Rapid Pliocene-Pleistocene erosion of the central Colorado Plateau documented by apatite thermochronology from the Henry Mountains

Persistent Link:
http://hdl.handle.net/10150/620828
Title:
Rapid Pliocene-Pleistocene erosion of the central Colorado Plateau documented by apatite thermochronology from the Henry Mountains
Author:
Murray, K. E.; Reiners, P. W.; Thomson, S. N.
Affiliation:
Univ Arizona, Dept Geosci
Issue Date:
2016-06
Publisher:
GEOLOGICAL SOC AMER, INC
Citation:
GEOLOGY, June 2016; v. 44; no. 6; p. 483–486
Journal:
Geology
Rights:
© 2016 Geological Society of America.
Collection Information:
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.
Abstract:
Apatite thermochronology is, in principle, uniquely suited to document the Cenozoic erosion of the Colorado Plateau (southwestern United States) and settle generations of debate regarding the region's history of uplift, erosion, and fluvial incision. The protracted near-surface history of the Colorado Plateau bedrock, however, complicates the temperature sensitivity of apatite thermochronometers. This has confounded efforts to see clear evidence of late Cenozoic erosion, especially in the central Colorado Plateau, where this problem is compounded by the diverse detrital apatite grains in the region's sedimentary bedrock. We overcome this problem in the thermal aureole of the Oligocene Henry Mountains intrusive complex, where these sandstones have apatite (U-Th-Sm)/He ages younger than 26 Ma with positive-slope age-effective U trends (3-25 Ma, 5-180 ppm eU) that resolve a distinctive late Cenozoic history. Thermal modeling results strongly suggest that the central Colorado Plateau was a stable Miocene landscape that was rapidly exhumed similar to 1.5-2 km during the past 5 m.y., likely in the past 3-2 m.y., at time-averaged rates of similar to 250-700 m/m.y. This demonstrates that substantial late Cenozoic erosion of the north-central plateau interior postdates the ca. 5.6 Ma integration of the Colorado River that lowered regional base level.
Note:
Published online 12 May 2016. 12 month embargo
ISSN:
0091-7613
DOI:
10.1130/G37733.1
Version:
Final accepted manuscript
Sponsors:
National Science Foundation (NSF); ARCS (Achievement Rewards for College Scientists); P.E.O. (Philanthropic Educational Organization); NSF grant [EAR-1219653, EAR-1338583]
Additional Links:
http://geology.gsapubs.org/content/early/2016/05/12/G37733.1.abstract

Full metadata record

DC FieldValue Language
dc.contributor.authorMurray, K. E.en
dc.contributor.authorReiners, P. W.en
dc.contributor.authorThomson, S. N.en
dc.date.accessioned2016-10-06T20:51:19Z-
dc.date.available2016-10-06T20:51:19Z-
dc.date.issued2016-06-
dc.identifier.citationGEOLOGY, June 2016; v. 44; no. 6; p. 483–486en
dc.identifier.issn0091-7613-
dc.identifier.doi10.1130/G37733.1-
dc.identifier.urihttp://hdl.handle.net/10150/620828-
dc.description.abstractApatite thermochronology is, in principle, uniquely suited to document the Cenozoic erosion of the Colorado Plateau (southwestern United States) and settle generations of debate regarding the region's history of uplift, erosion, and fluvial incision. The protracted near-surface history of the Colorado Plateau bedrock, however, complicates the temperature sensitivity of apatite thermochronometers. This has confounded efforts to see clear evidence of late Cenozoic erosion, especially in the central Colorado Plateau, where this problem is compounded by the diverse detrital apatite grains in the region's sedimentary bedrock. We overcome this problem in the thermal aureole of the Oligocene Henry Mountains intrusive complex, where these sandstones have apatite (U-Th-Sm)/He ages younger than 26 Ma with positive-slope age-effective U trends (3-25 Ma, 5-180 ppm eU) that resolve a distinctive late Cenozoic history. Thermal modeling results strongly suggest that the central Colorado Plateau was a stable Miocene landscape that was rapidly exhumed similar to 1.5-2 km during the past 5 m.y., likely in the past 3-2 m.y., at time-averaged rates of similar to 250-700 m/m.y. This demonstrates that substantial late Cenozoic erosion of the north-central plateau interior postdates the ca. 5.6 Ma integration of the Colorado River that lowered regional base level.en
dc.description.sponsorshipNational Science Foundation (NSF); ARCS (Achievement Rewards for College Scientists); P.E.O. (Philanthropic Educational Organization); NSF grant [EAR-1219653, EAR-1338583]en
dc.language.isoenen
dc.publisherGEOLOGICAL SOC AMER, INCen
dc.relation.urlhttp://geology.gsapubs.org/content/early/2016/05/12/G37733.1.abstracten
dc.rights© 2016 Geological Society of America.en
dc.titleRapid Pliocene-Pleistocene erosion of the central Colorado Plateau documented by apatite thermochronology from the Henry Mountainsen
dc.typeArticleen
dc.contributor.departmentUniv Arizona, Dept Geoscien
dc.identifier.journalGeologyen
dc.description.notePublished online 12 May 2016. 12 month embargoen
dc.description.collectioninformationThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.en
dc.eprint.versionFinal accepted manuscripten
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