Matches in SemOpenAlex for { <https://semopenalex.org/work/W2023531719> ?p ?o ?g. }
- W2023531719 endingPage "128" @default.
- W2023531719 startingPage "114" @default.
- W2023531719 abstract "The Pontides are characterized by a series of Mesozoic-Cenozoic fold belts comprising a N-vergent foreland fold and thrust belt in the Western Pontides and a concave, upward-shaped fold belt in the Eastern Pontides. The curvature of the fold belt follows the Caucasus which may imply a phase of oroclinal bending. In order to test whether the fold curvature represents a phase of oroclinal bending, a paleomagnetic study has been carried out in the Eastern Pontides on late Cretaceous and middle Eocene volcanic and sedimentary rocks from 29 sites. Rock magnetic studies reveal medium-temperature components with an unblocking temperature of 400–580 °C, indicating pseudo-single domain titanomagnetite as the most abundant carrier of magnetic remanence in the middle Eocene rocks studied here. In the upper Cretaceous rocks, a high-temperature component with an unblocking range of 580–650 °C was isolated. Stepwise thermal and alternating field demagnetization isolated two components of remanent magnetization in middle Eocene rocks comprising a low unblocking temperature/coercivity component near the present field direction and a characteristic remanent magnetization (ChRM) component of Ds = 332.3°, Is = 49.9° (k = 33.3, α95 = 9.2°, N = 15 sites). A positive fold test at a 95% confidence level and a reversal test indicate a primary magnetization. Component analysis of the upper Cretaceous rocks identifies a stable ChRM Ds = 160.3°, Is = −45.0°, (k = 85.6, α95 = 6.0°, N = 8 sites) following removal of secondary remanence. Their ChRM direction passes fold and reversal tests at a 95% confidence level. Both the upper Cretaceous and middle Eocene paleomagnetic data from the Eastern Pontides and the Lesser Caucasus clearly demonstrate evidence of oroclinal bending that occurred contemporaneouslywith the convergence between Arabia and Eurasia in the Paleocene." @default.
- W2023531719 created "2016-06-24" @default.
- W2023531719 creator A5065149384 @default.
- W2023531719 date "2011-08-01" @default.
- W2023531719 modified "2023-10-16" @default.
- W2023531719 title "New paleomagnetic constraints on the late Cretaceous and early Cenozoic tectonic history of the Eastern Pontides" @default.
- W2023531719 cites W1589162793 @default.
- W2023531719 cites W1968631381 @default.
- W2023531719 cites W1968906770 @default.
- W2023531719 cites W1972667733 @default.
- W2023531719 cites W1979068537 @default.
- W2023531719 cites W1982409099 @default.
- W2023531719 cites W1982798419 @default.
- W2023531719 cites W1985252659 @default.
- W2023531719 cites W1990713790 @default.
- W2023531719 cites W1994865926 @default.
- W2023531719 cites W1996585172 @default.
- W2023531719 cites W2005017717 @default.
- W2023531719 cites W2020518963 @default.
- W2023531719 cites W2028764239 @default.
- W2023531719 cites W2036580797 @default.
- W2023531719 cites W2037973110 @default.
- W2023531719 cites W2042981041 @default.
- W2023531719 cites W2045594539 @default.
- W2023531719 cites W2046947330 @default.
- W2023531719 cites W2052128667 @default.
- W2023531719 cites W2056386002 @default.
- W2023531719 cites W2063421616 @default.
- W2023531719 cites W2067616922 @default.
- W2023531719 cites W2069412307 @default.
- W2023531719 cites W2073871193 @default.
- W2023531719 cites W2085875161 @default.
- W2023531719 cites W2091693693 @default.
- W2023531719 cites W2093035173 @default.
- W2023531719 cites W2095293118 @default.
- W2023531719 cites W2109173312 @default.
- W2023531719 cites W2110868236 @default.
- W2023531719 cites W2118204502 @default.
- W2023531719 cites W2118515467 @default.
- W2023531719 cites W2121612795 @default.
- W2023531719 cites W2131678752 @default.
- W2023531719 cites W2148200847 @default.
- W2023531719 cites W2149277645 @default.
- W2023531719 cites W2163712338 @default.
- W2023531719 cites W2169115796 @default.
- W2023531719 cites W4234701869 @default.
- W2023531719 doi "https://doi.org/10.1016/j.jog.2010.12.004" @default.
- W2023531719 hasPublicationYear "2011" @default.
- W2023531719 type Work @default.
- W2023531719 sameAs 2023531719 @default.
- W2023531719 citedByCount "37" @default.
- W2023531719 countsByYear W20235317192012 @default.
- W2023531719 countsByYear W20235317192013 @default.
- W2023531719 countsByYear W20235317192014 @default.
- W2023531719 countsByYear W20235317192015 @default.
- W2023531719 countsByYear W20235317192016 @default.
- W2023531719 countsByYear W20235317192017 @default.
- W2023531719 countsByYear W20235317192018 @default.
- W2023531719 countsByYear W20235317192019 @default.
- W2023531719 countsByYear W20235317192020 @default.
- W2023531719 countsByYear W20235317192021 @default.
- W2023531719 countsByYear W20235317192022 @default.
- W2023531719 crossrefType "journal-article" @default.
- W2023531719 hasAuthorship W2023531719A5065149384 @default.
- W2023531719 hasConcept C109007969 @default.
- W2023531719 hasConcept C115260700 @default.
- W2023531719 hasConcept C121332964 @default.
- W2023531719 hasConcept C12294951 @default.
- W2023531719 hasConcept C127313418 @default.
- W2023531719 hasConcept C127413603 @default.
- W2023531719 hasConcept C151730666 @default.
- W2023531719 hasConcept C155058782 @default.
- W2023531719 hasConcept C189479680 @default.
- W2023531719 hasConcept C204330871 @default.
- W2023531719 hasConcept C32546565 @default.
- W2023531719 hasConcept C49015763 @default.
- W2023531719 hasConcept C53942344 @default.
- W2023531719 hasConcept C62520636 @default.
- W2023531719 hasConcept C6494504 @default.
- W2023531719 hasConcept C73707237 @default.
- W2023531719 hasConcept C78519656 @default.
- W2023531719 hasConceptScore W2023531719C109007969 @default.
- W2023531719 hasConceptScore W2023531719C115260700 @default.
- W2023531719 hasConceptScore W2023531719C121332964 @default.
- W2023531719 hasConceptScore W2023531719C12294951 @default.
- W2023531719 hasConceptScore W2023531719C127313418 @default.
- W2023531719 hasConceptScore W2023531719C127413603 @default.
- W2023531719 hasConceptScore W2023531719C151730666 @default.
- W2023531719 hasConceptScore W2023531719C155058782 @default.
- W2023531719 hasConceptScore W2023531719C189479680 @default.
- W2023531719 hasConceptScore W2023531719C204330871 @default.
- W2023531719 hasConceptScore W2023531719C32546565 @default.
- W2023531719 hasConceptScore W2023531719C49015763 @default.
- W2023531719 hasConceptScore W2023531719C53942344 @default.
- W2023531719 hasConceptScore W2023531719C62520636 @default.
- W2023531719 hasConceptScore W2023531719C6494504 @default.
- W2023531719 hasConceptScore W2023531719C73707237 @default.
- W2023531719 hasConceptScore W2023531719C78519656 @default.