Uplift and erosion of the San Bernardino Mountains associated with transpression along the San Andreas fault, California, as constrained by radiogenic helium thermochronometry-Reference-Cited by-同舟云学术

Uplift and erosion of the San Bernardino Mountains associated with transpression along the San Andreas fault, California, as constrained by radiogenic helium thermochronometry

Published:1998-06 Issue:3 Volume:17 Page:360-378
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Spotila James A.,Farley Kenneth A.,Sieh Kerry

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://www.agu.org/journals/tc/v017/i003/98TC00378/98TC00378.pdf

Reference67 articles.

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2. Morphology as a function of bedrock uplift and climate: A case study of the Transverse Ranges, southern California, from apatite fission track and DEM analysis (abstract);Blythe;EOS Trans., AGU,1996

3. Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California;Bohannon;Geology,1982

4. Bortugno , E. J. T. E. Spittler Geologic map of the San Bernardino Quadrangle, California Calif. Div. Mines Geol. 1986

5. Rapid, long-term rates of denudation;Burbank;Geology,1991

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