Contrasts between source parameters of M < 5.5 earthquakes in northern Baja California and southern California
Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baj...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Doser, Diane I. [verfasserIn] |
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| Format: |
E-Artikel |
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| Erschienen: |
Oxford, UK: Blackwell Publishing Ltd ; 1994 |
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| Schlagwörter: |
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| Umfang: |
Online-Ressource |
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| Reproduktion: |
2007 ; Blackwell Publishing Journal Backfiles 1879-2005 |
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| Übergeordnetes Werk: |
In: Geophysical journal international - Oxford . Wiley-Blackwell, 1922, 116(1994), 3, Seite 0 |
| Übergeordnetes Werk: |
volume:116 ; year:1994 ; number:3 ; pages:0 |
| Links: |
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| DOI / URN: |
10.1111/j.1365-246X.1994.tb03284.x |
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NLEJ239649753 |
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| 245 | 1 | 0 | |a Contrasts between source parameters of M < 5.5 earthquakes in northern Baja California and southern California |
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| 520 | |a Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baja fault systems of southern California and northern Mexico. Observed regional differences in rupture complexity, fault rupture lengths and aftershock/foreshock activity appear to be related to variations in heat flow and total fault offset. There appear to be no systematic variations in stress drop (as measured from far-field observations) between earthquakes along the Imperial-Cerro Prieto fault zone and those within the Peninsular Ranges of northern Baja California. Slip rates estimated from historical seismicity between 1915 and 1992 fall ? 1.5 cm yr−1 short of the estimated relative plate motion between the Pacific plate and North America for this region. | ||
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10.1111/j.1365-246X.1994.tb03284.x doi (DE-627)NLEJ239649753 DE-627 ger DE-627 rakwb Doser, Diane I. verfasserin aut Contrasts between source parameters of M < 5.5 earthquakes in northern Baja California and southern California Oxford, UK Blackwell Publishing Ltd 1994 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baja fault systems of southern California and northern Mexico. Observed regional differences in rupture complexity, fault rupture lengths and aftershock/foreshock activity appear to be related to variations in heat flow and total fault offset. There appear to be no systematic variations in stress drop (as measured from far-field observations) between earthquakes along the Imperial-Cerro Prieto fault zone and those within the Peninsular Ranges of northern Baja California. Slip rates estimated from historical seismicity between 1915 and 1992 fall ? 1.5 cm yr−1 short of the estimated relative plate motion between the Pacific plate and North America for this region. 2007 Blackwell Publishing Journal Backfiles 1879-2005 |2007|||||||||| aftershocks In Geophysical journal international Oxford . Wiley-Blackwell, 1922 116(1994), 3, Seite 0 Online-Ressource (DE-627)NLEJ243927827 (DE-600)2006420-2 1365-246X nnns volume:116 year:1994 number:3 pages:0 http://dx.doi.org/10.1111/j.1365-246X.1994.tb03284.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 116 1994 3 0 |
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10.1111/j.1365-246X.1994.tb03284.x doi (DE-627)NLEJ239649753 DE-627 ger DE-627 rakwb Doser, Diane I. verfasserin aut Contrasts between source parameters of M < 5.5 earthquakes in northern Baja California and southern California Oxford, UK Blackwell Publishing Ltd 1994 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baja fault systems of southern California and northern Mexico. Observed regional differences in rupture complexity, fault rupture lengths and aftershock/foreshock activity appear to be related to variations in heat flow and total fault offset. There appear to be no systematic variations in stress drop (as measured from far-field observations) between earthquakes along the Imperial-Cerro Prieto fault zone and those within the Peninsular Ranges of northern Baja California. Slip rates estimated from historical seismicity between 1915 and 1992 fall ? 1.5 cm yr−1 short of the estimated relative plate motion between the Pacific plate and North America for this region. 2007 Blackwell Publishing Journal Backfiles 1879-2005 |2007|||||||||| aftershocks In Geophysical journal international Oxford . Wiley-Blackwell, 1922 116(1994), 3, Seite 0 Online-Ressource (DE-627)NLEJ243927827 (DE-600)2006420-2 1365-246X nnns volume:116 year:1994 number:3 pages:0 http://dx.doi.org/10.1111/j.1365-246X.1994.tb03284.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 116 1994 3 0 |
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10.1111/j.1365-246X.1994.tb03284.x doi (DE-627)NLEJ239649753 DE-627 ger DE-627 rakwb Doser, Diane I. verfasserin aut Contrasts between source parameters of M < 5.5 earthquakes in northern Baja California and southern California Oxford, UK Blackwell Publishing Ltd 1994 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baja fault systems of southern California and northern Mexico. Observed regional differences in rupture complexity, fault rupture lengths and aftershock/foreshock activity appear to be related to variations in heat flow and total fault offset. There appear to be no systematic variations in stress drop (as measured from far-field observations) between earthquakes along the Imperial-Cerro Prieto fault zone and those within the Peninsular Ranges of northern Baja California. Slip rates estimated from historical seismicity between 1915 and 1992 fall ? 1.5 cm yr−1 short of the estimated relative plate motion between the Pacific plate and North America for this region. 2007 Blackwell Publishing Journal Backfiles 1879-2005 |2007|||||||||| aftershocks In Geophysical journal international Oxford . Wiley-Blackwell, 1922 116(1994), 3, Seite 0 Online-Ressource (DE-627)NLEJ243927827 (DE-600)2006420-2 1365-246X nnns volume:116 year:1994 number:3 pages:0 http://dx.doi.org/10.1111/j.1365-246X.1994.tb03284.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 116 1994 3 0 |
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10.1111/j.1365-246X.1994.tb03284.x doi (DE-627)NLEJ239649753 DE-627 ger DE-627 rakwb Doser, Diane I. verfasserin aut Contrasts between source parameters of M < 5.5 earthquakes in northern Baja California and southern California Oxford, UK Blackwell Publishing Ltd 1994 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baja fault systems of southern California and northern Mexico. Observed regional differences in rupture complexity, fault rupture lengths and aftershock/foreshock activity appear to be related to variations in heat flow and total fault offset. There appear to be no systematic variations in stress drop (as measured from far-field observations) between earthquakes along the Imperial-Cerro Prieto fault zone and those within the Peninsular Ranges of northern Baja California. Slip rates estimated from historical seismicity between 1915 and 1992 fall ? 1.5 cm yr−1 short of the estimated relative plate motion between the Pacific plate and North America for this region. 2007 Blackwell Publishing Journal Backfiles 1879-2005 |2007|||||||||| aftershocks In Geophysical journal international Oxford . Wiley-Blackwell, 1922 116(1994), 3, Seite 0 Online-Ressource (DE-627)NLEJ243927827 (DE-600)2006420-2 1365-246X nnns volume:116 year:1994 number:3 pages:0 http://dx.doi.org/10.1111/j.1365-246X.1994.tb03284.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 116 1994 3 0 |
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10.1111/j.1365-246X.1994.tb03284.x doi (DE-627)NLEJ239649753 DE-627 ger DE-627 rakwb Doser, Diane I. verfasserin aut Contrasts between source parameters of M < 5.5 earthquakes in northern Baja California and southern California Oxford, UK Blackwell Publishing Ltd 1994 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baja fault systems of southern California and northern Mexico. Observed regional differences in rupture complexity, fault rupture lengths and aftershock/foreshock activity appear to be related to variations in heat flow and total fault offset. There appear to be no systematic variations in stress drop (as measured from far-field observations) between earthquakes along the Imperial-Cerro Prieto fault zone and those within the Peninsular Ranges of northern Baja California. Slip rates estimated from historical seismicity between 1915 and 1992 fall ? 1.5 cm yr−1 short of the estimated relative plate motion between the Pacific plate and North America for this region. 2007 Blackwell Publishing Journal Backfiles 1879-2005 |2007|||||||||| aftershocks In Geophysical journal international Oxford . Wiley-Blackwell, 1922 116(1994), 3, Seite 0 Online-Ressource (DE-627)NLEJ243927827 (DE-600)2006420-2 1365-246X nnns volume:116 year:1994 number:3 pages:0 http://dx.doi.org/10.1111/j.1365-246X.1994.tb03284.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 116 1994 3 0 |
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Contrasts between source parameters of M < 5.5 earthquakes in northern Baja California and southern California |
| abstract |
Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baja fault systems of southern California and northern Mexico. Observed regional differences in rupture complexity, fault rupture lengths and aftershock/foreshock activity appear to be related to variations in heat flow and total fault offset. There appear to be no systematic variations in stress drop (as measured from far-field observations) between earthquakes along the Imperial-Cerro Prieto fault zone and those within the Peninsular Ranges of northern Baja California. Slip rates estimated from historical seismicity between 1915 and 1992 fall ? 1.5 cm yr−1 short of the estimated relative plate motion between the Pacific plate and North America for this region. |
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Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baja fault systems of southern California and northern Mexico. Observed regional differences in rupture complexity, fault rupture lengths and aftershock/foreshock activity appear to be related to variations in heat flow and total fault offset. There appear to be no systematic variations in stress drop (as measured from far-field observations) between earthquakes along the Imperial-Cerro Prieto fault zone and those within the Peninsular Ranges of northern Baja California. Slip rates estimated from historical seismicity between 1915 and 1992 fall ? 1.5 cm yr−1 short of the estimated relative plate motion between the Pacific plate and North America for this region. |
| abstract_unstemmed |
Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baja fault systems of southern California and northern Mexico. Observed regional differences in rupture complexity, fault rupture lengths and aftershock/foreshock activity appear to be related to variations in heat flow and total fault offset. There appear to be no systematic variations in stress drop (as measured from far-field observations) between earthquakes along the Imperial-Cerro Prieto fault zone and those within the Peninsular Ranges of northern Baja California. Slip rates estimated from historical seismicity between 1915 and 1992 fall ? 1.5 cm yr−1 short of the estimated relative plate motion between the Pacific plate and North America for this region. |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ239649753</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20210707092152.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">120426s1994 xx |||||o 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1111/j.1365-246X.1994.tb03284.x</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ239649753</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Doser, Diane I.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Contrasts between source parameters of M < 5.5 earthquakes in northern Baja California and southern California</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Oxford, UK</subfield><subfield code="b">Blackwell Publishing Ltd</subfield><subfield code="c">1994</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Earthquake source processes are determined for four historic events that occurred in Baja California between 1915 and 1954. These results are combined with previous studies of recent and historic seismicity to compare earthquake processes along the San Jacinto, Imperial-Cerro Prieto and northern Baja fault systems of southern California and northern Mexico. Observed regional differences in rupture complexity, fault rupture lengths and aftershock/foreshock activity appear to be related to variations in heat flow and total fault offset. There appear to be no systematic variations in stress drop (as measured from far-field observations) between earthquakes along the Imperial-Cerro Prieto fault zone and those within the Peninsular Ranges of northern Baja California. Slip rates estimated from historical seismicity between 1915 and 1992 fall ? 1.5 cm yr−1 short of the estimated relative plate motion between the Pacific plate and North America for this region.</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="d">2007</subfield><subfield code="f">Blackwell Publishing Journal Backfiles 1879-2005</subfield><subfield code="7">|2007||||||||||</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">aftershocks</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Geophysical journal international</subfield><subfield code="d">Oxford . Wiley-Blackwell, 1922</subfield><subfield code="g">116(1994), 3, Seite 0</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)NLEJ243927827</subfield><subfield code="w">(DE-600)2006420-2</subfield><subfield code="x">1365-246X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:116</subfield><subfield code="g">year:1994</subfield><subfield code="g">number:3</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1111/j.1365-246X.1994.tb03284.x</subfield><subfield code="q">text/html</subfield><subfield code="x">Verlag</subfield><subfield code="z">Deutschlandweit zugänglich</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-DJB</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">116</subfield><subfield code="j">1994</subfield><subfield code="e">3</subfield><subfield code="h">0</subfield></datafield></record></collection>
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