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The role of the Ebro Block on the deformation experienced within the Pyrenean realm: Insights from deformable plate tectonic models
Plate kinematic models of the Pyrenees have been extensively debated due to discrepancies between plate kinematic constraints for the Iberian plate and Atlantic/Tethyan related plate motions. Recently, the morphology of the Iberian plate and its partitioning into several continental blocks has been...
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Published in: | Journal of geodynamics 2023-03, Vol.155, p.101962, Article 101962 |
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description | Plate kinematic models of the Pyrenees have been extensively debated due to discrepancies between plate kinematic constraints for the Iberian plate and Atlantic/Tethyan related plate motions. Recently, the morphology of the Iberian plate and its partitioning into several continental blocks has been proposed as a solution towards reconciling discrepancies between previously published reconstructions that treat Iberia as a single, rigid, tectonic plate. Herein, the first deformable plate tectonic modeling study of the Pyrenean realm is presented using previously published and newly presented reconstructions of Iberia. Special emphasis is given to the kinematics of the Ebro Block, a continental block situated between the Pyrenees and Iberian Ranges, whose kinematics are considered to play a key role in the extensional deformation experienced within the Pyrenean realm. Temporal variations in strain rate and crustal thickness calculated by deformable plate models provide insights regarding the pre-orogenic template of the Pyrenees and the variability in regional stress directions along the Iberia-Eurasia plate boundary from the Triassic to Cenomanian. Models that propose transtensional rift phases within the Pyrenean realm induced by the Landes High and Ebro Block kinematics since the Triassic are successful in deriving crustal thicknesses indicative of a pre-orogenic hyperextended rifted margin within the Pyrenean realm. The results of this study demonstrate the importance of continental block kinematics during rift-related deformation and their impact on the evolution and partitioning of rift domains. Furthermore, this study also highlights potential avenues to consider for improving future plate kinematic models of Iberia, and regions elsewhere. |
doi_str_mv | 10.1016/j.jog.2023.101962 |
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Kim ; Tugend, Julie</creator><creatorcontrib>King, Michael T. ; Welford, J. Kim ; Tugend, Julie</creatorcontrib><description>Plate kinematic models of the Pyrenees have been extensively debated due to discrepancies between plate kinematic constraints for the Iberian plate and Atlantic/Tethyan related plate motions. Recently, the morphology of the Iberian plate and its partitioning into several continental blocks has been proposed as a solution towards reconciling discrepancies between previously published reconstructions that treat Iberia as a single, rigid, tectonic plate. Herein, the first deformable plate tectonic modeling study of the Pyrenean realm is presented using previously published and newly presented reconstructions of Iberia. Special emphasis is given to the kinematics of the Ebro Block, a continental block situated between the Pyrenees and Iberian Ranges, whose kinematics are considered to play a key role in the extensional deformation experienced within the Pyrenean realm. Temporal variations in strain rate and crustal thickness calculated by deformable plate models provide insights regarding the pre-orogenic template of the Pyrenees and the variability in regional stress directions along the Iberia-Eurasia plate boundary from the Triassic to Cenomanian. Models that propose transtensional rift phases within the Pyrenean realm induced by the Landes High and Ebro Block kinematics since the Triassic are successful in deriving crustal thicknesses indicative of a pre-orogenic hyperextended rifted margin within the Pyrenean realm. 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Furthermore, this study also highlights potential avenues to consider for improving future plate kinematic models of Iberia, and regions elsewhere.</description><identifier>ISSN: 0264-3707</identifier><identifier>DOI: 10.1016/j.jog.2023.101962</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Deformable plate models ; Earth Sciences ; Ebro Block ; GPlates ; Plate tectonics ; Pyrenees ; Rifting ; Sciences of the Universe ; Tectonics</subject><ispartof>Journal of geodynamics, 2023-03, Vol.155, p.101962, Article 101962</ispartof><rights>2023 The Authors</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c374t-207a0b52b0f1633c882be1c1d74f21d5e2e41ef287bfe15e519f1cea415ec4343</citedby><cites>FETCH-LOGICAL-c374t-207a0b52b0f1633c882be1c1d74f21d5e2e41ef287bfe15e519f1cea415ec4343</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,314,780,784,885,27924,27925</link.rule.ids><backlink>$$Uhttps://hal.science/hal-04607134$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>King, Michael T.</creatorcontrib><creatorcontrib>Welford, J. Kim</creatorcontrib><creatorcontrib>Tugend, Julie</creatorcontrib><title>The role of the Ebro Block on the deformation experienced within the Pyrenean realm: Insights from deformable plate tectonic models</title><title>Journal of geodynamics</title><description>Plate kinematic models of the Pyrenees have been extensively debated due to discrepancies between plate kinematic constraints for the Iberian plate and Atlantic/Tethyan related plate motions. Recently, the morphology of the Iberian plate and its partitioning into several continental blocks has been proposed as a solution towards reconciling discrepancies between previously published reconstructions that treat Iberia as a single, rigid, tectonic plate. Herein, the first deformable plate tectonic modeling study of the Pyrenean realm is presented using previously published and newly presented reconstructions of Iberia. Special emphasis is given to the kinematics of the Ebro Block, a continental block situated between the Pyrenees and Iberian Ranges, whose kinematics are considered to play a key role in the extensional deformation experienced within the Pyrenean realm. Temporal variations in strain rate and crustal thickness calculated by deformable plate models provide insights regarding the pre-orogenic template of the Pyrenees and the variability in regional stress directions along the Iberia-Eurasia plate boundary from the Triassic to Cenomanian. Models that propose transtensional rift phases within the Pyrenean realm induced by the Landes High and Ebro Block kinematics since the Triassic are successful in deriving crustal thicknesses indicative of a pre-orogenic hyperextended rifted margin within the Pyrenean realm. The results of this study demonstrate the importance of continental block kinematics during rift-related deformation and their impact on the evolution and partitioning of rift domains. Furthermore, this study also highlights potential avenues to consider for improving future plate kinematic models of Iberia, and regions elsewhere.</description><subject>Deformable plate models</subject><subject>Earth Sciences</subject><subject>Ebro Block</subject><subject>GPlates</subject><subject>Plate tectonics</subject><subject>Pyrenees</subject><subject>Rifting</subject><subject>Sciences of the Universe</subject><subject>Tectonics</subject><issn>0264-3707</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp9kD9PwzAQxT2ARCl8ADavDCm24_wpTKUCWqkSDGW2HOfcOCRxZUeFznxxHAKMTHf39N6d7ofQFSUzSmh6U89qu5sxwuJhnqfsBE0IS3kUZyQ7Q-fe14SQNJnnE_S5rQA72wC2GvehfyicxfeNVW_Ydt9KCdq6VvYmzPCxB2egU1Did9NXZrS8HB10IDvsQDbtLV533uyq3mPtbPu7oAhH9o3sAfegetsZhVtbQuMv0KmWjYfLnzpFr48P2-Uq2jw_rZeLTaTijPcRI5kkRcIKomkaxyrPWQFU0TLjmtEyAQacgmZ5VmigCSR0rqkCyUOveMzjKboe91ayEXtnWumOwkojVouNGDTCU5LRmB9o8NLRq5z13oH-C1AiBsqiFoGyGCiLkXLI3I2Z8BMcDDjh1cjKuPCxKK35J_0F2nCIWA</recordid><startdate>202303</startdate><enddate>202303</enddate><creator>King, Michael T.</creator><creator>Welford, J. Kim</creator><creator>Tugend, Julie</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>6I.</scope><scope>AAFTH</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>1XC</scope></search><sort><creationdate>202303</creationdate><title>The role of the Ebro Block on the deformation experienced within the Pyrenean realm: Insights from deformable plate tectonic models</title><author>King, Michael T. ; Welford, J. Kim ; Tugend, Julie</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c374t-207a0b52b0f1633c882be1c1d74f21d5e2e41ef287bfe15e519f1cea415ec4343</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Deformable plate models</topic><topic>Earth Sciences</topic><topic>Ebro Block</topic><topic>GPlates</topic><topic>Plate tectonics</topic><topic>Pyrenees</topic><topic>Rifting</topic><topic>Sciences of the Universe</topic><topic>Tectonics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>King, Michael T.</creatorcontrib><creatorcontrib>Welford, J. Kim</creatorcontrib><creatorcontrib>Tugend, Julie</creatorcontrib><collection>ScienceDirect Open Access Titles</collection><collection>Elsevier:ScienceDirect:Open Access</collection><collection>CrossRef</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Journal of geodynamics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>King, Michael T.</au><au>Welford, J. Kim</au><au>Tugend, Julie</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The role of the Ebro Block on the deformation experienced within the Pyrenean realm: Insights from deformable plate tectonic models</atitle><jtitle>Journal of geodynamics</jtitle><date>2023-03</date><risdate>2023</risdate><volume>155</volume><spage>101962</spage><pages>101962-</pages><artnum>101962</artnum><issn>0264-3707</issn><abstract>Plate kinematic models of the Pyrenees have been extensively debated due to discrepancies between plate kinematic constraints for the Iberian plate and Atlantic/Tethyan related plate motions. Recently, the morphology of the Iberian plate and its partitioning into several continental blocks has been proposed as a solution towards reconciling discrepancies between previously published reconstructions that treat Iberia as a single, rigid, tectonic plate. Herein, the first deformable plate tectonic modeling study of the Pyrenean realm is presented using previously published and newly presented reconstructions of Iberia. Special emphasis is given to the kinematics of the Ebro Block, a continental block situated between the Pyrenees and Iberian Ranges, whose kinematics are considered to play a key role in the extensional deformation experienced within the Pyrenean realm. Temporal variations in strain rate and crustal thickness calculated by deformable plate models provide insights regarding the pre-orogenic template of the Pyrenees and the variability in regional stress directions along the Iberia-Eurasia plate boundary from the Triassic to Cenomanian. Models that propose transtensional rift phases within the Pyrenean realm induced by the Landes High and Ebro Block kinematics since the Triassic are successful in deriving crustal thicknesses indicative of a pre-orogenic hyperextended rifted margin within the Pyrenean realm. The results of this study demonstrate the importance of continental block kinematics during rift-related deformation and their impact on the evolution and partitioning of rift domains. Furthermore, this study also highlights potential avenues to consider for improving future plate kinematic models of Iberia, and regions elsewhere.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.jog.2023.101962</doi><oa>free_for_read</oa></addata></record> |
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subjects | Deformable plate models Earth Sciences Ebro Block GPlates Plate tectonics Pyrenees Rifting Sciences of the Universe Tectonics |
title | The role of the Ebro Block on the deformation experienced within the Pyrenean realm: Insights from deformable plate tectonic models |
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