D
Identifieur interne : 007691 ( Istex/Corpus ); précédent : 007690; suivant : 007692D
Auteurs : Douglas M. Considine ; Glenn D. ConsidineSource :
Abstract
Abstract: The name of a somewhat variable group of extrusive igneous rocks similar to the rhyolites but richer in plagioclase feldspar. Typical dacites are felsitic to porphyritic in texture. Dacites are the extrusive equivalents of the quartz-rich varieties of diorites and are sometimes classified as quartz-bearing andesites. The porphyritic types usually occur toward the center of the thicker dacite flows, dikes and sills, as well as the marginal zones of laccoliths. Dacites are common in the Cordilleran province of North, Central and South America. The term, dacite, was proposed by G. Stache of Austria for lavas in the old Roman province of Dacia.
Url:
DOI: 10.1007/978-1-4757-6918-0_4
Links to Exploration step
ISTEX:F000820994ED13D235EC80CD85AEA5CD7D03AFA7Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">D</title>
<author><name sortKey="Considine, Douglas M" sort="Considine, Douglas M" uniqKey="Considine D" first="Douglas M." last="Considine">Douglas M. Considine</name>
</author>
<author><name sortKey="Considine, Glenn D" sort="Considine, Glenn D" uniqKey="Considine G" first="Glenn D." last="Considine">Glenn D. Considine</name>
</author>
</titleStmt>
<publicationStmt><idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:F000820994ED13D235EC80CD85AEA5CD7D03AFA7</idno>
<date when="1995" year="1995">1995</date>
<idno type="doi">10.1007/978-1-4757-6918-0_4</idno>
<idno type="url">https://api.istex.fr/document/F000820994ED13D235EC80CD85AEA5CD7D03AFA7/fulltext/pdf</idno>
<idno type="wicri:Area/Istex/Corpus">007691</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">007691</idno>
</publicationStmt>
<sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">D</title>
<author><name sortKey="Considine, Douglas M" sort="Considine, Douglas M" uniqKey="Considine D" first="Douglas M." last="Considine">Douglas M. Considine</name>
</author>
<author><name sortKey="Considine, Glenn D" sort="Considine, Glenn D" uniqKey="Considine G" first="Glenn D." last="Considine">Glenn D. Considine</name>
</author>
</analytic>
<monogr></monogr>
</biblStruct>
</sourceDesc>
</fileDesc>
<profileDesc><textClass></textClass>
<langUsage><language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">Abstract: The name of a somewhat variable group of extrusive igneous rocks similar to the rhyolites but richer in plagioclase feldspar. Typical dacites are felsitic to porphyritic in texture. Dacites are the extrusive equivalents of the quartz-rich varieties of diorites and are sometimes classified as quartz-bearing andesites. The porphyritic types usually occur toward the center of the thicker dacite flows, dikes and sills, as well as the marginal zones of laccoliths. Dacites are common in the Cordilleran province of North, Central and South America. The term, dacite, was proposed by G. Stache of Austria for lavas in the old Roman province of Dacia.</div>
</front>
</TEI>
<istex><corpusName>springer-ebooks</corpusName>
<editor><json:item><name>Douglas M. Considine P.E.</name>
</json:item>
<json:item><name>Glenn D. Considine</name>
</json:item>
</editor>
<author><json:item><name>Douglas M. Considine P.E.</name>
</json:item>
<json:item><name>Glenn D. Considine</name>
</json:item>
</author>
<arkIstex>ark:/67375/HCB-TXW3RTTB-C</arkIstex>
<language><json:string>eng</json:string>
</language>
<originalGenre><json:string>chapter</json:string>
</originalGenre>
<abstract>Abstract: The name of a somewhat variable group of extrusive igneous rocks similar to the rhyolites but richer in plagioclase feldspar. Typical dacites are felsitic to porphyritic in texture. Dacites are the extrusive equivalents of the quartz-rich varieties of diorites and are sometimes classified as quartz-bearing andesites. The porphyritic types usually occur toward the center of the thicker dacite flows, dikes and sills, as well as the marginal zones of laccoliths. Dacites are common in the Cordilleran province of North, Central and South America. The term, dacite, was proposed by G. Stache of Austria for lavas in the old Roman province of Dacia.</abstract>
<qualityIndicators><refBibsNative>false</refBibsNative>
<abstractWordCount>103</abstractWordCount>
<abstractCharCount>658</abstractCharCount>
<keywordCount>0</keywordCount>
<score>8.236</score>
<pdfWordCount>130273</pdfWordCount>
<pdfCharCount>760882</pdfCharCount>
<pdfVersion>1.4</pdfVersion>
<pdfPageCount>127</pdfPageCount>
<pdfPageSize>637.795 x 822.047 pts</pdfPageSize>
</qualityIndicators>
<title>D</title>
<chapterId><json:string>4</json:string>
<json:string>Chap4</json:string>
</chapterId>
<genre><json:string>chapter</json:string>
</genre>
<host><title>Van Nostrand’s Scientific Encyclopedia</title>
<language><json:string>unknown</json:string>
</language>
<copyrightDate>1995</copyrightDate>
<doi><json:string>10.1007/978-1-4757-6918-0</json:string>
</doi>
<eisbn><json:string>978-1-4757-6918-0</json:string>
</eisbn>
<bookId><json:string>978-1-4757-6918-0</json:string>
</bookId>
<isbn><json:string>978-1-4757-6920-3</json:string>
</isbn>
<pages><first>887</first>
<last>1013</last>
</pages>
<genre><json:string>book</json:string>
</genre>
<editor><json:item><name>Douglas M. Considine P.E.</name>
</json:item>
<json:item><name>Glenn D. Considine</name>
</json:item>
</editor>
<subject><json:item><value>Engineering</value>
</json:item>
<json:item><value>Engineering</value>
</json:item>
<json:item><value>Engineering, general</value>
</json:item>
</subject>
</host>
<ark><json:string>ark:/67375/HCB-TXW3RTTB-C</json:string>
</ark>
<publicationDate>1995</publicationDate>
<copyrightDate>1995</copyrightDate>
<doi><json:string>10.1007/978-1-4757-6918-0_4</json:string>
</doi>
<id>F000820994ED13D235EC80CD85AEA5CD7D03AFA7</id>
<score>1</score>
<fulltext><json:item><extension>pdf</extension>
<original>true</original>
<mimetype>application/pdf</mimetype>
<uri>https://api.istex.fr/document/F000820994ED13D235EC80CD85AEA5CD7D03AFA7/fulltext/pdf</uri>
</json:item>
<json:item><extension>zip</extension>
<original>false</original>
<mimetype>application/zip</mimetype>
<uri>https://api.istex.fr/document/F000820994ED13D235EC80CD85AEA5CD7D03AFA7/fulltext/zip</uri>
</json:item>
<istex:fulltextTEI uri="https://api.istex.fr/document/F000820994ED13D235EC80CD85AEA5CD7D03AFA7/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">D</title>
<respStmt><resp>Références bibliographiques récupérées via GROBID</resp>
<name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name>
</respStmt>
</titleStmt>
<publicationStmt><authority>ISTEX</authority>
<publisher scheme="https://publisher-list.data.istex.fr">Springer US</publisher>
<pubPlace>Boston, MA</pubPlace>
<availability><licence><p>Springer-Verlag US, 1995</p>
</licence>
<p scheme="https://loaded-corpus.data.istex.fr/ark:/67375/XBH-3XSW68JL-F">springer</p>
</availability>
<date>1995</date>
</publicationStmt>
<notesStmt><note type="chapter" scheme="https://content-type.data.istex.fr/ark:/67375/XTP-CGT4WMJM-6">chapter</note>
<note type="book" scheme="https://publication-type.data.istex.fr/ark:/67375/JMC-5WTPMB5N-F">book</note>
</notesStmt>
<sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">D</title>
<author xml:id="author-0000"><persName><forename type="first">Douglas</forename>
<surname>Considine</surname>
</persName>
<roleName type="degree">P.E.</roleName>
</author>
<author xml:id="author-0001"><persName><forename type="first">Glenn</forename>
<surname>Considine</surname>
</persName>
</author>
<editor xml:id="author-0002"><persName><forename type="first">Douglas</forename>
<forename type="first">M.</forename>
<surname>Considine</surname>
<roleName type="degree">P.E.</roleName>
</persName>
</editor>
<editor xml:id="author-0003"><persName><forename type="first">Glenn</forename>
<forename type="first">D.</forename>
<surname>Considine</surname>
</persName>
</editor>
<idno type="istex">F000820994ED13D235EC80CD85AEA5CD7D03AFA7</idno>
<idno type="ark">ark:/67375/HCB-TXW3RTTB-C</idno>
<idno type="DOI">10.1007/978-1-4757-6918-0_4</idno>
<idno type="ChapterID">4</idno>
<idno type="ChapterID">Chap4</idno>
</analytic>
<monogr><title level="m">Van Nostrand’s Scientific Encyclopedia</title>
<idno type="DOI">10.1007/978-1-4757-6918-0</idno>
<idno type="pISBN">978-1-4757-6920-3</idno>
<idno type="eISBN">978-1-4757-6918-0</idno>
<idno type="book-title-id">113421</idno>
<idno type="book-id">978-1-4757-6918-0</idno>
<idno type="book-chapter-count">26</idno>
<editor xml:id="book-author-0000"><persName><forename type="first">Douglas</forename>
<forename type="first">M.</forename>
<surname>Considine</surname>
<roleName type="degree">P.E.</roleName>
</persName>
</editor>
<editor xml:id="book-author-0001"><persName><forename type="first">Glenn</forename>
<forename type="first">D.</forename>
<surname>Considine</surname>
</persName>
</editor>
<imprint><publisher>Springer US</publisher>
<pubPlace>Boston, MA</pubPlace>
<date type="published" when="1995"></date>
<biblScope unit="page" from="887">887</biblScope>
<biblScope unit="page" to="1013">1013</biblScope>
</imprint>
</monogr>
</biblStruct>
</sourceDesc>
</fileDesc>
<profileDesc><creation><date>1995</date>
</creation>
<langUsage><language ident="en">en</language>
</langUsage>
<abstract xml:lang="en"><p>Abstract: The name of a somewhat variable group of extrusive igneous rocks similar to the rhyolites but richer in plagioclase feldspar. Typical dacites are felsitic to porphyritic in texture. Dacites are the extrusive equivalents of the quartz-rich varieties of diorites and are sometimes classified as quartz-bearing andesites. The porphyritic types usually occur toward the center of the thicker dacite flows, dikes and sills, as well as the marginal zones of laccoliths. Dacites are common in the Cordilleran province of North, Central and South America. The term, dacite, was proposed by G. Stache of Austria for lavas in the old Roman province of Dacia.</p>
</abstract>
<textClass><keywords scheme="Book-Subject-Collection"><list><label>SUCO11647</label>
<item><term>Engineering</term>
</item>
</list>
</keywords>
</textClass>
<textClass><keywords scheme="Book-Subject-Group"><list><label>SCT</label>
<label>SCT00004</label>
<item><term>Engineering</term>
</item>
<item><term>Engineering, general</term>
</item>
</list>
</keywords>
</textClass>
</profileDesc>
<revisionDesc><change when="1995">Published</change>
<change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-11-28">References added</change>
</revisionDesc>
</teiHeader>
</istex:fulltextTEI>
<json:item><extension>txt</extension>
<original>false</original>
<mimetype>text/plain</mimetype>
<uri>https://api.istex.fr/document/F000820994ED13D235EC80CD85AEA5CD7D03AFA7/fulltext/txt</uri>
</json:item>
</fulltext>
<metadata><istex:metadataXml wicri:clean="corpus springer-ebooks not found" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0" encoding="UTF-8"</istex:xmlDeclaration>
<istex:docType PUBLIC="-//Springer-Verlag//DTD A++ V2.4//EN" URI="http://devel.springer.de/A++/V2.4/DTD/A++V2.4.dtd" name="istex:docType"></istex:docType>
<istex:document><Publisher><PublisherInfo><PublisherName>Springer US</PublisherName>
<PublisherLocation>Boston, MA</PublisherLocation>
<PublisherImprintName>Springer</PublisherImprintName>
</PublisherInfo>
<Book Language="En"><BookInfo BookProductType="Monograph" ContainsESM="No" Language="En" MediaType="eBook" NumberingStyle="Unnumbered" OutputMedium="All" TocLevels="0"><BookID>978-1-4757-6918-0</BookID>
<BookTitle>Van Nostrand’s Scientific Encyclopedia</BookTitle>
<BookDOI>10.1007/978-1-4757-6918-0</BookDOI>
<BookTitleID>113421</BookTitleID>
<BookPrintISBN>978-1-4757-6920-3</BookPrintISBN>
<BookElectronicISBN>978-1-4757-6918-0</BookElectronicISBN>
<EditionNumber>8</EditionNumber>
<BookEdition>Eighth Edition</BookEdition>
<BookMultiVolumeCount>6</BookMultiVolumeCount>
<BookChapterCount>26</BookChapterCount>
<BookCopyright><CopyrightHolderName>Springer-Verlag US</CopyrightHolderName>
<CopyrightYear>1995</CopyrightYear>
</BookCopyright>
<BookSubjectGroup><BookSubject Code="SCT" Type="Primary">Engineering</BookSubject>
<BookSubject Code="SCT00004" Priority="1" Type="Secondary">Engineering, general</BookSubject>
<SubjectCollection Code="SUCO11647">Engineering</SubjectCollection>
</BookSubjectGroup>
</BookInfo>
<BookHeader><EditorGroup><Editor><EditorName DisplayOrder="Western"><GivenName>Douglas</GivenName>
<GivenName>M.</GivenName>
<FamilyName>Considine</FamilyName>
<Degrees>P.E.</Degrees>
</EditorName>
</Editor>
<Editor><EditorName DisplayOrder="Western"><GivenName>Glenn</GivenName>
<GivenName>D.</GivenName>
<FamilyName>Considine</FamilyName>
</EditorName>
</Editor>
</EditorGroup>
</BookHeader>
<Chapter ID="Chap4" Language="En"><ChapterInfo ChapterType="OriginalPaper" ContainsESM="No" Language="En" NumberingStyle="Unnumbered" OutputMedium="All" TocLevels="0"><ChapterID>4</ChapterID>
<ChapterDOI>10.1007/978-1-4757-6918-0_4</ChapterDOI>
<ChapterSequenceNumber>4</ChapterSequenceNumber>
<ChapterTitle Language="En">D</ChapterTitle>
<ChapterFirstPage>887</ChapterFirstPage>
<ChapterLastPage>1013</ChapterLastPage>
<ChapterCopyright><CopyrightHolderName>Springer Science+Business Media New York</CopyrightHolderName>
<CopyrightYear>1995</CopyrightYear>
</ChapterCopyright>
<ChapterHistory><RegistrationDate><Year>2013</Year>
<Month>3</Month>
<Day>18</Day>
</RegistrationDate>
</ChapterHistory>
<ChapterGrants Type="Regular"><MetadataGrant Grant="OpenAccess"></MetadataGrant>
<AbstractGrant Grant="OpenAccess"></AbstractGrant>
<BodyPDFGrant Grant="Restricted"></BodyPDFGrant>
<BodyHTMLGrant Grant="Restricted"></BodyHTMLGrant>
<BibliographyGrant Grant="Restricted"></BibliographyGrant>
<ESMGrant Grant="Restricted"></ESMGrant>
</ChapterGrants>
<ChapterContext><BookID>978-1-4757-6918-0</BookID>
<BookTitle>Van Nostrand’s Scientific Encyclopedia</BookTitle>
</ChapterContext>
</ChapterInfo>
<ChapterHeader><AuthorGroup><Author><AuthorName DisplayOrder="Western"><GivenName>Douglas</GivenName>
<GivenName>M.</GivenName>
<FamilyName>Considine</FamilyName>
<Degrees>P.E.</Degrees>
</AuthorName>
</Author>
<Author><AuthorName DisplayOrder="Western"><GivenName>Glenn</GivenName>
<GivenName>D.</GivenName>
<FamilyName>Considine</FamilyName>
</AuthorName>
</Author>
</AuthorGroup>
<Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading>
<Para>The name of a somewhat variable group of extrusive igneous rocks similar to the rhyolites but richer in plagioclase feldspar. Typical dacites are felsitic to porphyritic in texture. Dacites are the extrusive equivalents of the quartz-rich varieties of diorites and are sometimes classified as quartz-bearing andesites. The porphyritic types usually occur toward the center of the thicker dacite flows, dikes and sills, as well as the marginal zones of laccoliths. Dacites are common in the Cordilleran province of North, Central and South America. The term, dacite, was proposed by G. Stache of Austria for lavas in the old Roman province of Dacia.</Para>
</Abstract>
</ChapterHeader>
<NoBody></NoBody>
</Chapter>
</Book>
</Publisher>
</istex:document>
</istex:metadataXml>
<mods version="3.6"><titleInfo lang="en"><title>D</title>
</titleInfo>
<titleInfo type="alternative" contentType="CDATA" lang="en"><title>D</title>
</titleInfo>
<name type="personal"><namePart type="given">Douglas</namePart>
<namePart type="given">M.</namePart>
<namePart type="family">Considine</namePart>
<namePart type="termsOfAddress">P.E.</namePart>
<role><roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal"><namePart type="given">Glenn</namePart>
<namePart type="given">D.</namePart>
<namePart type="family">Considine</namePart>
<role><roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal"><namePart type="given">Douglas</namePart>
<namePart type="given">M.</namePart>
<namePart type="family">Considine</namePart>
<namePart type="termsOfAddress">P.E.</namePart>
<role><roleTerm type="text">editor</roleTerm>
</role>
</name>
<name type="personal"><namePart type="given">Glenn</namePart>
<namePart type="given">D.</namePart>
<namePart type="family">Considine</namePart>
<role><roleTerm type="text">editor</roleTerm>
</role>
</name>
<typeOfResource>text</typeOfResource>
<genre type="chapter" displayLabel="chapter" authority="ISTEX" authorityURI="https://content-type.data.istex.fr" valueURI="https://content-type.data.istex.fr/ark:/67375/XTP-CGT4WMJM-6"></genre>
<originInfo><publisher>Springer US</publisher>
<place><placeTerm type="text">Boston, MA</placeTerm>
</place>
<dateIssued encoding="w3cdtf">1995</dateIssued>
<dateIssued encoding="w3cdtf">1995</dateIssued>
<copyrightDate encoding="w3cdtf">1995</copyrightDate>
</originInfo>
<language><languageTerm type="code" authority="rfc3066">en</languageTerm>
<languageTerm type="code" authority="iso639-2b">eng</languageTerm>
</language>
<abstract lang="en">Abstract: The name of a somewhat variable group of extrusive igneous rocks similar to the rhyolites but richer in plagioclase feldspar. Typical dacites are felsitic to porphyritic in texture. Dacites are the extrusive equivalents of the quartz-rich varieties of diorites and are sometimes classified as quartz-bearing andesites. The porphyritic types usually occur toward the center of the thicker dacite flows, dikes and sills, as well as the marginal zones of laccoliths. Dacites are common in the Cordilleran province of North, Central and South America. The term, dacite, was proposed by G. Stache of Austria for lavas in the old Roman province of Dacia.</abstract>
<relatedItem type="host"><titleInfo><title>Van Nostrand’s Scientific Encyclopedia</title>
</titleInfo>
<name type="personal"><namePart type="given">Douglas</namePart>
<namePart type="given">M.</namePart>
<namePart type="family">Considine</namePart>
<namePart type="termsOfAddress">P.E.</namePart>
<role><roleTerm type="text">editor</roleTerm>
</role>
</name>
<name type="personal"><namePart type="given">Glenn</namePart>
<namePart type="given">D.</namePart>
<namePart type="family">Considine</namePart>
<role><roleTerm type="text">editor</roleTerm>
</role>
</name>
<genre type="book" displayLabel="Monograph" authority="ISTEX" authorityURI="https://publication-type.data.istex.fr" valueURI="https://publication-type.data.istex.fr/ark:/67375/JMC-5WTPMB5N-F">book</genre>
<originInfo><publisher>Springer</publisher>
<copyrightDate encoding="w3cdtf">1995</copyrightDate>
<issuance>monographic</issuance>
<edition>Eighth Edition</edition>
</originInfo>
<subject><genre>Book-Subject-Collection</genre>
<topic authority="SpringerSubjectCodes" authorityURI="SUCO11647">Engineering</topic>
</subject>
<subject><genre>Book-Subject-Group</genre>
<topic authority="SpringerSubjectCodes" authorityURI="SCT">Engineering</topic>
<topic authority="SpringerSubjectCodes" authorityURI="SCT00004">Engineering, general</topic>
</subject>
<identifier type="DOI">10.1007/978-1-4757-6918-0</identifier>
<identifier type="ISBN">978-1-4757-6920-3</identifier>
<identifier type="eISBN">978-1-4757-6918-0</identifier>
<identifier type="BookTitleID">113421</identifier>
<identifier type="BookID">978-1-4757-6918-0</identifier>
<identifier type="BookChapterCount">26</identifier>
<part><date>1995</date>
<extent unit="pages"><start>887</start>
<end>1013</end>
</extent>
</part>
<recordInfo><recordOrigin>Springer-Verlag US, 1995</recordOrigin>
</recordInfo>
</relatedItem>
<identifier type="istex">F000820994ED13D235EC80CD85AEA5CD7D03AFA7</identifier>
<identifier type="ark">ark:/67375/HCB-TXW3RTTB-C</identifier>
<identifier type="DOI">10.1007/978-1-4757-6918-0_4</identifier>
<identifier type="ChapterID">4</identifier>
<identifier type="ChapterID">Chap4</identifier>
<accessCondition type="use and reproduction" contentType="copyright">Springer-Verlag US, 1995</accessCondition>
<recordInfo><recordContentSource authority="ISTEX" authorityURI="https://loaded-corpus.data.istex.fr" valueURI="https://loaded-corpus.data.istex.fr/ark:/67375/XBH-3XSW68JL-F">springer</recordContentSource>
<recordOrigin>Springer Science+Business Media New York, 1995</recordOrigin>
</recordInfo>
</mods>
<json:item><extension>json</extension>
<original>false</original>
<mimetype>application/json</mimetype>
<uri>https://api.istex.fr/document/F000820994ED13D235EC80CD85AEA5CD7D03AFA7/metadata/json</uri>
</json:item>
</metadata>
<annexes><json:item><extension>xml</extension>
<original>true</original>
<mimetype>application/xml</mimetype>
<uri>https://api.istex.fr/document/F000820994ED13D235EC80CD85AEA5CD7D03AFA7/annexes/xml</uri>
</json:item>
</annexes>
<serie></serie>
</istex>
</record>
Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Santé/explor/EdenteV2/Data/Istex/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 007691 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 007691 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien |wiki= Wicri/Santé |area= EdenteV2 |flux= Istex |étape= Corpus |type= RBID |clé= ISTEX:F000820994ED13D235EC80CD85AEA5CD7D03AFA7 |texte= D }}
![]() | This area was generated with Dilib version V0.6.32. | ![]() |