Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece
Identifieur interne : 000363 ( Istex/Corpus ); précédent : 000362; suivant : 000364Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece
Auteurs : C. Thanassoulas ; N. XanthopoulosSource :
- Geothermics [ 0375-6505 ] ; 1991.
English descriptors
- KwdEn :
- Anomaly, Conductive, Conductive zones, Crystalline, Crystalline basement, Fracture, Fracture zones, Geoelectrical, Geophysical, Geophysical methods, Geophysical study, Geotermica italiana, Geotest, Geotest hellas, Geothermal, Geothermal fields, Gravity modelling, Gravity models, Ground surface, Hellas, High conductivity zones, Igme, Lesvos, Lesvos island, Peridotitic body, Polyhnitos, Polyhnitos area, Target areas, Tectonic features, Thanassoulas, Xanthopoulos.
- Teeft :
- Anomaly, Conductive, Conductive zones, Crystalline, Crystalline basement, Fracture, Fracture zones, Geoelectrical, Geophysical, Geophysical methods, Geophysical study, Geotermica italiana, Geotest, Geotest hellas, Geothermal, Geothermal fields, Gravity modelling, Gravity models, Ground surface, Hellas, High conductivity zones, Igme, Lesvos, Lesvos island, Peridotitic body, Polyhnitos, Polyhnitos area, Target areas, Tectonic features, Thanassoulas, Xanthopoulos.
Abstract
Abstract: In 1988, Geotest Hellas carried out a geophysical survey on Lesvos island using gravity, vertical electrical soundings and self-potential methods in order to study the geothermal potential of the island. This paper is based on the primary results presented by Geotest Hellas, which were re-examined and presented in a different form to facilitate the selection of the areas of strong geothermal interest. In particular, application of the gravity, vertical electrical sounding (VES) and self-potential (SP) methods has provided information on the geophysical structure of the geothermal target areas of Lesvos island. The gravity survey provided valuable information on the morphology and tectonics of the crystalline basement (and on the peridotitic body and pyroclastic sediments), for the study of the geothermal potential of the area. The electrical survey provided information on the highly conductive zones (usually associated with geothermal fields), the electrical stratigraphy and the tectonics of the main geological units of the target area. The SP survey mapped areas where electrical polarization is observed in the faulting system. An integrated interpretation of the results of all these surveys led to the selection of five target areas considered to be of high geothermal potential. The location of these target areas is shown in Fig. 14, ranked from 1 to 5 in decreasing order of priority.
Url:
DOI: 10.1016/0375-6505(91)90026-R
Links to Exploration step
ISTEX:A343123EA16384E91CECBDD0112F1A9A2E676180Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title>Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece</title>
<author><name sortKey="Thanassoulas, C" sort="Thanassoulas, C" uniqKey="Thanassoulas C" first="C." last="Thanassoulas">C. Thanassoulas</name>
<affiliation><mods:affiliation>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</mods:affiliation>
</affiliation>
</author>
<author><name sortKey="Xanthopoulos, N" sort="Xanthopoulos, N" uniqKey="Xanthopoulos N" first="N." last="Xanthopoulos">N. Xanthopoulos</name>
<affiliation><mods:affiliation>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</mods:affiliation>
</affiliation>
</author>
</titleStmt>
<publicationStmt><idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:A343123EA16384E91CECBDD0112F1A9A2E676180</idno>
<date when="1991" year="1991">1991</date>
<idno type="doi">10.1016/0375-6505(91)90026-R</idno>
<idno type="url">https://api.istex.fr/document/A343123EA16384E91CECBDD0112F1A9A2E676180/fulltext/pdf</idno>
<idno type="wicri:Area/Istex/Corpus">000363</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000363</idno>
</publicationStmt>
<sourceDesc><biblStruct><analytic><title level="a">Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece</title>
<author><name sortKey="Thanassoulas, C" sort="Thanassoulas, C" uniqKey="Thanassoulas C" first="C." last="Thanassoulas">C. Thanassoulas</name>
<affiliation><mods:affiliation>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</mods:affiliation>
</affiliation>
</author>
<author><name sortKey="Xanthopoulos, N" sort="Xanthopoulos, N" uniqKey="Xanthopoulos N" first="N." last="Xanthopoulos">N. Xanthopoulos</name>
<affiliation><mods:affiliation>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</mods:affiliation>
</affiliation>
</author>
</analytic>
<monogr></monogr>
<series><title level="j">Geothermics</title>
<title level="j" type="abbrev">GEOT</title>
<idno type="ISSN">0375-6505</idno>
<imprint><publisher>ELSEVIER</publisher>
<date type="published" when="1991">1991</date>
<biblScope unit="volume">20</biblScope>
<biblScope unit="issue">5–6</biblScope>
<biblScope unit="page" from="355">355</biblScope>
<biblScope unit="page" to="368">368</biblScope>
</imprint>
<idno type="ISSN">0375-6505</idno>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt><idno type="ISSN">0375-6505</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Anomaly</term>
<term>Conductive</term>
<term>Conductive zones</term>
<term>Crystalline</term>
<term>Crystalline basement</term>
<term>Fracture</term>
<term>Fracture zones</term>
<term>Geoelectrical</term>
<term>Geophysical</term>
<term>Geophysical methods</term>
<term>Geophysical study</term>
<term>Geotermica italiana</term>
<term>Geotest</term>
<term>Geotest hellas</term>
<term>Geothermal</term>
<term>Geothermal fields</term>
<term>Gravity modelling</term>
<term>Gravity models</term>
<term>Ground surface</term>
<term>Hellas</term>
<term>High conductivity zones</term>
<term>Igme</term>
<term>Lesvos</term>
<term>Lesvos island</term>
<term>Peridotitic body</term>
<term>Polyhnitos</term>
<term>Polyhnitos area</term>
<term>Target areas</term>
<term>Tectonic features</term>
<term>Thanassoulas</term>
<term>Xanthopoulos</term>
</keywords>
<keywords scheme="Teeft" xml:lang="en"><term>Anomaly</term>
<term>Conductive</term>
<term>Conductive zones</term>
<term>Crystalline</term>
<term>Crystalline basement</term>
<term>Fracture</term>
<term>Fracture zones</term>
<term>Geoelectrical</term>
<term>Geophysical</term>
<term>Geophysical methods</term>
<term>Geophysical study</term>
<term>Geotermica italiana</term>
<term>Geotest</term>
<term>Geotest hellas</term>
<term>Geothermal</term>
<term>Geothermal fields</term>
<term>Gravity modelling</term>
<term>Gravity models</term>
<term>Ground surface</term>
<term>Hellas</term>
<term>High conductivity zones</term>
<term>Igme</term>
<term>Lesvos</term>
<term>Lesvos island</term>
<term>Peridotitic body</term>
<term>Polyhnitos</term>
<term>Polyhnitos area</term>
<term>Target areas</term>
<term>Tectonic features</term>
<term>Thanassoulas</term>
<term>Xanthopoulos</term>
</keywords>
</textClass>
<langUsage><language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">Abstract: In 1988, Geotest Hellas carried out a geophysical survey on Lesvos island using gravity, vertical electrical soundings and self-potential methods in order to study the geothermal potential of the island. This paper is based on the primary results presented by Geotest Hellas, which were re-examined and presented in a different form to facilitate the selection of the areas of strong geothermal interest. In particular, application of the gravity, vertical electrical sounding (VES) and self-potential (SP) methods has provided information on the geophysical structure of the geothermal target areas of Lesvos island. The gravity survey provided valuable information on the morphology and tectonics of the crystalline basement (and on the peridotitic body and pyroclastic sediments), for the study of the geothermal potential of the area. The electrical survey provided information on the highly conductive zones (usually associated with geothermal fields), the electrical stratigraphy and the tectonics of the main geological units of the target area. The SP survey mapped areas where electrical polarization is observed in the faulting system. An integrated interpretation of the results of all these surveys led to the selection of five target areas considered to be of high geothermal potential. The location of these target areas is shown in Fig. 14, ranked from 1 to 5 in decreasing order of priority.</div>
</front>
</TEI>
<istex><corpusName>elsevier</corpusName>
<keywords><teeft><json:string>lesvos</json:string>
<json:string>crystalline basement</json:string>
<json:string>lesvos island</json:string>
<json:string>geothermal</json:string>
<json:string>geophysical</json:string>
<json:string>igme</json:string>
<json:string>hellas</json:string>
<json:string>geotest hellas</json:string>
<json:string>geotest</json:string>
<json:string>fracture zones</json:string>
<json:string>conductive</json:string>
<json:string>thanassoulas</json:string>
<json:string>geoelectrical</json:string>
<json:string>xanthopoulos</json:string>
<json:string>fracture</json:string>
<json:string>conductive zones</json:string>
<json:string>polyhnitos</json:string>
<json:string>geophysical methods</json:string>
<json:string>ground surface</json:string>
<json:string>high conductivity zones</json:string>
<json:string>geothermal fields</json:string>
<json:string>target areas</json:string>
<json:string>crystalline</json:string>
<json:string>anomaly</json:string>
<json:string>geophysical study</json:string>
<json:string>polyhnitos area</json:string>
<json:string>peridotitic body</json:string>
<json:string>gravity modelling</json:string>
<json:string>gravity models</json:string>
<json:string>tectonic features</json:string>
<json:string>geotermica italiana</json:string>
</teeft>
</keywords>
<author><json:item><name>C. Thanassoulas</name>
<affiliations><json:string>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</json:string>
</affiliations>
</json:item>
<json:item><name>N. Xanthopoulos</name>
<affiliations><json:string>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</json:string>
</affiliations>
</json:item>
</author>
<language><json:string>eng</json:string>
</language>
<originalGenre><json:string>Full-length article</json:string>
</originalGenre>
<abstract>In 1988, Geotest Hellas carried out a geophysical survey on Lesvos island using gravity, vertical electrical soundings and self-potential methods in order to study the geothermal potential of the island. This paper is based on the primary results presented by Geotest Hellas, which were re-examined and presented in a different form to facilitate the selection of the areas of strong geothermal interest. In particular, application of the gravity, vertical electrical sounding (VES) and self-potential (SP) methods has provided information on the geophysical structure of the geothermal target areas of Lesvos island. The gravity survey provided valuable information on the morphology and tectonics of the crystalline basement (and on the peridotitic body and pyroclastic sediments), for the study of the geothermal potential of the area. The electrical survey provided information on the highly conductive zones (usually associated with geothermal fields), the electrical stratigraphy and the tectonics of the main geological units of the target area. The SP survey mapped areas where electrical polarization is observed in the faulting system. An integrated interpretation of the results of all these surveys led to the selection of five target areas considered to be of high geothermal potential. The location of these target areas is shown in Fig. 14, ranked from 1 to 5 in decreasing order of priority.</abstract>
<qualityIndicators><score>6.216</score>
<pdfVersion>1.2</pdfVersion>
<pdfPageSize>540 x 720 pts</pdfPageSize>
<refBibsNative>true</refBibsNative>
<keywordCount>0</keywordCount>
<abstractCharCount>1407</abstractCharCount>
<pdfWordCount>3648</pdfWordCount>
<pdfCharCount>19440</pdfCharCount>
<pdfPageCount>14</pdfPageCount>
<abstractWordCount>214</abstractWordCount>
</qualityIndicators>
<title>Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece</title>
<pii><json:string>0375-6505(91)90026-R</json:string>
</pii>
<genre><json:string>research-article</json:string>
</genre>
<host><title>Geothermics</title>
<language><json:string>unknown</json:string>
</language>
<publicationDate>1991</publicationDate>
<issn><json:string>0375-6505</json:string>
</issn>
<pii><json:string>S0375-6505(00)X0074-0</json:string>
</pii>
<volume>20</volume>
<issue>5–6</issue>
<pages><first>355</first>
<last>368</last>
</pages>
<genre><json:string>journal</json:string>
</genre>
</host>
<categories><wos><json:string>science</json:string>
<json:string>geosciences, multidisciplinary</json:string>
<json:string>energy & fuels</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>1991</publicationDate>
<copyrightDate>1991</copyrightDate>
<doi><json:string>10.1016/0375-6505(91)90026-R</json:string>
</doi>
<id>A343123EA16384E91CECBDD0112F1A9A2E676180</id>
<score>1</score>
<fulltext><json:item><extension>pdf</extension>
<original>true</original>
<mimetype>application/pdf</mimetype>
<uri>https://api.istex.fr/document/A343123EA16384E91CECBDD0112F1A9A2E676180/fulltext/pdf</uri>
</json:item>
<json:item><extension>zip</extension>
<original>false</original>
<mimetype>application/zip</mimetype>
<uri>https://api.istex.fr/document/A343123EA16384E91CECBDD0112F1A9A2E676180/fulltext/zip</uri>
</json:item>
<istex:fulltextTEI uri="https://api.istex.fr/document/A343123EA16384E91CECBDD0112F1A9A2E676180/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a">Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece</title>
</titleStmt>
<publicationStmt><authority>ISTEX</authority>
<publisher>ELSEVIER</publisher>
<availability><p>ELSEVIER</p>
</availability>
<date>1991</date>
</publicationStmt>
<sourceDesc><biblStruct type="inbook"><analytic><title level="a">Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece</title>
<author xml:id="author-0000"><persName><forename type="first">C.</forename>
<surname>Thanassoulas</surname>
</persName>
<affiliation>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</affiliation>
</author>
<author xml:id="author-0001"><persName><forename type="first">N.</forename>
<surname>Xanthopoulos</surname>
</persName>
<affiliation>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</affiliation>
</author>
<idno type="istex">A343123EA16384E91CECBDD0112F1A9A2E676180</idno>
<idno type="DOI">10.1016/0375-6505(91)90026-R</idno>
<idno type="PII">0375-6505(91)90026-R</idno>
</analytic>
<monogr><title level="j">Geothermics</title>
<title level="j" type="abbrev">GEOT</title>
<idno type="pISSN">0375-6505</idno>
<idno type="PII">S0375-6505(00)X0074-0</idno>
<imprint><publisher>ELSEVIER</publisher>
<date type="published" when="1991"></date>
<biblScope unit="volume">20</biblScope>
<biblScope unit="issue">5–6</biblScope>
<biblScope unit="page" from="355">355</biblScope>
<biblScope unit="page" to="368">368</biblScope>
</imprint>
</monogr>
</biblStruct>
</sourceDesc>
</fileDesc>
<profileDesc><creation><date>1991</date>
</creation>
<langUsage><language ident="en">en</language>
</langUsage>
<abstract xml:lang="en"><p>In 1988, Geotest Hellas carried out a geophysical survey on Lesvos island using gravity, vertical electrical soundings and self-potential methods in order to study the geothermal potential of the island. This paper is based on the primary results presented by Geotest Hellas, which were re-examined and presented in a different form to facilitate the selection of the areas of strong geothermal interest. In particular, application of the gravity, vertical electrical sounding (VES) and self-potential (SP) methods has provided information on the geophysical structure of the geothermal target areas of Lesvos island. The gravity survey provided valuable information on the morphology and tectonics of the crystalline basement (and on the peridotitic body and pyroclastic sediments), for the study of the geothermal potential of the area. The electrical survey provided information on the highly conductive zones (usually associated with geothermal fields), the electrical stratigraphy and the tectonics of the main geological units of the target area. The SP survey mapped areas where electrical polarization is observed in the faulting system. An integrated interpretation of the results of all these surveys led to the selection of five target areas considered to be of high geothermal potential. The location of these target areas is shown in Fig. 14, ranked from 1 to 5 in decreasing order of priority.</p>
</abstract>
</profileDesc>
<revisionDesc><change when="1991">Published</change>
</revisionDesc>
</teiHeader>
</istex:fulltextTEI>
<json:item><extension>txt</extension>
<original>false</original>
<mimetype>text/plain</mimetype>
<uri>https://api.istex.fr/document/A343123EA16384E91CECBDD0112F1A9A2E676180/fulltext/txt</uri>
</json:item>
</fulltext>
<metadata><istex:metadataXml wicri:clean="Elsevier, elements deleted: tail"><istex:xmlDeclaration>version="1.0" encoding="utf-8"</istex:xmlDeclaration>
<istex:docType PUBLIC="-//ES//DTD journal article DTD version 4.5.2//EN//XML" URI="art452.dtd" name="istex:docType"></istex:docType>
<istex:document><converted-article version="4.5.2" docsubtype="fla"><item-info><jid>GEOT</jid>
<aid>9190026R</aid>
<ce:pii>0375-6505(91)90026-R</ce:pii>
<ce:doi>10.1016/0375-6505(91)90026-R</ce:doi>
<ce:copyright type="unknown" year="1991"></ce:copyright>
</item-info>
<head><ce:title>Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece</ce:title>
<ce:author-group><ce:author><ce:given-name>C.</ce:given-name>
<ce:surname>Thanassoulas</ce:surname>
</ce:author>
<ce:author><ce:given-name>N.</ce:given-name>
<ce:surname>Xanthopoulos</ce:surname>
</ce:author>
<ce:affiliation><ce:textfn>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</ce:textfn>
</ce:affiliation>
</ce:author-group>
<ce:abstract><ce:section-title>Abstract</ce:section-title>
<ce:abstract-sec><ce:simple-para>In 1988, Geotest Hellas carried out a geophysical survey on Lesvos island using gravity, vertical electrical soundings and self-potential methods in order to study the geothermal potential of the island. This paper is based on the primary results presented by Geotest Hellas, which were re-examined and presented in a different form to facilitate the selection of the areas of strong geothermal interest. In particular, application of the gravity, vertical electrical sounding (VES) and self-potential (SP) methods has provided information on the geophysical structure of the geothermal target areas of Lesvos island. The gravity survey provided valuable information on the morphology and tectonics of the crystalline basement (and on the peridotitic body and pyroclastic sediments), for the study of the geothermal potential of the area. The electrical survey provided information on the highly conductive zones (usually associated with geothermal fields), the electrical stratigraphy and the tectonics of the main geological units of the target area. The SP survey mapped areas where electrical polarization is observed in the faulting system. An integrated interpretation of the results of all these surveys led to the selection of five target areas considered to be of high geothermal potential. The location of these target areas is shown in Fig. 14, ranked from 1 to 5 in decreasing order of priority.</ce:simple-para>
</ce:abstract-sec>
</ce:abstract>
</head>
</converted-article>
</istex:document>
</istex:metadataXml>
<mods version="3.6"><titleInfo><title>Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece</title>
</titleInfo>
<titleInfo type="alternative" contentType="CDATA"><title>Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece</title>
</titleInfo>
<name type="personal"><namePart type="given">C.</namePart>
<namePart type="family">Thanassoulas</namePart>
<affiliation>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</affiliation>
<role><roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal"><namePart type="given">N.</namePart>
<namePart type="family">Xanthopoulos</namePart>
<affiliation>Institute of Geology and Mineral Exploration (IGME), Department of Geophysical Research, 70 Messoghion Avenue, Athens, 115-26, Greece</affiliation>
<role><roleTerm type="text">author</roleTerm>
</role>
</name>
<typeOfResource>text</typeOfResource>
<genre type="research-article" displayLabel="Full-length article" authority="ISTEX" authorityURI="https://content-type.data.istex.fr" valueURI="https://content-type.data.istex.fr/ark:/67375/XTP-1JC4F85T-7">research-article</genre>
<originInfo><publisher>ELSEVIER</publisher>
<dateIssued encoding="w3cdtf">1991</dateIssued>
<copyrightDate encoding="w3cdtf">1991</copyrightDate>
</originInfo>
<language><languageTerm type="code" authority="iso639-2b">eng</languageTerm>
<languageTerm type="code" authority="rfc3066">en</languageTerm>
</language>
<abstract lang="en">Abstract: In 1988, Geotest Hellas carried out a geophysical survey on Lesvos island using gravity, vertical electrical soundings and self-potential methods in order to study the geothermal potential of the island. This paper is based on the primary results presented by Geotest Hellas, which were re-examined and presented in a different form to facilitate the selection of the areas of strong geothermal interest. In particular, application of the gravity, vertical electrical sounding (VES) and self-potential (SP) methods has provided information on the geophysical structure of the geothermal target areas of Lesvos island. The gravity survey provided valuable information on the morphology and tectonics of the crystalline basement (and on the peridotitic body and pyroclastic sediments), for the study of the geothermal potential of the area. The electrical survey provided information on the highly conductive zones (usually associated with geothermal fields), the electrical stratigraphy and the tectonics of the main geological units of the target area. The SP survey mapped areas where electrical polarization is observed in the faulting system. An integrated interpretation of the results of all these surveys led to the selection of five target areas considered to be of high geothermal potential. The location of these target areas is shown in Fig. 14, ranked from 1 to 5 in decreasing order of priority.</abstract>
<relatedItem type="host"><titleInfo><title>Geothermics</title>
</titleInfo>
<titleInfo type="abbreviated"><title>GEOT</title>
</titleInfo>
<genre type="journal" authority="ISTEX" authorityURI="https://publication-type.data.istex.fr" valueURI="https://publication-type.data.istex.fr/ark:/67375/JMC-0GLKJH51-B">journal</genre>
<originInfo><publisher>ELSEVIER</publisher>
<dateIssued encoding="w3cdtf">1991</dateIssued>
</originInfo>
<identifier type="ISSN">0375-6505</identifier>
<identifier type="PII">S0375-6505(00)X0074-0</identifier>
<part><date>1991</date>
<detail type="volume"><number>20</number>
<caption>vol.</caption>
</detail>
<detail type="issue"><number>5–6</number>
<caption>no.</caption>
</detail>
<extent unit="issue-pages"><start>257</start>
<end>409</end>
</extent>
<extent unit="pages"><start>355</start>
<end>368</end>
</extent>
</part>
</relatedItem>
<identifier type="istex">A343123EA16384E91CECBDD0112F1A9A2E676180</identifier>
<identifier type="ark">ark:/67375/6H6-X3MMR3B3-Z</identifier>
<identifier type="DOI">10.1016/0375-6505(91)90026-R</identifier>
<identifier type="PII">0375-6505(91)90026-R</identifier>
<recordInfo><recordContentSource authority="ISTEX" authorityURI="https://loaded-corpus.data.istex.fr" valueURI="https://loaded-corpus.data.istex.fr/ark:/67375/XBH-HKKZVM7B-M">elsevier</recordContentSource>
</recordInfo>
</mods>
<json:item><extension>json</extension>
<original>false</original>
<mimetype>application/json</mimetype>
<uri>https://api.istex.fr/document/A343123EA16384E91CECBDD0112F1A9A2E676180/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 000363 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 000363 | 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:A343123EA16384E91CECBDD0112F1A9A2E676180 |texte= Location of possibly productive geothermal fracture zones/faults using integrated geophysicals methods over lesvos island geothermal field, Greece }}
![]() | This area was generated with Dilib version V0.6.33. | ![]() |