Earthquake hypocenters and focal mechanisms in central Oklahoma reveal a complex system of reactivated subsurface strike-slip faulting

Author:

McNamara D. E.1,Benz H. M.1,Herrmann R. B.2,Bergman E. A.3,Earle P.1,Holland A.4,Baldwin R.1,Gassner A.1

Affiliation:

1. U.S. Geological Survey; Denver Colorado USA

2. Department of Earth and Atmospheric Sciences; Saint Louis University; St. Louis Missouri USA

3. Global Seismological Services; Golden Colorado USA

4. Oklahoma Geological Survey; Norman Oklahoma USA

Funder

United States Geological Survey's National Earthquake Hazards Reduction Program

IRIS PASSCAL

NEIC

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference32 articles.

1. Alt , R. M. Zoback 2014 Development of a detailed stress map of Oklahoma for avoidance of potentially active faults when siting wastewater injection wells

2. Tulsa Geol. Soc., Digest;Bennison,1964

3. The 24 January 2013 ML 4.4 Earthquake near Paradox, Colorado, and its relation to deep well injection;Block;Seismol. Res. Lett.,2014

4. Seismicity and tectonics of western Venezuela;Dewey;Bull. Seismol. Soc. Am.,1972

5. Dolton , G. L. T. M. Finn 1989 Petroleum geology of the Nemaha uplift

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