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Research ArticleArticles

Topographic evolution of the Sierra Nevada measured directly by inversion of low-temperature thermochronology

Devin McPhillips and Mark T. Brandon
American Journal of Science February 2012, 312 (2) 90-116; DOI: https://doi.org/10.2475/02.2012.02
Devin McPhillips
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Mark T. Brandon
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American Journal of Science: 312 (2)
American Journal of Science
Vol. 312, Issue 2
1 Feb 2012
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Topographic evolution of the Sierra Nevada measured directly by inversion of low-temperature thermochronology
Devin McPhillips, Mark T. Brandon
American Journal of Science Feb 2012, 312 (2) 90-116; DOI: 10.2475/02.2012.02

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Topographic evolution of the Sierra Nevada measured directly by inversion of low-temperature thermochronology
Devin McPhillips, Mark T. Brandon
American Journal of Science Feb 2012, 312 (2) 90-116; DOI: 10.2475/02.2012.02
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  • Article
    • Abstract
    • INTRODUCTION
    • BACKGROUND
    • CONSTRAINTS ON SURFACE UPLIFT FROM THERMOCHRONOLOGY
    • MODELING AND INVERSION
    • RESULTS
    • DISCUSSION
    • CONCLUSIONS
    • ACKNOWLEDGMENTS
    • APPENDIX
    • REFERENCES
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  • Pliocene-Quaternary subsidence and exhumation of the southeastern San Joaquin Basin, California, in response to mantle lithosphere removal
  • Mitochondrial DNA haplotype distribution patterns in Pinus ponderosa (Pinaceae): Range-wide evolutionary history and implications for conservation
  • Epeirogenic transients related to mantle lithosphere removal in the southern Sierra Nevada region, California: Part II. Implications of rock uplift and basin subsidence relations
  • Exhumation of the southern Sierra Nevada-eastern Tehachapi Mountains constrained by low-temperature thermochronology: Implications for the initiation of the Garlock fault
  • Paleochannels, stream incision, erosion, topographic evolution, and alternative explanations of paleoaltimetry, Sierra Nevada, California
  • The Cenozoic climatic and topographic evolution of the western North American Cordillera
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