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dc.contributor.authorSteeples, Don W.
dc.contributor.authorPitt, A. M.
dc.date.accessioned2015-03-17T21:21:33Z
dc.date.available2015-03-17T21:21:33Z
dc.date.issued1976-02-10
dc.identifier.citationSteeples, D. W., and A. M. Pitt (1976), Microearthquakes in and near Long Valley, California, J. Geophys. Res., 81(5), 841–847, http://dx.doi.org/10.1029/JB081i005p00841.en_US
dc.identifier.urihttp://hdl.handle.net/1808/17106
dc.descriptionThis is the published version. Copyright 1976 American Geophysical Union. All Rights Reserved.en_US
dc.description.abstractSixteen portable seismograph stations were deployed in the vicinity of the Long Valley geothermal area, California, from April 27 to June 2, 1973. Only minor microearthquake activity was detected in the Long Valley caldera, but a high level of activity was detected to the south and east of the caldera. The abrupt spatial seismicity decrease at the southern boundary of the caldera suggests that the caldera is either structurally less competent than the surrounding crust or is at a junction of different regional tectonic deformation trends. No significant attenuation or delays occurred for either local P or S waves that traversed the caldera.en_US
dc.publisherAmerican Geophysical Unionen_US
dc.titleMicroearthquakes in and near Long Valley, Californiaen_US
dc.typeArticle
kusw.kuauthorSteeples, Don W.
kusw.kudepartmentGeologyen_US
dc.identifier.doi10.1029/JB081i005p00841
kusw.oaversionScholarly/refereed, publisher version
kusw.oapolicyThis item does not meet KU Open Access policy criteria.
dc.rights.accessrightsopenAccess


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