Understanding kinematics of intra-arc transcurrent deformation: Paleomagnetic evidence from the Liquiñe-Ofqui fault zone (Chile, 38-41°S)
Author:
Affiliation:
1. Istituto Nazionale di Geofisica e Vulcanologia; Rome Italy
2. Dipartimento di Fisica; Università di Bologna; Bologna Italy
3. Now at Department of Geophysics; University of São Paulo; São Paulo Brazil
Funder
Istituto Nazionale di Geofisica e Vulcanologia INGV
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Reference125 articles.
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3. Discordant paleomagnetic pole positions as evidence of regional shear in the western Cordillera of North America;Beck;Am. J. Sci.,1976
4. Model for late Mesozoic-early Tertiary tectonics of coastal California and western Mexico, and speculations on the origin of the San Andreas Fault;Beck;Tectonics,1986
5. Analysis of late Jurassic-Recent paleomagnetic data from active plate margins of South America;Beck;J. South Am. Earth Sci.,1988
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