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Radon and hydrologic anomalies on the Rough Creek Fault: Possible precursors to the M5.1 Eastern Kentucky Earthquake, 1980
Author(s) -
Steele S. R.
Publication year - 1981
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 - 10.1029/gl008i005p00465
Subject(s) - radon , geology , seismology , induced seismicity , epicenter , anomaly (physics) , fault (geology) , earthquake prediction , physics , condensed matter physics , quantum mechanics
Soil radon emanation increased sharply on the Rough Creek fault near the Illinois‐Kentucky border in April, 1980, 3 1/2 months before a M5.1 earthquake in eastern Kentucky, July 27, 1980. The spikelike anomaly was similar to a radon anomaly in the New Madrid seismic zone in 1979 that preceded by 2 months a M3.9 tremor at the site of that anomaly. Weekly radon monitoring was initiated on the Rough Creek fault after abrupt cessation of spring flow on the fault occurred at a site that had experienced similar flow cessation 1 month prior to a M5.3 earthquake in southeastern Illinois in 1968. Although the recent Kentucky epicenter was 380 km east of the site of the detected radon anomaly, factors relating to regional structures, recent seismicity, additional radon data, and the stress regime suggest that the hydrologic and radon anomalies may have been precursors to an eastward progression of strain that culminated in the eastern Kentucky tremor.

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