Nonvolcanic Tremors Deep Beneath the San Andreas Fault
We have discovered nonvolcanic tremor activity (i.e., long-duration seismic signals with no clear P or S waves) within a transform plate boundary zone along the San Andreas Fault near Cholame, California, the inferred epicentral region of the 1857 Fort Tejon earthquake (moment magnitude approximatel...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 2005-01, Vol.307 (5708), p.389-389 |
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| creator | Nadeau, Robert M Dolenc, David |
| description | We have discovered nonvolcanic tremor activity (i.e., long-duration seismic signals with no clear P or S waves) within a transform plate boundary zone along the San Andreas Fault near Cholame, California, the inferred epicentral region of the 1857 Fort Tejon earthquake (moment magnitude approximately 7.8). The tremors occur between 20 to 40 kilometers' depth, below the seismogenic zone (the upper approximately 15 kilometers of Earth's crust where earthquakes occur), and their activity rates may correlate with variations in local earthquake activity. |
| doi_str_mv | 10.1126/science.1107142 |
| format | Article |
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The tremors occur between 20 to 40 kilometers' depth, below the seismogenic zone (the upper approximately 15 kilometers of Earth's crust where earthquakes occur), and their activity rates may correlate with variations in local earthquake activity.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.1107142</identifier><identifier>PMID: 15591163</identifier><identifier>CODEN: SCIEAS</identifier><language>eng</language><publisher>Washington, DC: American Association for the Advancement of Science</publisher><subject>Analysis ; Brevia ; Earth sciences ; Earth, ocean, space ; Earthquakes ; Earthquakes, seismology ; Energy ; Exact sciences and technology ; Geologic tremors ; Internal geophysics ; Observations ; Sampling ; Seismic prospecting ; Seismic surveying ; Seismology ; Subduction zones ; Tectonics. Structural geology. Plate tectonics ; United States ; Volcanoes</subject><ispartof>Science (American Association for the Advancement of Science), 2005-01, Vol.307 (5708), p.389-389</ispartof><rights>Copyright 2005 American Association for the Advancement of Science</rights><rights>2005 INIST-CNRS</rights><rights>COPYRIGHT 2005 American Association for the Advancement of Science</rights><rights>COPYRIGHT 2005 American Association for the Advancement of Science</rights><rights>Copyright American Association for the Advancement of Science Jan 21, 2005</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a829t-84364a882498af6ce66e7b1007067056b2c6d807eefeab95bf47322af27d23ff3</citedby><cites>FETCH-LOGICAL-a829t-84364a882498af6ce66e7b1007067056b2c6d807eefeab95bf47322af27d23ff3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/3840049$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/3840049$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,2884,2885,27924,27925,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=16472175$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/15591163$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Nadeau, Robert M</creatorcontrib><creatorcontrib>Dolenc, David</creatorcontrib><title>Nonvolcanic Tremors Deep Beneath the San Andreas Fault</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>We have discovered nonvolcanic tremor activity (i.e., long-duration seismic signals with no clear P or S waves) within a transform plate boundary zone along the San Andreas Fault near Cholame, California, the inferred epicentral region of the 1857 Fort Tejon earthquake (moment magnitude approximately 7.8). The tremors occur between 20 to 40 kilometers' depth, below the seismogenic zone (the upper approximately 15 kilometers of Earth's crust where earthquakes occur), and their activity rates may correlate with variations in local earthquake activity.</description><subject>Analysis</subject><subject>Brevia</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Earthquakes</subject><subject>Earthquakes, seismology</subject><subject>Energy</subject><subject>Exact sciences and technology</subject><subject>Geologic tremors</subject><subject>Internal geophysics</subject><subject>Observations</subject><subject>Sampling</subject><subject>Seismic prospecting</subject><subject>Seismic surveying</subject><subject>Seismology</subject><subject>Subduction zones</subject><subject>Tectonics. Structural geology. 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David</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Nonvolcanic Tremors Deep Beneath the San Andreas Fault</atitle><jtitle>Science (American Association for the Advancement of Science)</jtitle><addtitle>Science</addtitle><date>2005-01-21</date><risdate>2005</risdate><volume>307</volume><issue>5708</issue><spage>389</spage><epage>389</epage><pages>389-389</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><coden>SCIEAS</coden><abstract>We have discovered nonvolcanic tremor activity (i.e., long-duration seismic signals with no clear P or S waves) within a transform plate boundary zone along the San Andreas Fault near Cholame, California, the inferred epicentral region of the 1857 Fort Tejon earthquake (moment magnitude approximately 7.8). The tremors occur between 20 to 40 kilometers' depth, below the seismogenic zone (the upper approximately 15 kilometers of Earth's crust where earthquakes occur), and their activity rates may correlate with variations in local earthquake activity.</abstract><cop>Washington, DC</cop><pub>American Association for the Advancement of Science</pub><pmid>15591163</pmid><doi>10.1126/science.1107142</doi><tpages>1</tpages></addata></record> |
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| identifier | ISSN: 0036-8075 |
| ispartof | Science (American Association for the Advancement of Science), 2005-01, Vol.307 (5708), p.389-389 |
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| source | JSTOR Archive Collection A-Z Listing; American Association for the Advancement of Science |
| subjects | Analysis Brevia Earth sciences Earth, ocean, space Earthquakes Earthquakes, seismology Energy Exact sciences and technology Geologic tremors Internal geophysics Observations Sampling Seismic prospecting Seismic surveying Seismology Subduction zones Tectonics. Structural geology. Plate tectonics United States Volcanoes |
| title | Nonvolcanic Tremors Deep Beneath the San Andreas Fault |
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