Time‐Invariant Late Quaternary Slip Rates Along the Agua Blanca Fault, Northern Baja California, Mexico-Reference-Cited by-同舟云学术

Time‐Invariant Late Quaternary Slip Rates Along the Agua Blanca Fault, Northern Baja California, Mexico

Author:

Gold P. O.¹²³^ORCID,Behr W. M.¹²^ORCID,Fletcher J. M.⁴^ORCID,Rockwell T. K.⁵^ORCID,Figueiredo P. M.⁶⁷^ORCID

Affiliation:

1. Department of Geological Sciences, Jackson School of Geosciences University of Texas at Austin Austin TX USA

2. Geological Institute, Department of Earth Sciences ETH Zurich Zurich Switzerland

3. Now at ExxonMobil Corporation Spring TX USA

4. Departmento de Geología Centro de Investigación Científica y de Educación Superior de Ensenada Ensenada Mexico

5. Department of Geological Sciences San Diego State University San Diego CA USA

6. Department of Geology University of Cincinnati Cincinnati OH USA

7. Now at the Department of Marine, Earth, and Atmospheric Sciences North Carolina State University Raleigh NC USA

Funder

National Science Foundation

U.S. Geological Survey

Southern California Earthquake Center

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

Reference117 articles.

1. Dose‐rate conversion factors: Update;Adamiec G.;Ancient TL,1998

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