Rotational kinematics of a curved fold: The Balzes anticline (Southern Pyrenees)
This study deals with how vertical-axis rotations are accommodated in thrust fronts. Studies on the rotational kinematics of fold and thrust belts are limited owing to the scarcity of the record of syntectonic rocks and other data required for 4D reconstruction approaches. We studied the Balzes anti...
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creator | Rodríguez-Pintó, A. Pueyo, E.L. Calvín, P. Sánchez, E. Ramajo, J. Casas, A.M. Ramón, M.J. Pocoví, A. Barnolas, A. Román, T. |
description | This study deals with how vertical-axis rotations are accommodated in thrust fronts. Studies on the rotational kinematics of fold and thrust belts are limited owing to the scarcity of the record of syntectonic rocks and other data required for 4D reconstruction approaches. We studied the Balzes anticline, a 17-km long, thrust-related, arc-shaped anticline with dense paleomagnetic sampling (75 sites) to unravel the origin of its curvature (about 50° of arc in map view). The availability of both synfolding and synrotational indicators enables us to decipher the complete kinematic history of the fold. Reliable paleomagnetic data (more than 500 specimens and about 1000 measurements) were obtained from Ypresian to Priabonian rocks, typically with six demagnetization steps. The ChRM is unblocked between 420 and 575°C in most samples (85%), and at 675°C in the others. The primary direction displays two polarities and passes the fold test. Vertical axis rotation values for the structure range from non-significant up to >80° clockwise. A strike vs. rotation diagram clearly relates this variability to the fold curvature (VAR=−46°+0.5∗TREND [R=0.97]) and reveals the addition of primary and secondary curvatures. The original (primary) curvature is related to the emplacement of the thrust sheet underlying the Balzes anticline; it shows an obliquity of approximately 15° with respect to the expected Pyrenean trend. Progressive unconformity in the field (Santa Marina site) provides a record of a Middle–Late Lutetian major folding event. The detailed analysis of the synrotational sedimentary record together with accurate temporal calibration based on previous magnetostratigraphic data allows us to date the rotation stage as Lutetian–Bartonian and to estimate the rotation velocity of the Balzes anticline to have been about 5.2°/Ma, both in agreement with previously published observations for the South Pyrenean front.
•Kinematics model with chronologic frame of 75 VAR sites (>1000 demagnetizations)•Syn-folding and syn-rotational materials enables to decipher the kinematic history•The exceptional chronologic frame leads a folding age of Middle–Upper Lutetian•This 17km oblique fold reveals primary and secondary curvature•Balzes anticline rotation velocity: 5.2°/M.a. and rotation stage: Lutetian–Bartonian |
doi_str_mv | 10.1016/j.tecto.2016.02.049 |
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•Kinematics model with chronologic frame of 75 VAR sites (>1000 demagnetizations)•Syn-folding and syn-rotational materials enables to decipher the kinematic history•The exceptional chronologic frame leads a folding age of Middle–Upper Lutetian•This 17km oblique fold reveals primary and secondary curvature•Balzes anticline rotation velocity: 5.2°/M.a. and rotation stage: Lutetian–Bartonian</description><identifier>ISSN: 0040-1951</identifier><identifier>EISSN: 1879-3266</identifier><identifier>DOI: 10.1016/j.tecto.2016.02.049</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Anticlines ; Balzes anticline ; Curvature ; External Sierras ; Fold and thrust belts ; Kinematics ; Mathematical analysis ; Paleomagnetism ; Rocks ; Rotation kinematics ; Rotational ; Thrust ; Trends</subject><ispartof>Tectonophysics, 2016-05, Vol.677-678, p.171-189</ispartof><rights>2016 Elsevier B.V.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a503t-e9e1e8337e2fb046ff89f41ebf37e989b9beeaf598e52860a9f032d8d60f573c3</citedby><cites>FETCH-LOGICAL-a503t-e9e1e8337e2fb046ff89f41ebf37e989b9beeaf598e52860a9f032d8d60f573c3</cites><orcidid>0000-0002-4485-2139</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.tecto.2016.02.049$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>315,782,786,3552,27931,27932,46002</link.rule.ids></links><search><creatorcontrib>Rodríguez-Pintó, A.</creatorcontrib><creatorcontrib>Pueyo, E.L.</creatorcontrib><creatorcontrib>Calvín, P.</creatorcontrib><creatorcontrib>Sánchez, E.</creatorcontrib><creatorcontrib>Ramajo, J.</creatorcontrib><creatorcontrib>Casas, A.M.</creatorcontrib><creatorcontrib>Ramón, M.J.</creatorcontrib><creatorcontrib>Pocoví, A.</creatorcontrib><creatorcontrib>Barnolas, A.</creatorcontrib><creatorcontrib>Román, T.</creatorcontrib><title>Rotational kinematics of a curved fold: The Balzes anticline (Southern Pyrenees)</title><title>Tectonophysics</title><description>This study deals with how vertical-axis rotations are accommodated in thrust fronts. Studies on the rotational kinematics of fold and thrust belts are limited owing to the scarcity of the record of syntectonic rocks and other data required for 4D reconstruction approaches. We studied the Balzes anticline, a 17-km long, thrust-related, arc-shaped anticline with dense paleomagnetic sampling (75 sites) to unravel the origin of its curvature (about 50° of arc in map view). The availability of both synfolding and synrotational indicators enables us to decipher the complete kinematic history of the fold. Reliable paleomagnetic data (more than 500 specimens and about 1000 measurements) were obtained from Ypresian to Priabonian rocks, typically with six demagnetization steps. The ChRM is unblocked between 420 and 575°C in most samples (85%), and at 675°C in the others. The primary direction displays two polarities and passes the fold test. Vertical axis rotation values for the structure range from non-significant up to >80° clockwise. A strike vs. rotation diagram clearly relates this variability to the fold curvature (VAR=−46°+0.5∗TREND [R=0.97]) and reveals the addition of primary and secondary curvatures. The original (primary) curvature is related to the emplacement of the thrust sheet underlying the Balzes anticline; it shows an obliquity of approximately 15° with respect to the expected Pyrenean trend. Progressive unconformity in the field (Santa Marina site) provides a record of a Middle–Late Lutetian major folding event. The detailed analysis of the synrotational sedimentary record together with accurate temporal calibration based on previous magnetostratigraphic data allows us to date the rotation stage as Lutetian–Bartonian and to estimate the rotation velocity of the Balzes anticline to have been about 5.2°/Ma, both in agreement with previously published observations for the South Pyrenean front.
•Kinematics model with chronologic frame of 75 VAR sites (>1000 demagnetizations)•Syn-folding and syn-rotational materials enables to decipher the kinematic history•The exceptional chronologic frame leads a folding age of Middle–Upper Lutetian•This 17km oblique fold reveals primary and secondary curvature•Balzes anticline rotation velocity: 5.2°/M.a. and rotation stage: Lutetian–Bartonian</description><subject>Anticlines</subject><subject>Balzes anticline</subject><subject>Curvature</subject><subject>External Sierras</subject><subject>Fold and thrust belts</subject><subject>Kinematics</subject><subject>Mathematical analysis</subject><subject>Paleomagnetism</subject><subject>Rocks</subject><subject>Rotation kinematics</subject><subject>Rotational</subject><subject>Thrust</subject><subject>Trends</subject><issn>0040-1951</issn><issn>1879-3266</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNqNkE1LAzEQhoMoWKu_wEuO9bDrJNnNJoIHLX6BoPhxDunuBLduNzXZCvXXm1rP4ml4h-cdmIeQYwY5AyZP5_mA9eBznkIOPIdC75ARU5XOBJdyl4wACsiYLtk-OYhxDgCSlXJEHp_8YIfW97aj722PixTqSL2jltar8IkNdb5rzujLG9JL231hpLZPTJdgOnn2q-ENQ08f1wF7xHhySPac7SIe_c4xeb2-epneZvcPN3fTi_vMliCGDDUyVEJUyN0MCumc0q5gOHNppZWe6RmidaVWWHIlwWoHgjeqkeDKStRiTCbbu8vgP1YYB7NoY41dZ3v0q2iY4mVRac3hHygoKQpRbVCxRevgYwzozDK0CxvWhoHZqDZz86PabFQb4CapTq3zbQvTw58tBhPrFvsamzYk2DS-_bP_DZ7giDY</recordid><startdate>20160523</startdate><enddate>20160523</enddate><creator>Rodríguez-Pintó, A.</creator><creator>Pueyo, E.L.</creator><creator>Calvín, P.</creator><creator>Sánchez, E.</creator><creator>Ramajo, J.</creator><creator>Casas, A.M.</creator><creator>Ramón, M.J.</creator><creator>Pocoví, A.</creator><creator>Barnolas, A.</creator><creator>Román, T.</creator><general>Elsevier 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><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0002-4485-2139</orcidid></search><sort><creationdate>20160523</creationdate><title>Rotational kinematics of a curved fold: The Balzes anticline (Southern Pyrenees)</title><author>Rodríguez-Pintó, A. ; Pueyo, E.L. ; Calvín, P. ; Sánchez, E. ; Ramajo, J. ; Casas, A.M. ; Ramón, M.J. ; Pocoví, A. ; Barnolas, A. ; Román, T.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a503t-e9e1e8337e2fb046ff89f41ebf37e989b9beeaf598e52860a9f032d8d60f573c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Anticlines</topic><topic>Balzes anticline</topic><topic>Curvature</topic><topic>External Sierras</topic><topic>Fold and thrust belts</topic><topic>Kinematics</topic><topic>Mathematical analysis</topic><topic>Paleomagnetism</topic><topic>Rocks</topic><topic>Rotation kinematics</topic><topic>Rotational</topic><topic>Thrust</topic><topic>Trends</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Rodríguez-Pintó, A.</creatorcontrib><creatorcontrib>Pueyo, E.L.</creatorcontrib><creatorcontrib>Calvín, P.</creatorcontrib><creatorcontrib>Sánchez, E.</creatorcontrib><creatorcontrib>Ramajo, J.</creatorcontrib><creatorcontrib>Casas, A.M.</creatorcontrib><creatorcontrib>Ramón, M.J.</creatorcontrib><creatorcontrib>Pocoví, A.</creatorcontrib><creatorcontrib>Barnolas, A.</creatorcontrib><creatorcontrib>Román, T.</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><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Tectonophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rodríguez-Pintó, A.</au><au>Pueyo, E.L.</au><au>Calvín, P.</au><au>Sánchez, E.</au><au>Ramajo, J.</au><au>Casas, A.M.</au><au>Ramón, M.J.</au><au>Pocoví, A.</au><au>Barnolas, A.</au><au>Román, T.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Rotational kinematics of a curved fold: The Balzes anticline (Southern Pyrenees)</atitle><jtitle>Tectonophysics</jtitle><date>2016-05-23</date><risdate>2016</risdate><volume>677-678</volume><spage>171</spage><epage>189</epage><pages>171-189</pages><issn>0040-1951</issn><eissn>1879-3266</eissn><abstract>This study deals with how vertical-axis rotations are accommodated in thrust fronts. Studies on the rotational kinematics of fold and thrust belts are limited owing to the scarcity of the record of syntectonic rocks and other data required for 4D reconstruction approaches. We studied the Balzes anticline, a 17-km long, thrust-related, arc-shaped anticline with dense paleomagnetic sampling (75 sites) to unravel the origin of its curvature (about 50° of arc in map view). The availability of both synfolding and synrotational indicators enables us to decipher the complete kinematic history of the fold. Reliable paleomagnetic data (more than 500 specimens and about 1000 measurements) were obtained from Ypresian to Priabonian rocks, typically with six demagnetization steps. The ChRM is unblocked between 420 and 575°C in most samples (85%), and at 675°C in the others. The primary direction displays two polarities and passes the fold test. Vertical axis rotation values for the structure range from non-significant up to >80° clockwise. A strike vs. rotation diagram clearly relates this variability to the fold curvature (VAR=−46°+0.5∗TREND [R=0.97]) and reveals the addition of primary and secondary curvatures. The original (primary) curvature is related to the emplacement of the thrust sheet underlying the Balzes anticline; it shows an obliquity of approximately 15° with respect to the expected Pyrenean trend. Progressive unconformity in the field (Santa Marina site) provides a record of a Middle–Late Lutetian major folding event. The detailed analysis of the synrotational sedimentary record together with accurate temporal calibration based on previous magnetostratigraphic data allows us to date the rotation stage as Lutetian–Bartonian and to estimate the rotation velocity of the Balzes anticline to have been about 5.2°/Ma, both in agreement with previously published observations for the South Pyrenean front.
•Kinematics model with chronologic frame of 75 VAR sites (>1000 demagnetizations)•Syn-folding and syn-rotational materials enables to decipher the kinematic history•The exceptional chronologic frame leads a folding age of Middle–Upper Lutetian•This 17km oblique fold reveals primary and secondary curvature•Balzes anticline rotation velocity: 5.2°/M.a. and rotation stage: Lutetian–Bartonian</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.tecto.2016.02.049</doi><tpages>19</tpages><orcidid>https://orcid.org/0000-0002-4485-2139</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Anticlines Balzes anticline Curvature External Sierras Fold and thrust belts Kinematics Mathematical analysis Paleomagnetism Rocks Rotation kinematics Rotational Thrust Trends |
title | Rotational kinematics of a curved fold: The Balzes anticline (Southern Pyrenees) |
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