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Insights from low‐temperature thermochronometry into transpressional deformation and crustal exhumation along the San Andreas fault in the western Transverse Ranges, California
dc.contributor.authorNiemi, Nathan A.en_US
dc.contributor.authorBuscher, Jamie T.en_US
dc.contributor.authorSpotila, James A.en_US
dc.contributor.authorHouse, Martha A.en_US
dc.contributor.authorKelley, Shari A.en_US
dc.date.accessioned2014-02-11T17:57:19Z
dc.date.available2015-02-03T16:14:39Zen_US
dc.date.issued2013-12en_US
dc.identifier.citationNiemi, Nathan A.; Buscher, Jamie T.; Spotila, James A.; House, Martha A.; Kelley, Shari A. (2013). "Insights from low‐temperature thermochronometry into transpressional deformation and crustal exhumation along the San Andreas fault in the western Transverse Ranges, California." Tectonics 32(6): 1602-1622.en_US
dc.identifier.issn0278-7407en_US
dc.identifier.issn1944-9194en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/102707
dc.description.abstractThe San Emigdio Mountains are an example of an archetypical, transpressional structural system, bounded to the south by the San Andreas strike‐slip fault, and to the north by the active Wheeler Ridge thrust. Apatite (U‐Th)/He and apatite and zircon fission track ages were obtained along transects across the range and from wells in and to the north of the range. Apatite (U‐Th)/He ages are 4–6 Ma adjacent to the San Andreas fault, and both (U‐Th)/He and fission track ages grow older with distance to the north from the San Andreas. The young ages north of the San Andreas fault contrast with early Miocene (U‐Th)/He ages from Mount Pinos on the south side of the fault. Restoration of sample paleodepths in the San Emigdio Mountains using a regional unconformity at the base of the Eocene Tejon Formation indicates that the San Emigdio Mountains represent a crustal fragment that has been exhumed more than 5 km along the San Andreas fault since late Miocene time. Marked differences in the timing and rate of exhumation between the northern and southern sides of the San Andreas fault are difficult to reconcile with existing structural models of the western Transverse Ranges as a thin‐skinned thrust system. Instead, these results suggest that rheologic heterogeneities may play a role in localizing deformation along the Big Bend of the San Andreas fault as the San Emigdio Mountains are compressed between the crystalline basement of Mount Pinos and oceanic crust that underlies the southern San Joaquin Valley. Key Points There is Pliocene exhumation of the western Transverse Ranges Localization of deformation may be controlled by lithospheric strength Strain is partitioned between the San Andreas and regional thrustsen_US
dc.publisherPacific Section SEPM (Society for Sedimentary Geology)en_US
dc.publisherWiley Periodicals, Inc.en_US
dc.subject.otherExhumationen_US
dc.subject.otherSan Andreas Faulten_US
dc.subject.otherTranspressionen_US
dc.subject.otherLow‐Temperature Thermochronometryen_US
dc.subject.otherSan Emigdio Mountainsen_US
dc.subject.otherMount Pinosen_US
dc.titleInsights from low‐temperature thermochronometry into transpressional deformation and crustal exhumation along the San Andreas fault in the western Transverse Ranges, Californiaen_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelGeological Sciencesen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/102707/1/tect20096.pdf
dc.identifier.doi10.1002/2013TC003377en_US
dc.identifier.sourceTectonicsen_US
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