The 20 March 1992 South Aegean, Greece, earthquake (Ms= 5.3): possible anomalous effects
Identifieur interne : 000379 ( Istex/Corpus ); précédent : 000378; suivant : 000380The 20 March 1992 South Aegean, Greece, earthquake (Ms= 5.3): possible anomalous effects
Auteurs : Gerassimos A. PapadopoulosSource :
- Terra Nova [ 0954-4879 ] ; 1993-07.
English descriptors
- KwdEn :
- Aftershock, Aftershock sequence, Ancient times, Building damage, Central part, Continental deformation, Earthquake, Earthquake epicentre, Earthquake magnitude, Earthquake planning, Earthquake precursors, Earthquake sequence, Epicentral, Epicentral distance, Fundamental research, Ground acceleration, Ground cracks, Ground failures, Hellenic system, Hivadolimni, Instrumental data, Instrumental period, Larger events, Largest aftershock, Liquefaction, Liquefaction occurrence, Long distance, Mainshock, Many others, Many places, Maximum intensity, Microearthquake activity, Milo, Milos island, National observatory, Other greek regions, Paleomagnetic rotations, Papadopoulos, Papazachos, Precursor, Precursor time, Preliminary location, Protection organization, Regression analysis, Seismic, Seismic events, Seismological institute, Several disciplines, Small earthquake magnitude, Southern part, Straight line, Tectonic, Tectonic earthquakes, Tectonic origin, Tokyo univ, Village houses, Volcanic, Volcanic activities, Volcanic activity, Volcanic eruptions, Volcanic island, Volcanic products.
- Teeft :
- Aftershock, Aftershock sequence, Ancient times, Building damage, Central part, Continental deformation, Earthquake, Earthquake epicentre, Earthquake magnitude, Earthquake planning, Earthquake precursors, Earthquake sequence, Epicentral, Epicentral distance, Fundamental research, Ground acceleration, Ground cracks, Ground failures, Hellenic system, Hivadolimni, Instrumental data, Instrumental period, Larger events, Largest aftershock, Liquefaction, Liquefaction occurrence, Long distance, Mainshock, Many others, Many places, Maximum intensity, Microearthquake activity, Milo, Milos island, National observatory, Other greek regions, Paleomagnetic rotations, Papadopoulos, Papazachos, Precursor, Precursor time, Preliminary location, Protection organization, Regression analysis, Seismic, Seismic events, Seismological institute, Several disciplines, Small earthquake magnitude, Southern part, Straight line, Tectonic, Tectonic earthquakes, Tectonic origin, Tokyo univ, Village houses, Volcanic, Volcanic activities, Volcanic activity, Volcanic eruptions, Volcanic island, Volcanic products.
Abstract
The earthquake (Ms= 5.3) of 20 March 1992 and its aftershocks, which occurred near the volcanic island complex of Milos, South Aegean, Greece, are studied on the basis of filed observations and instrumental data. The mainshock caused some building damage, the maximum intensity of VI+ (MM) being assigned to Triovasalos, Milos. Ground cracks, liquefaction in soil, landslides and rockfalls were observed in Milos. Liquefaction took place at an apparently anomalously long epicentral distance (D= 12 km) and is associated with unusually small earthquake magnitude. Abnormal animal behaviour was reported no longer than twelve hours before the mainshock. The b‐value (= 1.02) of the G–R relation for the aftershock sequence, the exponentially decreasing number of aftershocks with time, and the difference (= 0.5) in magnitude between the mainshock and its largest aftershock imply that the origin of these earthquakes is tectonic and not associated with the volcanic field of Milos.
Url:
DOI: 10.1111/j.1365-3121.1993.tb00273.x
Links to Exploration step
ISTEX:E090F7CFFDCDE4B99D89653C42C91074CBD513ACLe document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">The 20 March 1992 South Aegean, Greece, earthquake (Ms= 5.3): possible anomalous effects</title><author><name sortKey="Papadopoulos, Gerassimos A" sort="Papadopoulos, Gerassimos A" uniqKey="Papadopoulos G" first="Gerassimos A." last="Papadopoulos">Gerassimos A. Papadopoulos</name><affiliation><mods:affiliation>Department of Seismotectonics, Earthquake Planning and Protection Organization, 226 Messogion Ave., 15561 Athens, Greece</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:E090F7CFFDCDE4B99D89653C42C91074CBD513AC</idno><date when="1993" year="1993">1993</date><idno type="doi">10.1111/j.1365-3121.1993.tb00273.x</idno><idno type="url">https://api.istex.fr/document/E090F7CFFDCDE4B99D89653C42C91074CBD513AC/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000379</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000379</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main">The 20 March 1992 South Aegean, Greece, earthquake (<hi rend="italic">M</hi><hi rend="subscript">s</hi>= 5.3): possible anomalous effects</title><author><name sortKey="Papadopoulos, Gerassimos A" sort="Papadopoulos, Gerassimos A" uniqKey="Papadopoulos G" first="Gerassimos A." last="Papadopoulos">Gerassimos A. Papadopoulos</name><affiliation><mods:affiliation>Department of Seismotectonics, Earthquake Planning and Protection Organization, 226 Messogion Ave., 15561 Athens, Greece</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j" type="main">Terra Nova</title><title level="j" type="alt">TERRA NOVA</title><idno type="ISSN">0954-4879</idno><idno type="eISSN">1365-3121</idno><imprint><biblScope unit="vol">5</biblScope><biblScope unit="issue">4</biblScope><biblScope unit="page" from="399">399</biblScope><biblScope unit="page" to="404">404</biblScope><biblScope unit="page-count">6</biblScope><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="1993-07">1993-07</date></imprint><idno type="ISSN">0954-4879</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0954-4879</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Aftershock</term><term>Aftershock sequence</term><term>Ancient times</term><term>Building damage</term><term>Central part</term><term>Continental deformation</term><term>Earthquake</term><term>Earthquake epicentre</term><term>Earthquake magnitude</term><term>Earthquake planning</term><term>Earthquake precursors</term><term>Earthquake sequence</term><term>Epicentral</term><term>Epicentral distance</term><term>Fundamental research</term><term>Ground acceleration</term><term>Ground cracks</term><term>Ground failures</term><term>Hellenic system</term><term>Hivadolimni</term><term>Instrumental data</term><term>Instrumental period</term><term>Larger events</term><term>Largest aftershock</term><term>Liquefaction</term><term>Liquefaction occurrence</term><term>Long distance</term><term>Mainshock</term><term>Many others</term><term>Many places</term><term>Maximum intensity</term><term>Microearthquake activity</term><term>Milo</term><term>Milos island</term><term>National observatory</term><term>Other greek regions</term><term>Paleomagnetic rotations</term><term>Papadopoulos</term><term>Papazachos</term><term>Precursor</term><term>Precursor time</term><term>Preliminary location</term><term>Protection organization</term><term>Regression analysis</term><term>Seismic</term><term>Seismic events</term><term>Seismological institute</term><term>Several disciplines</term><term>Small earthquake magnitude</term><term>Southern part</term><term>Straight line</term><term>Tectonic</term><term>Tectonic earthquakes</term><term>Tectonic origin</term><term>Tokyo univ</term><term>Village houses</term><term>Volcanic</term><term>Volcanic activities</term><term>Volcanic activity</term><term>Volcanic eruptions</term><term>Volcanic island</term><term>Volcanic products</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Aftershock</term><term>Aftershock sequence</term><term>Ancient times</term><term>Building damage</term><term>Central part</term><term>Continental deformation</term><term>Earthquake</term><term>Earthquake epicentre</term><term>Earthquake magnitude</term><term>Earthquake planning</term><term>Earthquake precursors</term><term>Earthquake sequence</term><term>Epicentral</term><term>Epicentral distance</term><term>Fundamental research</term><term>Ground acceleration</term><term>Ground cracks</term><term>Ground failures</term><term>Hellenic system</term><term>Hivadolimni</term><term>Instrumental data</term><term>Instrumental period</term><term>Larger events</term><term>Largest aftershock</term><term>Liquefaction</term><term>Liquefaction occurrence</term><term>Long distance</term><term>Mainshock</term><term>Many others</term><term>Many places</term><term>Maximum intensity</term><term>Microearthquake activity</term><term>Milo</term><term>Milos island</term><term>National observatory</term><term>Other greek regions</term><term>Paleomagnetic rotations</term><term>Papadopoulos</term><term>Papazachos</term><term>Precursor</term><term>Precursor time</term><term>Preliminary location</term><term>Protection organization</term><term>Regression analysis</term><term>Seismic</term><term>Seismic events</term><term>Seismological institute</term><term>Several disciplines</term><term>Small earthquake magnitude</term><term>Southern part</term><term>Straight line</term><term>Tectonic</term><term>Tectonic earthquakes</term><term>Tectonic origin</term><term>Tokyo univ</term><term>Village houses</term><term>Volcanic</term><term>Volcanic activities</term><term>Volcanic activity</term><term>Volcanic eruptions</term><term>Volcanic island</term><term>Volcanic products</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The earthquake (Ms= 5.3) of 20 March 1992 and its aftershocks, which occurred near the volcanic island complex of Milos, South Aegean, Greece, are studied on the basis of filed observations and instrumental data. The mainshock caused some building damage, the maximum intensity of VI+ (MM) being assigned to Triovasalos, Milos. Ground cracks, liquefaction in soil, landslides and rockfalls were observed in Milos. Liquefaction took place at an apparently anomalously long epicentral distance (D= 12 km) and is associated with unusually small earthquake magnitude. Abnormal animal behaviour was reported no longer than twelve hours before the mainshock. The b‐value (= 1.02) of the G–R relation for the aftershock sequence, the exponentially decreasing number of aftershocks with time, and the difference (= 0.5) in magnitude between the mainshock and its largest aftershock imply that the origin of these earthquakes is tectonic and not associated with the volcanic field of Milos.</div></front></TEI><istex><corpusName>wiley</corpusName><keywords><teeft><json:string>milo</json:string><json:string>papadopoulos</json:string><json:string>aftershock</json:string><json:string>mainshock</json:string><json:string>liquefaction</json:string><json:string>papazachos</json:string><json:string>tectonic</json:string><json:string>precursor</json:string><json:string>epicentral</json:string><json:string>hivadolimni</json:string><json:string>epicentral distance</json:string><json:string>ground cracks</json:string><json:string>earthquake precursors</json:string><json:string>seismic</json:string><json:string>volcanic</json:string><json:string>maximum intensity</json:string><json:string>earthquake magnitude</json:string><json:string>earthquake</json:string><json:string>volcanic island</json:string><json:string>earthquake sequence</json:string><json:string>microearthquake activity</json:string><json:string>largest aftershock</json:string><json:string>precursor time</json:string><json:string>milos island</json:string><json:string>straight line</json:string><json:string>ground acceleration</json:string><json:string>tectonic origin</json:string><json:string>volcanic eruptions</json:string><json:string>ground failures</json:string><json:string>other greek regions</json:string><json:string>instrumental period</json:string><json:string>aftershock sequence</json:string><json:string>preliminary location</json:string><json:string>protection organization</json:string><json:string>larger events</json:string><json:string>ancient times</json:string><json:string>instrumental data</json:string><json:string>volcanic activities</json:string><json:string>several disciplines</json:string><json:string>many others</json:string><json:string>earthquake planning</json:string><json:string>building damage</json:string><json:string>volcanic activity</json:string><json:string>southern part</json:string><json:string>village houses</json:string><json:string>earthquake epicentre</json:string><json:string>seismological institute</json:string><json:string>many places</json:string><json:string>central part</json:string><json:string>liquefaction occurrence</json:string><json:string>long distance</json:string><json:string>tectonic earthquakes</json:string><json:string>regression analysis</json:string><json:string>national observatory</json:string><json:string>hellenic system</json:string><json:string>fundamental research</json:string><json:string>volcanic products</json:string><json:string>tokyo univ</json:string><json:string>small earthquake magnitude</json:string><json:string>paleomagnetic rotations</json:string><json:string>continental deformation</json:string><json:string>seismic events</json:string></teeft></keywords><author><json:item><name>Gerassimos A. Papadopoulos</name><affiliations><json:string>Department of Seismotectonics, Earthquake Planning and Protection Organization, 226 Messogion Ave., 15561 Athens, Greece</json:string></affiliations></json:item></author><articleId><json:string>TER399</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>The earthquake (Ms= 5.3) of 20 March 1992 and its aftershocks, which occurred near the volcanic island complex of Milos, South Aegean, Greece, are studied on the basis of filed observations and instrumental data. The mainshock caused some building damage, the maximum intensity of VI+ (MM) being assigned to Triovasalos, Milos. Ground cracks, liquefaction in soil, landslides and rockfalls were observed in Milos. Liquefaction took place at an apparently anomalously long epicentral distance (D= 12 km) and is associated with unusually small earthquake magnitude. Abnormal animal behaviour was reported no longer than twelve hours before the mainshock. The b‐value (= 1.02) of the G–R relation for the aftershock sequence, the exponentially decreasing number of aftershocks with time, and the difference (= 0.5) in magnitude between the mainshock and its largest aftershock imply that the origin of these earthquakes is tectonic and not associated with the volcanic field of Milos.</abstract><qualityIndicators><score>5.914</score><pdfVersion>1.4</pdfVersion><pdfPageSize>588.959 x 783.839 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>981</abstractCharCount><pdfWordCount>3626</pdfWordCount><pdfCharCount>24150</pdfCharCount><pdfPageCount>6</pdfPageCount><abstractWordCount>149</abstractWordCount></qualityIndicators><title>The 20 March 1992 South Aegean, Greece, earthquake (Ms= 5.3): possible anomalous effects</title><genre><json:string>article</json:string></genre><host><title>Terra Nova</title><language><json:string>unknown</json:string></language><doi><json:string>10.1111/(ISSN)1365-3121</json:string></doi><issn><json:string>0954-4879</json:string></issn><eissn><json:string>1365-3121</json:string></eissn><publisherId><json:string>TER</json:string></publisherId><volume>5</volume><issue>4</issue><pages><first>399</first><last>404</last><total>6</total></pages><genre><json:string>journal</json:string></genre></host><categories><wos><json:string>science</json:string><json:string>geosciences, multidisciplinary</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>earth & environmental sciences</json:string><json:string>geochemistry & geophysics</json:string></scienceMetrix><inist><json:string>sciences appliquees, technologies et medecines</json:string><json:string>sciences exactes et technologie</json:string><json:string>terre, ocean, espace</json:string><json:string>sciences de la terre</json:string></inist></categories><publicationDate>1993</publicationDate><copyrightDate>1993</copyrightDate><doi><json:string>10.1111/j.1365-3121.1993.tb00273.x</json:string></doi><id>E090F7CFFDCDE4B99D89653C42C91074CBD513AC</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/E090F7CFFDCDE4B99D89653C42C91074CBD513AC/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/E090F7CFFDCDE4B99D89653C42C91074CBD513AC/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/E090F7CFFDCDE4B99D89653C42C91074CBD513AC/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main">The 20 March 1992 South Aegean, Greece, earthquake (<hi rend="italic">M</hi><hi rend="subscript">s</hi>= 5.3): possible anomalous effects</title></titleStmt><publicationStmt><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="1993-07"></date></publicationStmt><notesStmt><note type="content-type" subtype="article" source="article" scheme="https://content-type.data.istex.fr/ark:/67375/XTP-6N5SZHKN-D">article</note><note type="publication-type" subtype="journal" scheme="https://publication-type.data.istex.fr/ark:/67375/JMC-0GLKJH51-B">journal</note></notesStmt><sourceDesc><biblStruct type="article"><analytic><title level="a" type="main">The 20 March 1992 South Aegean, Greece, earthquake (<hi rend="italic">M</hi><hi rend="subscript">s</hi>= 5.3): possible anomalous effects</title><author xml:id="author-0000"><persName><forename type="first">Gerassimos A.</forename><surname>Papadopoulos</surname></persName><affiliation>Department of Seismotectonics, Earthquake Planning and Protection Organization, 226 Messogion Ave., 15561 Athens, Greece<address><country key="GR"></country></address></affiliation></author><idno type="istex">E090F7CFFDCDE4B99D89653C42C91074CBD513AC</idno><idno type="DOI">10.1111/j.1365-3121.1993.tb00273.x</idno><idno type="unit">TER399</idno><idno type="toTypesetVersion">file:TER.TER399.pdf</idno></analytic><monogr><title level="j" type="main">Terra Nova</title><title level="j" type="alt">TERRA NOVA</title><idno type="pISSN">0954-4879</idno><idno type="eISSN">1365-3121</idno><idno type="book-DOI">10.1111/(ISSN)1365-3121</idno><idno type="book-part-DOI">10.1111/ter.1993.5.issue-4</idno><idno type="product">TER</idno><idno type="publisherDivision">ST</idno><imprint><biblScope unit="vol">5</biblScope><biblScope unit="issue">4</biblScope><biblScope unit="page" from="399">399</biblScope><biblScope unit="page" to="404">404</biblScope><biblScope unit="page-count">6</biblScope><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="1993-07"></date></imprint></monogr></biblStruct></sourceDesc></fileDesc><profileDesc><abstract xml:lang="en" style="main"><p>The earthquake (<hi rend="italic">M</hi><hi rend="subscript">s</hi>= 5.3) of 20 March 1992 and its aftershocks, which occurred near the volcanic island complex of Milos, South Aegean, Greece, are studied on the basis of filed observations and instrumental data. The mainshock caused some building damage, the maximum intensity of VI+ (MM) being assigned to Triovasalos, Milos. Ground cracks, liquefaction in soil, landslides and rockfalls were observed in Milos. Liquefaction took place at an apparently anomalously long epicentral distance (<hi rend="italic">D</hi>= 12 km) and is associated with unusually small earthquake magnitude. Abnormal animal behaviour was reported no longer than twelve hours before the mainshock. The <hi rend="italic">b</hi>‐value (= 1.02) of the G–R relation for the aftershock sequence, the exponentially decreasing number of aftershocks with time, and the difference (= 0.5) in magnitude between the mainshock and its largest aftershock imply that the origin of these earthquakes is tectonic and not associated with the volcanic field of Milos.</p></abstract><langUsage><language ident="EN"></language></langUsage></profileDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/E090F7CFFDCDE4B99D89653C42C91074CBD513AC/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component version="2.0" type="serialArticle" xml:lang="en"><header><publicationMeta level="product"><publisherInfo><publisherName>Blackwell Publishing Ltd</publisherName><publisherLoc>Oxford, UK</publisherLoc></publisherInfo><doi origin="wiley" registered="yes">10.1111/(ISSN)1365-3121</doi><issn type="print">0954-4879</issn><issn type="electronic">1365-3121</issn><idGroup><id type="product" value="TER"></id><id type="publisherDivision" value="ST"></id></idGroup><titleGroup><title type="main" sort="TERRA NOVA">Terra Nova</title></titleGroup></publicationMeta><publicationMeta level="part" position="07004"><doi origin="wiley">10.1111/ter.1993.5.issue-4</doi><numberingGroup><numbering type="journalVolume" number="5">5</numbering><numbering type="journalIssue" number="4">4</numbering></numberingGroup><coverDate startDate="1993-07">July 1993</coverDate></publicationMeta><publicationMeta level="unit" type="article" position="0039900" status="forIssue"><doi origin="wiley">10.1111/j.1365-3121.1993.tb00273.x</doi><idGroup><id type="unit" value="TER399"></id></idGroup><countGroup><count type="pageTotal" number="6"></count></countGroup><eventGroup><event type="firstOnline" date="2007-07-01"></event><event type="publishedOnlineFinalForm" date="2007-07-01"></event><event type="xmlConverted" agent="Converter:BPG_TO_WML3G version:2.3.2 mode:FullText source:HeaderRef result:HeaderRef" date="2010-03-02"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:3.8.8" date="2014-02-10"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-11-04"></event></eventGroup><numberingGroup><numbering type="pageFirst" number="399">399</numbering><numbering type="pageLast" number="404">404</numbering></numberingGroup><linkGroup><link type="toTypesetVersion" href="file:TER.TER399.pdf"></link></linkGroup></publicationMeta><contentMeta><unparsedEditorialHistory>14 August 1992, revision accepted 11 December 1992</unparsedEditorialHistory><countGroup><count type="referenceTotal" number="35"></count><count type="linksCrossRef" number="1"></count></countGroup><titleGroup><title type="main">The 20 March 1992 South Aegean, Greece, earthquake (<i>M</i><sub>s</sub>= 5.3): possible anomalous effects</title></titleGroup><creators><creator creatorRole="author" xml:id="cr1" affiliationRef="#a1"><personName><givenNames>Gerassimos A.</givenNames><familyName>Papadopoulos</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="a1" countryCode="GR"><unparsedAffiliation>Department of Seismotectonics, Earthquake Planning and Protection Organization, 226 Messogion Ave., 15561 Athens, Greece</unparsedAffiliation></affiliation></affiliationGroup><abstractGroup><abstract type="main" xml:lang="en"><p>The earthquake (<i>M</i><sub>s</sub>= 5.3) of 20 March 1992 and its aftershocks, which occurred near the volcanic island complex of Milos, South Aegean, Greece, are studied on the basis of filed observations and instrumental data. The mainshock caused some building damage, the maximum intensity of VI+ (MM) being assigned to Triovasalos, Milos. Ground cracks, liquefaction in soil, landslides and rockfalls were observed in Milos. Liquefaction took place at an apparently anomalously long epicentral distance (<i>D</i>= 12 km) and is associated with unusually small earthquake magnitude. Abnormal animal behaviour was reported no longer than twelve hours before the mainshock. The <i>b</i>‐value (= 1.02) of the G–R relation for the aftershock sequence, the exponentially decreasing number of aftershocks with time, and the difference (= 0.5) in magnitude between the mainshock and its largest aftershock imply that the origin of these earthquakes is tectonic and not associated with the volcanic field of Milos.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>The 20 March 1992 South Aegean, Greece, earthquake (Ms= 5.3): possible anomalous effects</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>The 20 March 1992 South Aegean, Greece, earthquake (Ms= 5.3): possible anomalous effects</title></titleInfo><name type="personal"><namePart type="given">Gerassimos A.</namePart><namePart type="family">Papadopoulos</namePart><affiliation>Department of Seismotectonics, Earthquake Planning and Protection Organization, 226 Messogion Ave., 15561 Athens, Greece</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><place><placeTerm type="text">Oxford, UK</placeTerm></place><dateIssued encoding="w3cdtf">1993-07</dateIssued><edition>14 August 1992, revision accepted 11 December 1992</edition><copyrightDate encoding="w3cdtf">1993</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="references">35</extent></physicalDescription><abstract lang="en">The earthquake (Ms= 5.3) of 20 March 1992 and its aftershocks, which occurred near the volcanic island complex of Milos, South Aegean, Greece, are studied on the basis of filed observations and instrumental data. The mainshock caused some building damage, the maximum intensity of VI+ (MM) being assigned to Triovasalos, Milos. Ground cracks, liquefaction in soil, landslides and rockfalls were observed in Milos. Liquefaction took place at an apparently anomalously long epicentral distance (D= 12 km) and is associated with unusually small earthquake magnitude. Abnormal animal behaviour was reported no longer than twelve hours before the mainshock. The b‐value (= 1.02) of the G–R relation for the aftershock sequence, the exponentially decreasing number of aftershocks with time, and the difference (= 0.5) in magnitude between the mainshock and its largest aftershock imply that the origin of these earthquakes is tectonic and not associated with the volcanic field of Milos.</abstract><relatedItem type="host"><titleInfo><title>Terra Nova</title></titleInfo><genre type="journal">journal</genre><identifier type="ISSN">0954-4879</identifier><identifier type="eISSN">1365-3121</identifier><identifier type="DOI">10.1111/(ISSN)1365-3121</identifier><identifier type="PublisherID">TER</identifier><part><date>1993</date><detail type="volume"><caption>vol.</caption><number>5</number></detail><detail type="issue"><caption>no.</caption><number>4</number></detail><extent unit="pages"><start>399</start><end>404</end><total>6</total></extent></part></relatedItem><identifier type="istex">E090F7CFFDCDE4B99D89653C42C91074CBD513AC</identifier><identifier type="DOI">10.1111/j.1365-3121.1993.tb00273.x</identifier><identifier type="ArticleID">TER399</identifier><recordInfo><recordContentSource>WILEY</recordContentSource><recordOrigin>Blackwell Publishing Ltd</recordOrigin></recordInfo></mods><json:item><extension>json</extension><original>false</original><mimetype>application/json</mimetype><uri>https://api.istex.fr/document/E090F7CFFDCDE4B99D89653C42C91074CBD513AC/metadata/json</uri></json:item></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Terre/explor/NissirosV1/Data/Istex/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000379 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 000379 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Terre
|area= NissirosV1
|flux= Istex
|étape= Corpus
|type= RBID
|clé= ISTEX:E090F7CFFDCDE4B99D89653C42C91074CBD513AC
|texte= The 20 March 1992 South Aegean, Greece, earthquake (Ms= 5.3): possible anomalous effects
}}
| This area was generated with Dilib version V0.6.33. |  |