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Far‐field pressurization likely caused one of the largest injection induced earthquakes by reactivating a large preexisting basement fault structure
Author(s) -
Yeck W. L.,
Weingarten M.,
Benz H. M.,
McNamara D. E.,
Bergman E. A.,
Herrmann R. B.,
Rubinstein J. L.,
Earle P. S.
Publication year - 2016
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2016gl070861
Subject(s) - geology , seismology , precambrian , induced seismicity , sequence (biology) , cabin pressurization , fault (geology) , basement , seismic moment , intraplate earthquake , tectonics , paleontology , geography , archaeology , aerospace engineering , engineering , genetics , biology
The M w 5.1 Fairview, Oklahoma, earthquake on 13 February 2016 and its associated seismicity produced the largest moment release in the central and eastern United States since the 2011 M w 5.7 Prague, Oklahoma, earthquake sequence and is one of the largest earthquakes potentially linked to wastewater injection. This energetic sequence has produced five earthquakes with M w 4.4 or larger. Almost all of these earthquakes occur in Precambrian basement on a partially unmapped 14 km long fault. Regional injection into the Arbuckle Group increased approximately sevenfold in the 36 months prior to the start of the sequence (January 2015). We suggest far‐field pressurization from clustered, high‐rate wells greater than 12 km from this sequence induced these earthquakes. As compared to the Fairview sequence, seismicity is diffuse near high‐rate wells, where pressure changes are expected to be largest. This points to the critical role that preexisting faults play in the occurrence of large induced earthquakes.