The Dynamic History of 220 Million Years of Subduction Below Mexico: A Correlation Between Slab Geometry and Overriding Plate Deformation Based on Geology, Paleomagnetism, and Seismic Tomography
Author:
Affiliation:
1. Department of Earth Sciences; Utrecht University; Utrecht Netherlands
2. Department of Geological Sciences; San Diego State University; San Diego CA USA
3. Center for Earth Evolution and Dynamics; University of Oslo; Oslo Norway
Funder
Nederlandse Organisatie voor Wetenschappelijk Onderzoek
Norwegian Research Council - Centres of excellence funding scheme
Centres of Excellence funding scheme
NWO Vidi
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018GC007739/fullpdf
Reference173 articles.
1. Detrital zircon ages in Palaeozoic and Mesozoic basement assemblages of the Peninsular Ranges batholith, Baja California, Mexico: Constraints for depositional ages and provenance;Alsleben;International Geology Review,2012
2. Amaru , M. 2007 Global travel time tomography with 3-D reference models
3. Franciscan subduction off to a slow start: Evidence from high-precision Lu-Hf garnet ages on high grade-blocks;Anczkiewicz;Earth and Planetary Science Letters,2004
4. Atwater , T. M. 1998 Late tectonic history of Southern California with emphasis on the Western Transverse ranges and Northern Channel Islands plate tectonic history of Southern California with emphasis on the western Transverse Ranges and Northern Channel Islands
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