On the migration of precursors of strong earthquakes
It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic pert...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Bella, F. [verfasserIn] Biag, P.F. [verfasserIn] Caputo, M. [verfasserIn] |
|---|
| Format: |
E-Artikel |
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| Erschienen: |
Oxford, UK: Blackwell Publishing Ltd ; 1992 |
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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: Terra nova - Oxford [u.a.] : Wiley-Blackwell, 1989, 4(1992), 6, Seite 0 |
| Übergeordnetes Werk: |
volume:4 ; year:1992 ; number:6 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1111/j.1365-3121.1992.tb00617.x |
|---|
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NLEJ241894409 |
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| 520 | |a It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic perturbation causes a set of precursors of the same strong earthquake is discussed and it is concluded that each precursor is associated with a different perturbation. | ||
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| 700 | 1 | |a Caputo, M. |e verfasserin |4 aut | |
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| 700 | 1 | |a Ermini, A. |4 oth | |
| 700 | 1 | |a Sgrigna, V. |4 oth | |
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10.1111/j.1365-3121.1992.tb00617.x doi (DE-627)NLEJ241894409 DE-627 ger DE-627 rakwb Bella, F. verfasserin aut On the migration of precursors of strong earthquakes Oxford, UK Blackwell Publishing Ltd 1992 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic perturbation causes a set of precursors of the same strong earthquake is discussed and it is concluded that each precursor is associated with a different perturbation. 2007 Blackwell Publishing Journal Backfiles 1879-2005 |2007|||||||||| Biag, P.F. verfasserin aut Caputo, M. verfasserin aut Monica, G. Della oth Ermini, A. oth Sgrigna, V. oth In Terra nova Oxford [u.a.] : Wiley-Blackwell, 1989 4(1992), 6, Seite 0 Online-Ressource (DE-627)NLEJ243926359 (DE-600)2020958-7 1365-3121 nnns volume:4 year:1992 number:6 pages:0 http://dx.doi.org/10.1111/j.1365-3121.1992.tb00617.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 4 1992 6 0 |
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10.1111/j.1365-3121.1992.tb00617.x doi (DE-627)NLEJ241894409 DE-627 ger DE-627 rakwb Bella, F. verfasserin aut On the migration of precursors of strong earthquakes Oxford, UK Blackwell Publishing Ltd 1992 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic perturbation causes a set of precursors of the same strong earthquake is discussed and it is concluded that each precursor is associated with a different perturbation. 2007 Blackwell Publishing Journal Backfiles 1879-2005 |2007|||||||||| Biag, P.F. verfasserin aut Caputo, M. verfasserin aut Monica, G. Della oth Ermini, A. oth Sgrigna, V. oth In Terra nova Oxford [u.a.] : Wiley-Blackwell, 1989 4(1992), 6, Seite 0 Online-Ressource (DE-627)NLEJ243926359 (DE-600)2020958-7 1365-3121 nnns volume:4 year:1992 number:6 pages:0 http://dx.doi.org/10.1111/j.1365-3121.1992.tb00617.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 4 1992 6 0 |
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10.1111/j.1365-3121.1992.tb00617.x doi (DE-627)NLEJ241894409 DE-627 ger DE-627 rakwb Bella, F. verfasserin aut On the migration of precursors of strong earthquakes Oxford, UK Blackwell Publishing Ltd 1992 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic perturbation causes a set of precursors of the same strong earthquake is discussed and it is concluded that each precursor is associated with a different perturbation. 2007 Blackwell Publishing Journal Backfiles 1879-2005 |2007|||||||||| Biag, P.F. verfasserin aut Caputo, M. verfasserin aut Monica, G. Della oth Ermini, A. oth Sgrigna, V. oth In Terra nova Oxford [u.a.] : Wiley-Blackwell, 1989 4(1992), 6, Seite 0 Online-Ressource (DE-627)NLEJ243926359 (DE-600)2020958-7 1365-3121 nnns volume:4 year:1992 number:6 pages:0 http://dx.doi.org/10.1111/j.1365-3121.1992.tb00617.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 4 1992 6 0 |
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10.1111/j.1365-3121.1992.tb00617.x doi (DE-627)NLEJ241894409 DE-627 ger DE-627 rakwb Bella, F. verfasserin aut On the migration of precursors of strong earthquakes Oxford, UK Blackwell Publishing Ltd 1992 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic perturbation causes a set of precursors of the same strong earthquake is discussed and it is concluded that each precursor is associated with a different perturbation. 2007 Blackwell Publishing Journal Backfiles 1879-2005 |2007|||||||||| Biag, P.F. verfasserin aut Caputo, M. verfasserin aut Monica, G. Della oth Ermini, A. oth Sgrigna, V. oth In Terra nova Oxford [u.a.] : Wiley-Blackwell, 1989 4(1992), 6, Seite 0 Online-Ressource (DE-627)NLEJ243926359 (DE-600)2020958-7 1365-3121 nnns volume:4 year:1992 number:6 pages:0 http://dx.doi.org/10.1111/j.1365-3121.1992.tb00617.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 4 1992 6 0 |
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10.1111/j.1365-3121.1992.tb00617.x doi (DE-627)NLEJ241894409 DE-627 ger DE-627 rakwb Bella, F. verfasserin aut On the migration of precursors of strong earthquakes Oxford, UK Blackwell Publishing Ltd 1992 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic perturbation causes a set of precursors of the same strong earthquake is discussed and it is concluded that each precursor is associated with a different perturbation. 2007 Blackwell Publishing Journal Backfiles 1879-2005 |2007|||||||||| Biag, P.F. verfasserin aut Caputo, M. verfasserin aut Monica, G. Della oth Ermini, A. oth Sgrigna, V. oth In Terra nova Oxford [u.a.] : Wiley-Blackwell, 1989 4(1992), 6, Seite 0 Online-Ressource (DE-627)NLEJ243926359 (DE-600)2020958-7 1365-3121 nnns volume:4 year:1992 number:6 pages:0 http://dx.doi.org/10.1111/j.1365-3121.1992.tb00617.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 4 1992 6 0 |
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on the migration of precursors of strong earthquakes |
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On the migration of precursors of strong earthquakes |
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It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic perturbation causes a set of precursors of the same strong earthquake is discussed and it is concluded that each precursor is associated with a different perturbation. |
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It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic perturbation causes a set of precursors of the same strong earthquake is discussed and it is concluded that each precursor is associated with a different perturbation. |
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It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic perturbation causes a set of precursors of the same strong earthquake is discussed and it is concluded that each precursor is associated with a different perturbation. |
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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">NLEJ241894409</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20210707143428.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">120427s1992 xx |||||o 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1111/j.1365-3121.1992.tb00617.x</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ241894409</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">Bella, F.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">On the migration of precursors of strong earthquakes</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Oxford, UK</subfield><subfield code="b">Blackwell Publishing Ltd</subfield><subfield code="c">1992</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">It is found that perturbations presumedly associated with swarms, the B patterns and the BG pattern precursors of strong earthquakes in New Zealand, California and Apennines, propagate in the crust of the Earth with a velocity of the order of cm1. The hypothesis that a single travelling elastic perturbation causes a set of precursors of the same strong earthquake is discussed and it is concluded that each precursor is associated with a different perturbation.</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="700" ind1="1" ind2=" "><subfield code="a">Biag, P.F.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Caputo, M.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Monica, G. Della</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ermini, A.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sgrigna, V.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Terra nova</subfield><subfield code="d">Oxford [u.a.] : Wiley-Blackwell, 1989</subfield><subfield code="g">4(1992), 6, Seite 0</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)NLEJ243926359</subfield><subfield code="w">(DE-600)2020958-7</subfield><subfield code="x">1365-3121</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:4</subfield><subfield code="g">year:1992</subfield><subfield code="g">number:6</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.1365-3121.1992.tb00617.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">4</subfield><subfield code="j">1992</subfield><subfield code="e">6</subfield><subfield code="h">0</subfield></datafield></record></collection>
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