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Seismic Evidence for an Earthquake Nucleation Phase
Near-source observations show that earthquakes initiate with a distinctive seismic nucleation phase that is characterized by a low rate of moment release relative to the rest of the event. This phase was observed for the 30 earthquakes having moment magnitudes 2.6 to 8.1, and the size and duration o...
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Published in: | Science (American Association for the Advancement of Science) 1995-05, Vol.268 (5212), p.851-855 |
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description | Near-source observations show that earthquakes initiate with a distinctive seismic nucleation phase that is characterized by a low rate of moment release relative to the rest of the event. This phase was observed for the 30 earthquakes having moment magnitudes 2.6 to 8.1, and the size and duration of this phase scale with the eventual size of the earthquake. During the nucleation phase, moment release was irregular and appears to have been confined to a limited region of the fault. It was characteristically followed by quadratic growth in the moment rate as rupture began to propagate away from the nucleation zone. These observations suggest that the nucleation process exerts a strong influence on the size of the eventual earthquake. |
doi_str_mv | 10.1126/science.268.5212.851 |
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L. ; Beroza, G. C.</creator><creatorcontrib>Ellsworth, W. L. ; Beroza, G. C.</creatorcontrib><description>Near-source observations show that earthquakes initiate with a distinctive seismic nucleation phase that is characterized by a low rate of moment release relative to the rest of the event. This phase was observed for the 30 earthquakes having moment magnitudes 2.6 to 8.1, and the size and duration of this phase scale with the eventual size of the earthquake. During the nucleation phase, moment release was irregular and appears to have been confined to a limited region of the fault. It was characteristically followed by quadratic growth in the moment rate as rupture began to propagate away from the nucleation zone. 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L.</creatorcontrib><creatorcontrib>Beroza, G. C.</creatorcontrib><title>Seismic Evidence for an Earthquake Nucleation Phase</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>Near-source observations show that earthquakes initiate with a distinctive seismic nucleation phase that is characterized by a low rate of moment release relative to the rest of the event. This phase was observed for the 30 earthquakes having moment magnitudes 2.6 to 8.1, and the size and duration of this phase scale with the eventual size of the earthquake. During the nucleation phase, moment release was irregular and appears to have been confined to a limited region of the fault. It was characteristically followed by quadratic growth in the moment rate as rupture began to propagate away from the nucleation zone. These observations suggest that the nucleation process exerts a strong influence on the size of the eventual earthquake.</description><subject>Boundary layer separation</subject><subject>Cubes</subject><subject>Earth</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Earthquakes</subject><subject>Earthquakes, seismology</subject><subject>Exact sciences and technology</subject><subject>Exhibits</subject><subject>Internal geophysics</subject><subject>Kinetics</subject><subject>Motion</subject><subject>Musical intervals</subject><subject>Nucleation</subject><subject>Observation</subject><subject>Observations</subject><subject>P waves</subject><subject>Personality</subject><subject>Seismographs</subject><subject>Seismology</subject><subject>Wave velocity</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1995</creationdate><recordtype>article</recordtype><sourceid>ALSLI</sourceid><sourceid>CJNVE</sourceid><sourceid>M0P</sourceid><recordid>eNqN0t9v0zAQB_AIgVgZ_AcTihACHpbiH7FjP46qlEnVijTg1bo65y4lTTY7mcZ_j6tGQ0UVVH6w5Pv4pNN9k-SMkjGlTH4MtsLG4phJNRaMsrES9EkyokSLTDPCnyYjQrjMFCnESfIihDUhsab58-SEFoVmtNCjhF9jFTaVTaf3Vbntl7rWp9CkU_DdzV0PPzG96m2N0FVtk369gYAvk2cO6oCvhvs0-f55-m3yJZsvZpeTi3kGSqguQ2mFVa7kulSukDbPRcG0xiVBcCIHEGBLrtyy4A4kccyqpRDU0Vi0SEp-mrzf9b317V2PoTObKlisa2iw7YMpcp4XUkv6f8k5IyKnIsp3_5RMaCWY5BG--Quu2943cV7DKBdxlpxFdL5DK6jRVI1rOw92hQ16qNsGXRWfL6jUPLbUkWcHeDwlxhUc8h_2fCQdPnQr6EMwl9dXR9PFj6Ppp9mxVM3me_T8ELVtXeMKTQzGZLHH8x23vg3BozO3vtqA_2UoMdt8myHfJubbbPNtYr7jt9fDVvrlBss_n4ZAR_B2ABAs1M5DY6vw6LhgImfbPmc7tg5d6x_LTKlCy5z_BrqdB4g</recordid><startdate>19950512</startdate><enddate>19950512</enddate><creator>Ellsworth, W. 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L.</au><au>Beroza, G. C.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Seismic Evidence for an Earthquake Nucleation Phase</atitle><jtitle>Science (American Association for the Advancement of Science)</jtitle><addtitle>Science</addtitle><date>1995-05-12</date><risdate>1995</risdate><volume>268</volume><issue>5212</issue><spage>851</spage><epage>855</epage><pages>851-855</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><coden>SCIEAS</coden><abstract>Near-source observations show that earthquakes initiate with a distinctive seismic nucleation phase that is characterized by a low rate of moment release relative to the rest of the event. This phase was observed for the 30 earthquakes having moment magnitudes 2.6 to 8.1, and the size and duration of this phase scale with the eventual size of the earthquake. During the nucleation phase, moment release was irregular and appears to have been confined to a limited region of the fault. It was characteristically followed by quadratic growth in the moment rate as rupture began to propagate away from the nucleation zone. These observations suggest that the nucleation process exerts a strong influence on the size of the eventual earthquake.</abstract><cop>Washington, DC</cop><pub>American Society for the Advancement of Science</pub><pmid>17792179</pmid><doi>10.1126/science.268.5212.851</doi><tpages>5</tpages></addata></record> |
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subjects | Boundary layer separation Cubes Earth Earth sciences Earth, ocean, space Earthquakes Earthquakes, seismology Exact sciences and technology Exhibits Internal geophysics Kinetics Motion Musical intervals Nucleation Observation Observations P waves Personality Seismographs Seismology Wave velocity |
title | Seismic Evidence for an Earthquake Nucleation Phase |
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