Slip history and the role of the Agua Blanca fault in the tectonics of the North American–Pacific plate boundary of southern California, USA and Baja California, Mexico

Author:

Wetmore Paul H.1,Malservisi Rocco1,Fletcher John M.2,Alsleben Helge3,Wilson James1,Callihan Sean1,Springer Adam1,González-Yajimovich Oscar4,Gold Peter O.5

Affiliation:

1. Department of Geology, University of South Florida, Tampa, Florida 33620, USA

2. Departamento de Geología, Centro de Investigación Científica y de Educación Superior de Ensenada, Carretera Tijuana-Ensenada No. 3918, Zona Playitas, Ensenada, Baja California, Mexico C.P. 22860

3. School of Geology, Energy and the Environment, Texas Christian University, Fort Worth, Texas 76129, USA

4. Universidad Autónoma de Baja California, Ensenada, Baja California, Mexico C.P. 22860

5. Jackson School of Geosciences, University of Texas at Austin, Austin, Texas 78712, USA

Publisher

Geological Society of America

Subject

Stratigraphy,Geology

Reference92 articles.

1. Agua Blanca fault—A major transverse structure of northern Baja California, Mexico;Allen,1960

2. The type Alisitos Formation (Cretaceous, Aptian–Albian) of Baja California and its bivalve fauna;Allison,1974

3. Complex deformation during arc-continent collision: Quantifying finite strain in the accreted Alisitos arc, Peninsular Ranges batholith, Baja California;Alsleben;Journal of Structural Geology,2008

4. Detrital zircon ages in Paleozoic and Mesozoic basement assemblages of the Peninsular Ranges batholith, Baja California, Mexico: Constraints for depositional ages and provenance;Alsleben;International Geology Review,2011

5. Structural evidence of mid-Cretaceous suturing of the Alisitos arc to North America from the Sierra Calamajue, Baja California, Mexico;Alsleben,2014

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