The Akato Tagh bend along the Altyn Tagh fault, northwest Tibet 1: Smoothing by vertical-axis rotation and the effect of topographic stresses on bend-flanking faults-Reference-Cited by-同舟云学术

The Akato Tagh bend along the Altyn Tagh fault, northwest Tibet 1: Smoothing by vertical-axis rotation and the effect of topographic stresses on bend-flanking faults

Published:2004-11-01 Issue:11-12 Volume:116 Page:1423-1442
ISSN:0016-7606
Container-title:Geological Society of America Bulletin
language:en
Short-container-title:Geological Society of America Bulletin

Author:

Cowgill E.,Yin A.,Arrowsmith J. R.,Feng W. X.,Shuanhong Z.

Publisher

Geological Society of America

Subject

Geology

Reference92 articles.

1. Evolution of the Northern Santa Cruz Mountains by Advection of Crust Past a San Andreas Fault Bend

2. Evolution of the Santa Cruz Mountains, California, through tectonic growth and geomorphic decay

3. Erosion as a driving mechanism of intracontinental mountain growth

4. `Forebergs', flower structures, and the development of large intra-continental strike-slip faults: the Gurvan Bogd fault system in Mongolia

5. Transform-normal extension and asymmetric basins: An alternative to pull-apart models

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