3E2828399644%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a339t-e4110d0d6448c4e88a5fda2e29335f46a3f4ed04a51fba3cf32cfbb15f75076d3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2828399644&rft_id=info:pmid/&rfr_iscdi=true