Fault trends on the seaward slope of the Aleutian Trench: Implications for a laterally changing stress field tied to a westward increase in oblique convergence-Reference-Cited by-同舟云学术

Fault trends on the seaward slope of the Aleutian Trench: Implications for a laterally changing stress field tied to a westward increase in oblique convergence

Published:2003-10 Issue:B10 Volume:108 Page:
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Mortera-Gutiérrez Carlos A.¹,Scholl David W.²,Carlson Richard L.³

Affiliation:

1. Instituto de Geofísica; Universidad Nacional Autónoma de México; Coyoacán México

2. U.S. Geological Survey; Menlo Park California USA

3. Department of Geology and Geophysics; Texas A&M University; College Station Texas USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference64 articles.

1. Aki , K. P. G. Richards Quantitative Seismology 1 W. H. Freeman New York 1980

2. Displacement partitioning and arc-parallel extension in the Aleutian volcanic island arc;Avé Lallemant;Tectonophysics,1996

3. Active displacement partitioning and arc-parallel extension of the volcanic arc based on Global Positioning System geodesy and kinematic analysis;Avé Lallemant;Geology,2000

4. The mechanics of oblique slip faulting;Bott;Geol. Mag.,1959

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