Paleomagnetic constraints on the kinematic relationship between the Guerrero terrane (Mexico) and North America since Early Cretaceous time

Author:

Boschman Lydian M.1,Molina Garza Roberto S.2,Langereis Cor G.1,van Hinsbergen Douwe J.J.1

Affiliation:

1. Department of Earth Sciences, Utrecht University, Heidelberglaan 2, 3584 CS Utrecht, Netherlands

2. Centro de Geociencias, Universidad Nacional Autónoma de México, Boulevard Juriquilla 3001, Juriquilla, Querétaro 76230, Mexico

Publisher

Geological Society of America

Subject

Geology

Reference80 articles.

1. Counterclockwise rotations in the late Eocene–Oligocene volcanic fields of San Luis Potosí and Sierra de Guanajuato (eastern Mesa Central, Mexico);Andreani;Tectonophysics,2014

2. Geomagnetic secular variation in the Cretaceous normal superchron and in the Jurassic;Biggin;Physics of the Earth and Planetary Interiors,2008

3. The volcano-sedimentary setting of the Kuroko type VHMS district of Cuale, Jalisco, Mexico;Bissig;Geological Society of America Abstracts with Programs,2003

4. Paleomagnetic data and the accretion of the Guerrero terrane, southern México continental margin;Böhnel,1989

5. Stratigraphic assessment of the Arcelia-Teloloapan area, southern Mexico: Implications for southern Mexico’s post-Neocomian tectonic evolution;Cabral-Cano;Journal of South American Earth Sciences,2000

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