@article{ref1,
title="Seismicity remotely triggered by the magnitude 7.3 landers, california, earthquake",
journal="Science",
year="1993",
author="Hill, D. P. and Reasenberg, P. A. and Michael, A. and Arabaz, W. J. and Beroza, G. and Brumbaugh, D. and Brune, J. N. and Castro, R. and Davis, S. and Depolo, D. and Ellsworth, W. L. and Gomberg, Joan and Harmsen, S. and House, L. and Jackson, Susan M. and Johnston, M. J. and Jones, Loring and Keller, R. and Malone, S. and Munguia, L. and Nava, S. and Pechmann, J. C. and Sanford, A. and Simpson, R. W. and Smith, R. B. and Stark, M. and Stickney, M. and Vidal, A. and Walter, S. and Wong, V. and Zollweg, J.",
volume="260",
number="5114",
pages="1617-1623",
abstract="The magnitude 7.3 Landers earthquake of 28 June 1992 triggered a remarkably sudden and widespread increase in earthquake activity across much of the western United States. The triggered earthquakes, which occurred at distances up to 1250 kilometers (17 source dimensions) from the Landers mainshock, were confined to areas of persistent seismicity and strike-slip to normal faulting. Many of the triggered areas also are sites of geothermal and recent volcanic activity. Static stress changes calculated for elastic models of the earthquake appear to be too small to have caused the triggering. The most promising explanations involve nonlinear interactions between large dynamic strains accompanying seismic waves from the mainshock and crustal fluids (perhaps including crustal magma).<p /><p>Language: en</p>",
language="en",
issn="0036-8075",
doi="10.1126/science.260.5114.1617",
url="http://dx.doi.org/10.1126/science.260.5114.1617"
}