Late-stage evolution of the Chemehuevi and Sacramento detachment faults from apatite (U-Th)/He thermochronometry--Evidence for mid-Miocene accelerated slip-Reference-Cited by-同舟云学术

Late-stage evolution of the Chemehuevi and Sacramento detachment faults from apatite (U-Th)/He thermochronometry--Evidence for mid-Miocene accelerated slip

Published:2006-05-01 Issue:5-6 Volume:118 Page:689-709
ISSN:0016-7606
Container-title:Geological Society of America Bulletin
language:en
Short-container-title:Geological Society of America Bulletin

Author:

Carter T. J.,Kohn B. P.,Foster D. A.,Gleadow A. J.W.,Woodhead J. D.

Publisher

Geological Society of America

Subject

Geology

Reference99 articles.

1. Significance of K-Ar Ages of Tertiary Rocks from the Lake Mead Region, Nevada-Arizona

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3. Low-angle normal fault earthquakes and triggering

4. Field tests of rolling hinges: Existence, mechanical types, and implications for extensional tectonics

5. Space-time patterns and tectonic controls of Tertiary extension and magmatism in the Great Basin of the western United States

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