Fault kinematics of the Magallanes-Fagnano fault system, southern Chile; an example of diffuse strain and sinistral transtension along a continental transform margin

Author:

Betka Paul,Klepeis Keith,Mosher Sharon

Funder

University of Texas at Austin

MSD K.K.

Jackson School of Geosciences,University of Texas at Austin

National Science Foundation

American Association of Petroleum Geologists

Publisher

Elsevier BV

Subject

Geology

Reference114 articles.

1. Graphical determination of principal stress directions for slickenside lineation populations; an attempt to modify Arthaud's method;Aleksandrowski;J. Struct. Geol.,1985

2. Structural Geology Algorithms—Vectors and Tensors;Allmendinger,2013

3. Geometry and evolution of the frontal part of the Magallanes foreland thrust and fold belt (Vicuña Area), Tierra del Fuego, southern Chile;Alvarez Marron;Am. Assoc. Pet Geol. Bull.,1993

4. Detrital-zircon geochronology of the eastern magallanes foreland basin: implications for eocene kinematics of the northern scotia arc and drake passage;Barbeau;Earth Planet. Sci. Lett.,2009

5. Strike-slip fault geometry in Turkey and its influence on earthquake activity;Barka;Tectonics,1988

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