An Experimentally Constrained Petrogenetic Grid in the Silica-Saturated Portion of the System KFMASH at High Temperatures and Pressures
Identifieur interne : 001245 ( Istex/Corpus ); précédent : 001244; suivant : 001246An Experimentally Constrained Petrogenetic Grid in the Silica-Saturated Portion of the System KFMASH at High Temperatures and Pressures
Auteurs : Kaushik Das ; Somnath Dasgupta ; Hiroyuki MiuraSource :
- Journal of Petrology [ 0022-3530 ] ; 2003-06.
English descriptors
Abstract
Experiments in the quartz-saturated part of the system KFMASH under fO2 conditions of the haematite–magnetite buffer and using bulk compositions with XMg of 0·81, 0·72, 0·53 define the stability limits of several mineral assemblages within the P–T field 9–12 kbar, 850–1100°C. The stability limits of the mineral assemblages orthopyroxene + spinel + cordierite ± sapphirine, orthopyroxene + garnet + sapphirine, sapphirine + cordierite + orthopyroxene and garnet + orthopyroxene + spinel have been delineated on the basis of P–T and T–X pseudosections. Sapphirine did not appear in the bulk composition of XMg = 0·53. A partial petrogenetic grid applicable to high Mg–Al granulites metamorphosed at high fO2, developed in our earlier work, was extended to higher pressures. The experimental results were successfully applied to several high-grade terranes to estimate P–T conditions and retrograde P–T trajectories.
Url:
DOI: 10.1093/petrology/44.6.1055
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ISTEX:1023F93607ECA96C8607A1B0A896651AC6FE8A07Le document en format XML
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Fax: +81-11-706-4650.</mods:affiliation></affiliation><affiliation><mods:affiliation>E-mail: kaus@ep.sci.hokudai.ac.jp</mods:affiliation></affiliation></author><author><name sortKey="Dasgupta, Somnath" sort="Dasgupta, Somnath" uniqKey="Dasgupta S" first="Somnath" last="Dasgupta">Somnath Dasgupta</name><affiliation><mods:affiliation>DEPARTMENT OF GEOLOGICAL SCIENCES, JADAVPUR UNIVERSITY, KOLKATA, INDIA</mods:affiliation></affiliation></author><author><name sortKey="Miura, Hiroyuki" sort="Miura, Hiroyuki" uniqKey="Miura H" first="Hiroyuki" last="Miura">Hiroyuki Miura</name><affiliation><mods:affiliation>DIVISION OF EARTH AND PLANETARY SCIENCES, GRADUATE SCHOOL OF SCIENCE, HOKKAIDO UNIVERSITY, N10W8, KITA-KU, SAPPORO-SHI, JAPAN, 060-0810</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Petrology</title><title level="j" type="abbrev">J. Petrology</title><idno type="ISSN">0022-3530</idno><idno type="eISSN">1460-2415</idno><imprint><publisher>Oxford University Press</publisher><date type="published" when="2003-06">2003-06</date><biblScope unit="volume">44</biblScope><biblScope unit="issue">6</biblScope><biblScope unit="page" from="1055">1055</biblScope><biblScope unit="page" to="1075">1075</biblScope></imprint><idno type="ISSN">0022-3530</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0022-3530</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>KFMASH equilibria</term><term>experimental petrogenetic grid at high fO2</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Experiments in the quartz-saturated part of the system KFMASH under fO2 conditions of the haematite–magnetite buffer and using bulk compositions with XMg of 0·81, 0·72, 0·53 define the stability limits of several mineral assemblages within the P–T field 9–12 kbar, 850–1100°C. The stability limits of the mineral assemblages orthopyroxene + spinel + cordierite ± sapphirine, orthopyroxene + garnet + sapphirine, sapphirine + cordierite + orthopyroxene and garnet + orthopyroxene + spinel have been delineated on the basis of P–T and T–X pseudosections. Sapphirine did not appear in the bulk composition of XMg = 0·53. A partial petrogenetic grid applicable to high Mg–Al granulites metamorphosed at high fO2, developed in our earlier work, was extended to higher pressures. The experimental results were successfully applied to several high-grade terranes to estimate P–T conditions and retrograde P–T trajectories.</div></front></TEI><istex><corpusName>oup</corpusName><author><json:item><name>KAUSHIK DAS</name><affiliations><json:string>DIVISION OF EARTH AND PLANETARY SCIENCES, GRADUATE SCHOOL OF SCIENCE, HOKKAIDO UNIVERSITY, N10W8, KITA-KU, SAPPORO-SHI, JAPAN, 060-0810</json:string><json:string>Telephone: +81-11-706-4651. Fax: +81-11-706-4650.</json:string><json:string>E-mail: kaus@ep.sci.hokudai.ac.jp</json:string></affiliations></json:item><json:item><name>SOMNATH DASGUPTA</name><affiliations><json:string>DEPARTMENT OF GEOLOGICAL SCIENCES, JADAVPUR UNIVERSITY, KOLKATA, INDIA</json:string></affiliations></json:item><json:item><name>HIROYUKI MIURA</name><affiliations><json:string>DIVISION OF EARTH AND PLANETARY SCIENCES, GRADUATE SCHOOL OF SCIENCE, HOKKAIDO UNIVERSITY, N10W8, KITA-KU, SAPPORO-SHI, JAPAN, 060-0810</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>KFMASH equilibria</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>experimental petrogenetic grid at high fO2</value></json:item></subject><language><json:string>eng</json:string></language><originalGenre><json:string>research-article</json:string></originalGenre><abstract>Experiments in the quartz-saturated part of the system KFMASH under fO2 conditions of the haematite–magnetite buffer and using bulk compositions with XMg of 0·81, 0·72, 0·53 define the stability limits of several mineral assemblages within the P–T field 9–12 kbar, 850–1100°C. The stability limits of the mineral assemblages orthopyroxene + spinel + cordierite ± sapphirine, orthopyroxene + garnet + sapphirine, sapphirine + cordierite + orthopyroxene and garnet + orthopyroxene + spinel have been delineated on the basis of P–T and T–X pseudosections. Sapphirine did not appear in the bulk composition of XMg = 0·53. A partial petrogenetic grid applicable to high Mg–Al granulites metamorphosed at high fO2, developed in our earlier work, was extended to higher pressures. 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Fax: +81-11-706-4650. E-mail: kaus@ep.sci.hokudai.ac.jp</note></notesStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">An Experimentally Constrained Petrogenetic Grid in the Silica-Saturated Portion of the System KFMASH at High Temperatures and Pressures</title><author xml:id="author-0000"><persName><forename type="first">KAUSHIK</forename><surname>DAS</surname></persName><email>kaus@ep.sci.hokudai.ac.jp</email><affiliation>DIVISION OF EARTH AND PLANETARY SCIENCES, GRADUATE SCHOOL OF SCIENCE, HOKKAIDO UNIVERSITY, N10W8, KITA-KU, SAPPORO-SHI, JAPAN, 060-0810</affiliation><affiliation>Telephone: +81-11-706-4651. Fax: +81-11-706-4650.</affiliation></author><author xml:id="author-0001"><persName><forename type="first">SOMNATH</forename><surname>DASGUPTA</surname></persName><affiliation>DEPARTMENT OF GEOLOGICAL SCIENCES, JADAVPUR UNIVERSITY, KOLKATA, INDIA</affiliation></author><author xml:id="author-0002"><persName><forename type="first">HIROYUKI</forename><surname>MIURA</surname></persName><affiliation>DIVISION OF EARTH AND PLANETARY SCIENCES, GRADUATE SCHOOL OF SCIENCE, HOKKAIDO UNIVERSITY, N10W8, KITA-KU, SAPPORO-SHI, JAPAN, 060-0810</affiliation></author><idno type="istex">1023F93607ECA96C8607A1B0A896651AC6FE8A07</idno><idno type="DOI">10.1093/petrology/44.6.1055</idno><idno type="local">egg029</idno></analytic><monogr><title level="j">Journal of Petrology</title><title level="j" type="abbrev">J. Petrology</title><idno type="pISSN">0022-3530</idno><idno type="eISSN">1460-2415</idno><idno type="PublisherID">petroj</idno><idno type="PublisherID-hwp">petrology</idno><idno type="PublisherID-nlm-ta">J Petrology</idno><imprint><publisher>Oxford University Press</publisher><date type="published" when="2003-06"></date><biblScope unit="volume">44</biblScope><biblScope unit="issue">6</biblScope><biblScope unit="page" from="1055">1055</biblScope><biblScope unit="page" to="1075">1075</biblScope></imprint></monogr></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2003</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Experiments in the quartz-saturated part of the system KFMASH under fO2 conditions of the haematite–magnetite buffer and using bulk compositions with XMg of 0·81, 0·72, 0·53 define the stability limits of several mineral assemblages within the P–T field 9–12 kbar, 850–1100°C. The stability limits of the mineral assemblages orthopyroxene + spinel + cordierite ± sapphirine, orthopyroxene + garnet + sapphirine, sapphirine + cordierite + orthopyroxene and garnet + orthopyroxene + spinel have been delineated on the basis of P–T and T–X pseudosections. Sapphirine did not appear in the bulk composition of XMg = 0·53. A partial petrogenetic grid applicable to high Mg–Al granulites metamorphosed at high fO2, developed in our earlier work, was extended to higher pressures. The experimental results were successfully applied to several high-grade terranes to estimate P–T conditions and retrograde P–T trajectories.</p></abstract><textClass xml:lang="en"><keywords scheme="keyword"><list><head>KWD</head><item><term>KFMASH equilibria</term></item><item><term>experimental petrogenetic grid at high fO2</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2003-06">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/1023F93607ECA96C8607A1B0A896651AC6FE8A07/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="corpus oup" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0" encoding="US-ASCII"</istex:xmlDeclaration><istex:docType PUBLIC="-//NLM//DTD Journal Publishing DTD v2.3 20070202//EN" URI="journalpublishing.dtd" name="istex:docType"></istex:docType><istex:document><article xml:lang="en" article-type="research-article"><front><journal-meta><journal-id journal-id-type="hwp">petrology</journal-id><journal-id journal-id-type="nlm-ta">J Petrology</journal-id><journal-id journal-id-type="publisher-id">petroj</journal-id><journal-title>Journal of Petrology</journal-title><abbrev-journal-title abbrev-type="publisher">J. Petrology</abbrev-journal-title><issn pub-type="ppub">0022-3530</issn><issn pub-type="epub">1460-2415</issn><publisher><publisher-name>Oxford University Press</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="other">egg029</article-id><article-id pub-id-type="doi">10.1093/petrology/44.6.1055</article-id><article-categories><subj-group subj-group-type="heading"><subject>ARTICLE</subject></subj-group></article-categories><title-group><article-title>An Experimentally Constrained Petrogenetic Grid in the Silica-Saturated Portion of the System KFMASH at High Temperatures and Pressures</article-title></title-group><contrib-group><contrib contrib-type="author"><name><surname>DAS</surname><given-names>KAUSHIK</given-names></name><xref rid="A1">1</xref><xref rid="C1">*</xref></contrib><contrib contrib-type="author"><name><surname>DASGUPTA</surname><given-names>SOMNATH</given-names></name><xref rid="A2">2</xref></contrib><contrib contrib-type="author"><name><surname>MIURA</surname><given-names>HIROYUKI</given-names></name><xref rid="A1">1</xref></contrib><aff id="A1"><label>1</label>DIVISION OF EARTH AND PLANETARY SCIENCES, GRADUATE SCHOOL OF SCIENCE, HOKKAIDO UNIVERSITY, N10W8, KITA-KU, SAPPORO-SHI, JAPAN, 060-0810</aff><aff id="A2"><label>2</label>DEPARTMENT OF GEOLOGICAL SCIENCES, JADAVPUR UNIVERSITY, KOLKATA, INDIA</aff></contrib-group><author-notes><corresp id="C1">Telephone: +81-11-706-4651. Fax: +81-11-706-4650. E-mail: <ext-link xlink:href="kaus@ep.sci.hokudai.ac.jp" ext-link-type="email">kaus@ep.sci.hokudai.ac.jp</ext-link></corresp></author-notes><pub-date pub-type="ppub"><month>06</month><year>2003</year></pub-date><volume>44</volume><issue>6</issue><fpage>1055</fpage><lpage>1075</lpage><history><date date-type="accepted"><day>06</day><month>12</month><year>2002</year></date><date date-type="received"><day>17</day><month>02</month><year>2002</year></date></history><permissions><copyright-year>2003</copyright-year></permissions><abstract xml:lang="en"><p>Experiments in the quartz-saturated part of the system KFMASH under <italic>f</italic>O<sub>2</sub> conditions of the haematite–magnetite buffer and using bulk compositions with <italic>X</italic><sub>Mg</sub> of 0·81, 0·72, 0·53 define the stability limits of several mineral assemblages within the <italic>P</italic>–<italic>T</italic> field 9–12 kbar, 850–1100°C. The stability limits of the mineral assemblages orthopyroxene + spinel + cordierite ± sapphirine, orthopyroxene + garnet + sapphirine, sapphirine + cordierite + orthopyroxene and garnet + orthopyroxene + spinel have been delineated on the basis of <italic>P</italic>–<italic>T</italic> and <italic>T–X</italic> pseudosections. Sapphirine did not appear in the bulk composition of <italic>X</italic><sub>Mg</sub> = 0·53. A partial petrogenetic grid applicable to high Mg–Al granulites metamorphosed at high <italic>f</italic>O<sub>2</sub>, developed in our earlier work, was extended to higher pressures. The experimental results were successfully applied to several high-grade terranes to estimate <italic>P</italic>–<italic>T</italic> conditions and retrograde <italic>P</italic>–<italic>T</italic> trajectories.</p></abstract><kwd-group kwd-group-type="KWD" xml:lang="en"><kwd>KFMASH equilibria</kwd><kwd>experimental petrogenetic grid at high <italic>f</italic>O<sub>2</sub></kwd></kwd-group><custom-meta-wrap><custom-meta><meta-name>hwp-legacy-fpage</meta-name><meta-value>1055</meta-value></custom-meta><custom-meta><meta-name>hwp-legacy-dochead</meta-name><meta-value>ARTICLE</meta-value></custom-meta></custom-meta-wrap></article-meta></front></article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>An Experimentally Constrained Petrogenetic Grid in the Silica-Saturated Portion of the System KFMASH at High Temperatures and Pressures</title></titleInfo><titleInfo type="alternative" lang="en" contentType="CDATA"><title>An Experimentally Constrained Petrogenetic Grid in the Silica-Saturated Portion of the System KFMASH at High Temperatures and Pressures</title></titleInfo><name type="personal"><namePart type="given">KAUSHIK</namePart><namePart type="family">DAS</namePart><affiliation>DIVISION OF EARTH AND PLANETARY SCIENCES, GRADUATE SCHOOL OF SCIENCE, HOKKAIDO UNIVERSITY, N10W8, KITA-KU, SAPPORO-SHI, JAPAN, 060-0810</affiliation><affiliation>Telephone: +81-11-706-4651. Fax: +81-11-706-4650.</affiliation><affiliation>E-mail: kaus@ep.sci.hokudai.ac.jp</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">SOMNATH</namePart><namePart type="family">DASGUPTA</namePart><affiliation>DEPARTMENT OF GEOLOGICAL SCIENCES, JADAVPUR UNIVERSITY, KOLKATA, INDIA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">HIROYUKI</namePart><namePart type="family">MIURA</namePart><affiliation>DIVISION OF EARTH AND PLANETARY SCIENCES, GRADUATE SCHOOL OF SCIENCE, HOKKAIDO UNIVERSITY, N10W8, KITA-KU, SAPPORO-SHI, JAPAN, 060-0810</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="research-article"></genre><originInfo><publisher>Oxford University Press</publisher><dateIssued encoding="w3cdtf">2003-06</dateIssued><copyrightDate encoding="w3cdtf">2003</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Experiments in the quartz-saturated part of the system KFMASH under fO2 conditions of the haematite–magnetite buffer and using bulk compositions with XMg of 0·81, 0·72, 0·53 define the stability limits of several mineral assemblages within the P–T field 9–12 kbar, 850–1100°C. The stability limits of the mineral assemblages orthopyroxene + spinel + cordierite ± sapphirine, orthopyroxene + garnet + sapphirine, sapphirine + cordierite + orthopyroxene and garnet + orthopyroxene + spinel have been delineated on the basis of P–T and T–X pseudosections. Sapphirine did not appear in the bulk composition of XMg = 0·53. A partial petrogenetic grid applicable to high Mg–Al granulites metamorphosed at high fO2, developed in our earlier work, was extended to higher pressures. The experimental results were successfully applied to several high-grade terranes to estimate P–T conditions and retrograde P–T trajectories.</abstract><note type="author-notes">Telephone: +81-11-706-4651. Fax: +81-11-706-4650. E-mail: kaus@ep.sci.hokudai.ac.jp</note><subject lang="en"><genre>KWD</genre><topic>KFMASH equilibria</topic><topic>experimental petrogenetic grid at high fO2</topic></subject><relatedItem type="host"><titleInfo><title>Journal of Petrology</title></titleInfo><titleInfo type="abbreviated"><title>J. 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|type= RBID
|clé= ISTEX:1023F93607ECA96C8607A1B0A896651AC6FE8A07
|texte= An Experimentally Constrained Petrogenetic Grid in the Silica-Saturated Portion of the System KFMASH at High Temperatures and Pressures
}}
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