Viscoplastic flow in migmatites deduced from fabric anisotropy: An example from the Naxos dome, Greece
Identifieur interne : 002372 ( Istex/Corpus ); précédent : 002371; suivant : 002373Viscoplastic flow in migmatites deduced from fabric anisotropy: An example from the Naxos dome, Greece
Auteurs : Seth C. Kruckenberg ; Eric C. Ferré ; Christian Teyssier ; Olivier Vanderhaeghe ; Donna L. Whitney ; Nicholas C. A. Seaton ; Justin A. SkordSource :
- Journal of Geophysical Research: Solid Earth [ 0148-0227 ] ; 2010-09.
Abstract
Many migmatites represent crystallized partially molten crust and therefore record the mechanisms and pathways of orogenic crustal flow. Field and microstructural methods may be insufficient to characterize the planar and linear elements of rock fabric in migmatites due to obscured flow fabrics or protracted deformation. In the Naxos dome (Greece), we test the anisotropy of magnetic susceptibility (AMS) as a tool for recovering mineral fabric symmetry and the kinematic axes of flow in migmatites. Measurements of 155 migmatite samples yield dominantly low values (<300 × 10−6 [SI]) of bulk magnetic susceptibility (Km) consistent with biotite being the dominant carrier of the AMS. Higher values of Km, thermomagnetic, hysteresis, and microstructural data, however, suggest a ferromagnetic contribution from magnetite in a subset of samples (N = 15). Using electron backscatter diffraction (EBSD) analysis, we establish the correspondence of the biotite subfabric with the AMS and structural fabric of the Naxos migmatites. EBSD data from biotite suggests that magnetic lineation in these dominantly paramagnetic migmatites arises from a zone axis orientation of biotite crystals organized about the direction of viscoplastic flow. Over a range of spatial scales, migmatitic foliation and magnetic foliation are well correlated. The magnetic lineation recovered by AMS displays a coherent organization despite the heterogeneous structure and composition of the Naxos migmatites. These data suggest that the apparent complexity of migmatites masks a simpler flow regime controlled by bulk viscoplastic flow. Furthermore, our study demonstrates the utility of the AMS method for studying the dynamics of partially molten orogenic crust.
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DOI: 10.1029/2009JB007012
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Ferré</name><affiliation><mods:affiliation>Department of Geology, Southern Illinois University at Carbondale, Illinois, Carbondale, USA</mods:affiliation></affiliation></author><author><name sortKey="Teyssier, Christian" sort="Teyssier, Christian" uniqKey="Teyssier C" first="Christian" last="Teyssier">Christian Teyssier</name><affiliation><mods:affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</mods:affiliation></affiliation></author><author><name sortKey="Vanderhaeghe, Olivier" sort="Vanderhaeghe, Olivier" uniqKey="Vanderhaeghe O" first="Olivier" last="Vanderhaeghe">Olivier Vanderhaeghe</name><affiliation><mods:affiliation>G2R, Université Henri Poincaré Nancy 1, Vandoeuvre‐lès‐Nancy, France</mods:affiliation></affiliation></author><author><name sortKey="Whitney, Donna L" sort="Whitney, Donna L" uniqKey="Whitney D" first="Donna L." last="Whitney">Donna L. Whitney</name><affiliation><mods:affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</mods:affiliation></affiliation></author><author><name sortKey="Seaton, Nicholas C A" sort="Seaton, Nicholas C A" uniqKey="Seaton N" first="Nicholas C. A." last="Seaton">Nicholas C. A. Seaton</name><affiliation><mods:affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</mods:affiliation></affiliation></author><author><name sortKey="Skord, Justin A" sort="Skord, Justin A" uniqKey="Skord J" first="Justin A." last="Skord">Justin A. Skord</name><affiliation><mods:affiliation>Department of Geology, Southern Illinois University at Carbondale, Carbondale, Illinois, USA</mods:affiliation></affiliation><affiliation><mods:affiliation>Now at Department of Geological Sciences and Engineering, University of Nevada, Reno, Reno, Nevada, USA.</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:F9A2422C72B11EA7E9C74586F1A1BC1C7FE34FDB</idno><date when="2010" year="2010">2010</date><idno type="doi">10.1029/2009JB007012</idno><idno type="url">https://api.istex.fr/document/F9A2422C72B11EA7E9C74586F1A1BC1C7FE34FDB/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">002372</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">002372</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Viscoplastic flow in migmatites deduced from fabric anisotropy: An example from the Naxos dome, Greece</title><author><name sortKey="Kruckenberg, Seth C" sort="Kruckenberg, Seth C" uniqKey="Kruckenberg S" first="Seth C." last="Kruckenberg">Seth C. Kruckenberg</name><affiliation><mods:affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minneapolis, Minnesota, USA</mods:affiliation></affiliation><affiliation><mods:affiliation>Now at Department of Geoscience, University of Wisconsin‐Madison, Madison, Wisconsin, USA.</mods:affiliation></affiliation><affiliation><mods:affiliation>E-mail: seth@geology.wisc.edu</mods:affiliation></affiliation></author><author><name sortKey="Ferre, Eric C" sort="Ferre, Eric C" uniqKey="Ferre E" first="Eric C." last="Ferré">Eric C. Ferré</name><affiliation><mods:affiliation>Department of Geology, Southern Illinois University at Carbondale, Illinois, Carbondale, USA</mods:affiliation></affiliation></author><author><name sortKey="Teyssier, Christian" sort="Teyssier, Christian" uniqKey="Teyssier C" first="Christian" last="Teyssier">Christian Teyssier</name><affiliation><mods:affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</mods:affiliation></affiliation></author><author><name sortKey="Vanderhaeghe, Olivier" sort="Vanderhaeghe, Olivier" uniqKey="Vanderhaeghe O" first="Olivier" last="Vanderhaeghe">Olivier Vanderhaeghe</name><affiliation><mods:affiliation>G2R, Université Henri Poincaré Nancy 1, Vandoeuvre‐lès‐Nancy, France</mods:affiliation></affiliation></author><author><name sortKey="Whitney, Donna L" sort="Whitney, Donna L" uniqKey="Whitney D" first="Donna L." last="Whitney">Donna L. Whitney</name><affiliation><mods:affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</mods:affiliation></affiliation></author><author><name sortKey="Seaton, Nicholas C A" sort="Seaton, Nicholas C A" uniqKey="Seaton N" first="Nicholas C. A." last="Seaton">Nicholas C. A. Seaton</name><affiliation><mods:affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</mods:affiliation></affiliation></author><author><name sortKey="Skord, Justin A" sort="Skord, Justin A" uniqKey="Skord J" first="Justin A." last="Skord">Justin A. Skord</name><affiliation><mods:affiliation>Department of Geology, Southern Illinois University at Carbondale, Carbondale, Illinois, USA</mods:affiliation></affiliation><affiliation><mods:affiliation>Now at Department of Geological Sciences and Engineering, University of Nevada, Reno, Reno, Nevada, USA.</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Geophysical Research: Solid Earth</title><title level="j" type="abbrev">J. Geophys. Res.</title><idno type="ISSN">0148-0227</idno><idno type="eISSN">2156-2202</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2010-09">2010-09</date><biblScope unit="volume">115</biblScope><biblScope unit="issue">B9</biblScope><biblScope unit="page" from="/">n/a</biblScope><biblScope unit="page" to="/">n/a</biblScope></imprint><idno type="ISSN">0148-0227</idno></series><idno type="istex">F9A2422C72B11EA7E9C74586F1A1BC1C7FE34FDB</idno><idno type="DOI">10.1029/2009JB007012</idno><idno type="ArticleID">2009JB007012</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0148-0227</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">Many migmatites represent crystallized partially molten crust and therefore record the mechanisms and pathways of orogenic crustal flow. Field and microstructural methods may be insufficient to characterize the planar and linear elements of rock fabric in migmatites due to obscured flow fabrics or protracted deformation. In the Naxos dome (Greece), we test the anisotropy of magnetic susceptibility (AMS) as a tool for recovering mineral fabric symmetry and the kinematic axes of flow in migmatites. Measurements of 155 migmatite samples yield dominantly low values (<300 × 10−6 [SI]) of bulk magnetic susceptibility (Km) consistent with biotite being the dominant carrier of the AMS. Higher values of Km, thermomagnetic, hysteresis, and microstructural data, however, suggest a ferromagnetic contribution from magnetite in a subset of samples (N = 15). Using electron backscatter diffraction (EBSD) analysis, we establish the correspondence of the biotite subfabric with the AMS and structural fabric of the Naxos migmatites. EBSD data from biotite suggests that magnetic lineation in these dominantly paramagnetic migmatites arises from a zone axis orientation of biotite crystals organized about the direction of viscoplastic flow. Over a range of spatial scales, migmatitic foliation and magnetic foliation are well correlated. The magnetic lineation recovered by AMS displays a coherent organization despite the heterogeneous structure and composition of the Naxos migmatites. These data suggest that the apparent complexity of migmatites masks a simpler flow regime controlled by bulk viscoplastic flow. Furthermore, our study demonstrates the utility of the AMS method for studying the dynamics of partially molten orogenic crust.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Seth C. Kruckenberg</name><affiliations><json:string>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minneapolis, Minnesota, USA</json:string><json:string>Now at Department of Geoscience, University of Wisconsin‐Madison, Madison, Wisconsin, USA.</json:string><json:string>E-mail: seth@geology.wisc.edu</json:string></affiliations></json:item><json:item><name>Eric C. Ferré</name><affiliations><json:string>Department of Geology, Southern Illinois University at Carbondale, Illinois, Carbondale, USA</json:string></affiliations></json:item><json:item><name>Christian Teyssier</name><affiliations><json:string>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</json:string></affiliations></json:item><json:item><name>Olivier Vanderhaeghe</name><affiliations><json:string>G2R, Université Henri Poincaré Nancy 1, Vandoeuvre‐lès‐Nancy, France</json:string></affiliations></json:item><json:item><name>Donna L. Whitney</name><affiliations><json:string>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</json:string></affiliations></json:item><json:item><name>Nicholas C. A. Seaton</name><affiliations><json:string>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</json:string></affiliations></json:item><json:item><name>Justin A. Skord</name><affiliations><json:string>Department of Geology, Southern Illinois University at Carbondale, Carbondale, Illinois, USA</json:string><json:string>Now at Department of Geological Sciences and Engineering, University of Nevada, Reno, Reno, Nevada, USA.</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>migmatite</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Naxos</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>AMS</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>magnetic</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>EBSD</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>fabric</value></json:item></subject><articleId><json:string>2009JB007012</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>Many migmatites represent crystallized partially molten crust and therefore record the mechanisms and pathways of orogenic crustal flow. Field and microstructural methods may be insufficient to characterize the planar and linear elements of rock fabric in migmatites due to obscured flow fabrics or protracted deformation. In the Naxos dome (Greece), we test the anisotropy of magnetic susceptibility (AMS) as a tool for recovering mineral fabric symmetry and the kinematic axes of flow in migmatites. Measurements of 155 migmatite samples yield dominantly low values (>300 × 10−6 [SI]) of bulk magnetic susceptibility (Km) consistent with biotite being the dominant carrier of the AMS. Higher values of Km, thermomagnetic, hysteresis, and microstructural data, however, suggest a ferromagnetic contribution from magnetite in a subset of samples (N = 15). Using electron backscatter diffraction (EBSD) analysis, we establish the correspondence of the biotite subfabric with the AMS and structural fabric of the Naxos migmatites. EBSD data from biotite suggests that magnetic lineation in these dominantly paramagnetic migmatites arises from a zone axis orientation of biotite crystals organized about the direction of viscoplastic flow. Over a range of spatial scales, migmatitic foliation and magnetic foliation are well correlated. The magnetic lineation recovered by AMS displays a coherent organization despite the heterogeneous structure and composition of the Naxos migmatites. These data suggest that the apparent complexity of migmatites masks a simpler flow regime controlled by bulk viscoplastic flow. Furthermore, our study demonstrates the utility of the AMS method for studying the dynamics of partially molten orogenic crust.</abstract><qualityIndicators><score>9.5</score><pdfVersion>1.6</pdfVersion><pdfPageSize>612 x 792 pts (letter)</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>1739</abstractCharCount><pdfWordCount>9220</pdfWordCount><pdfCharCount>60040</pdfCharCount><pdfPageCount>18</pdfPageCount><abstractWordCount>251</abstractWordCount></qualityIndicators><title>Viscoplastic flow in migmatites deduced from fabric anisotropy: An example from the Naxos dome, Greece</title><refBibs><json:item><author><json:item><name>D. Avigad</name></json:item></author><host><volume>10</volume><pages><last>1319</last><first>1309</first></pages><author></author><title>Eur. J. Mineral.</title></host><title>High‐pressure metamorphism and cooling on SE Naxos (Cyclades, Greece)</title></json:item><json:item><author><json:item><name>C. 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A.</forename><surname>Seaton</surname></persName><affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</affiliation></author><author xml:id="author-7"><persName><forename type="first">Justin A.</forename><surname>Skord</surname></persName><affiliation>Department of Geology, Southern Illinois University at Carbondale, Carbondale, Illinois, USA</affiliation><affiliation>Now at Department of Geological Sciences and Engineering, University of Nevada, Reno, Reno, Nevada, USA.</affiliation></author></analytic><monogr><title level="j">Journal of Geophysical Research: Solid Earth</title><title level="j" type="abbrev">J. Geophys. Res.</title><idno type="pISSN">0148-0227</idno><idno type="eISSN">2156-2202</idno><idno type="DOI">10.1002/(ISSN)2156-2202b</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2010-09"></date><biblScope unit="volume">115</biblScope><biblScope unit="issue">B9</biblScope><biblScope unit="page" from="/">n/a</biblScope><biblScope unit="page" to="/">n/a</biblScope></imprint></monogr><idno type="istex">F9A2422C72B11EA7E9C74586F1A1BC1C7FE34FDB</idno><idno type="DOI">10.1029/2009JB007012</idno><idno type="ArticleID">2009JB007012</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2010</date></creation><langUsage><language ident="en">en</language></langUsage><abstract><p>Many migmatites represent crystallized partially molten crust and therefore record the mechanisms and pathways of orogenic crustal flow. Field and microstructural methods may be insufficient to characterize the planar and linear elements of rock fabric in migmatites due to obscured flow fabrics or protracted deformation. In the Naxos dome (Greece), we test the anisotropy of magnetic susceptibility (AMS) as a tool for recovering mineral fabric symmetry and the kinematic axes of flow in migmatites. Measurements of 155 migmatite samples yield dominantly low values (<300 × 10−6 [SI]) of bulk magnetic susceptibility (Km) consistent with biotite being the dominant carrier of the AMS. Higher values of Km, thermomagnetic, hysteresis, and microstructural data, however, suggest a ferromagnetic contribution from magnetite in a subset of samples (N = 15). Using electron backscatter diffraction (EBSD) analysis, we establish the correspondence of the biotite subfabric with the AMS and structural fabric of the Naxos migmatites. EBSD data from biotite suggests that magnetic lineation in these dominantly paramagnetic migmatites arises from a zone axis orientation of biotite crystals organized about the direction of viscoplastic flow. Over a range of spatial scales, migmatitic foliation and magnetic foliation are well correlated. The magnetic lineation recovered by AMS displays a coherent organization despite the heterogeneous structure and composition of the Naxos migmatites. These data suggest that the apparent complexity of migmatites masks a simpler flow regime controlled by bulk viscoplastic flow. Furthermore, our study demonstrates the utility of the AMS method for studying the dynamics of partially molten orogenic crust.</p></abstract><textClass><keywords scheme="keyword"><list><head>keywords</head><item><term>migmatite</term></item><item><term>Naxos</term></item><item><term>AMS</term></item><item><term>magnetic</term></item><item><term>EBSD</term></item><item><term>fabric</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>index-terms</head><item><term>Geodesy and Gravity/Tectonophysics</term></item><item><term>EXPLORATION GEOPHYSICS</term></item><item><term>Continental structures</term></item><item><term>GEOMAGNETISM AND PALEOMAGNETISM</term></item><item><term>Magnetic fabrics and anisotropy</term></item><item><term>MINERALOGY AND PETROLOGY</term></item><item><term>Petrography, microstructures, and textures</term></item><item><term>STRUCTURAL GEOLOGY</term></item><item><term>Instruments and techniques</term></item><item><term>Rheology: crust and lithosphere</term></item><item><term>TECTONOPHYSICS</term></item><item><term>Continental tectonics: general</term></item><item><term>Rheology: crust and lithosphere</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>article-category</head><item><term>Geodesy and Gravity/Tectonophysics</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2009-10-07">Received</change><change when="2010-03-29">Registration</change><change when="2010-09">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/F9A2422C72B11EA7E9C74586F1A1BC1C7FE34FDB/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 type="serialArticle" version="2.0" xml:lang="en" xml:id="jgrb16413"><header><publicationMeta level="product"><doi>10.1002/(ISSN)2156-2202b</doi><issn type="print">0148-0227</issn><issn type="electronic">2156-2202</issn><idGroup><id type="product" value="JGRB"></id><id type="coden" value="JGREA2"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH">Journal of Geophysical Research: Solid Earth</title><title type="short">J. Geophys. Res.</title></titleGroup></publicationMeta><publicationMeta level="part" position="90"><doi>10.1002/jgrb.v115.B9</doi><idGroup><id type="focusSection" value="2"></id></idGroup><titleGroup><title type="focusSection" xml:lang="en">Journal of Geophysical Research: Solid Earth</title></titleGroup><numberingGroup><numbering type="journalVolume" number="115">115</numbering><numbering type="journalIssue">B9</numbering></numberingGroup><coverDate startDate="2010-09">September 2010</coverDate></publicationMeta><publicationMeta level="unit" position="260" type="article" status="forIssue"><doi>10.1029/2009JB007012</doi><idGroup><id type="editorialOffice" value="2009JB007012"></id><id type="society" value="B09401"></id><id type="unit" value="JGRB16413"></id></idGroup><countGroup><count type="pageTotal" number="18"></count></countGroup><titleGroup><title type="articleCategory">Geodesy and Gravity/Tectonophysics</title><title type="tocHeading1">Geodesy and Gravity/Tectonophysics</title></titleGroup><copyright ownership="thirdParty">Copyright 2010 by the American Geophysical Union.</copyright><eventGroup><event type="manuscriptReceived" date="2009-10-07"></event><event type="manuscriptRevised" date="2010-03-09"></event><event type="manuscriptAccepted" date="2010-03-29"></event><event type="firstOnline" date="2010-09-01"></event><event type="publishedOnlineFinalForm" date="2010-09-01"></event><event type="xmlConverted" agent="SPi Global Converter:AGUv3.44_TO_WileyML3Gv1.0.3 version:1.1; WileyML 3G Packaging Tool v1.0; AGU2WileyML3G Final Clean Up v1.0" date="2012-12-18"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:3.8.8" date="2014-01-31"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-30"></event></eventGroup><numberingGroup><numbering type="pageFirst">n/a</numbering><numbering type="pageLast">n/a</numbering></numberingGroup><subjectInfo><subject href="http://psi.agu.org/subset/ETG">Geodesy and Gravity/Tectonophysics</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0900">EXPLORATION GEOPHYSICS</subject><subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0905">Continental structures</subject></subjectInfo><subject href="http://psi.agu.org/taxonomy5/1500">GEOMAGNETISM AND PALEOMAGNETISM</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/1518">Magnetic fabrics and anisotropy</subject></subjectInfo><subject href="http://psi.agu.org/taxonomy5/3600">MINERALOGY AND PETROLOGY</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/3625">Petrography, microstructures, and textures</subject></subjectInfo><subject href="http://psi.agu.org/taxonomy5/8000">STRUCTURAL GEOLOGY</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/8094">Instruments and techniques</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/8031">Rheology: crust and lithosphere</subject></subjectInfo><subject href="http://psi.agu.org/taxonomy5/8100">TECTONOPHYSICS</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/8110">Continental tectonics: general</subject><subject href="http://psi.agu.org/taxonomy5/8159">Rheology: crust and lithosphere</subject></subjectInfo></subjectInfo><selfCitationGroup><citation xml:id="jgrb16413-cit-0000" type="self"><author><familyName>Kruckenberg</familyName>, <givenNames>S. C.</givenNames></author>, <author><givenNames>E. C.</givenNames> <familyName>Ferré</familyName></author>, <author><givenNames>C.</givenNames> <familyName>Teyssier</familyName></author>, <author><givenNames>O.</givenNames> <familyName>Vanderhaeghe</familyName></author>, <author><givenNames>D. L.</givenNames> <familyName>Whitney</familyName></author>, <author><givenNames>N. C. A.</givenNames> <familyName>Seaton</familyName></author>, and <author><givenNames>J. A.</givenNames> <familyName>Skord</familyName></author> (<pubYear year="2010">2010</pubYear>), <articleTitle>Viscoplastic flow in migmatites deduced from fabric anisotropy: An example from the Naxos dome, Greece</articleTitle>, <journalTitle>J. Geophys. Res.</journalTitle>, <vol>115</vol>, B09401, doi:<accessionId ref="info:doi/10.1029/2009JB007012">10.1029/2009JB007012</accessionId>.</citation></selfCitationGroup><linkGroup><link type="toTypesetVersion" href="file:JGRB.JGRB16413.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="wordTotal" number="10100"></count><count type="figureTotal" number="11"></count></countGroup><titleGroup><title type="main">Viscoplastic flow in migmatites deduced from fabric anisotropy: An example from the Naxos dome, Greece</title><title type="short">VISCOPLASTIC FLOW IN MIGMATITES</title><title type="shortAuthors">Kruckenberg <i>et al</i>.</title></titleGroup><creators><creator creatorRole="author" xml:id="jgrb16413-cr-0001" affiliationRef="#jgrb16413-aff-0001 #jgrb16413-aff-0004"><personName><givenNames>Seth C.</givenNames> <familyName>Kruckenberg</familyName></personName><contactDetails><email normalForm="seth@geology.wisc.edu">seth@geology.wisc.edu</email></contactDetails></creator><creator creatorRole="author" xml:id="jgrb16413-cr-0002" affiliationRef="#jgrb16413-aff-0002"><personName><givenNames>Eric C.</givenNames> <familyName>Ferré</familyName></personName></creator><creator creatorRole="author" xml:id="jgrb16413-cr-0003" affiliationRef="#jgrb16413-aff-0001"><personName><givenNames>Christian</givenNames> <familyName>Teyssier</familyName></personName></creator><creator creatorRole="author" xml:id="jgrb16413-cr-0004" affiliationRef="#jgrb16413-aff-0003"><personName><givenNames>Olivier</givenNames> <familyName>Vanderhaeghe</familyName></personName></creator><creator creatorRole="author" xml:id="jgrb16413-cr-0005" affiliationRef="#jgrb16413-aff-0001"><personName><givenNames>Donna L.</givenNames> <familyName>Whitney</familyName></personName></creator><creator creatorRole="author" xml:id="jgrb16413-cr-0006" affiliationRef="#jgrb16413-aff-0001"><personName><givenNames>Nicholas C. A.</givenNames> <familyName>Seaton</familyName></personName></creator><creator creatorRole="author" xml:id="jgrb16413-cr-0007" affiliationRef="#jgrb16413-aff-0002 #jgrb16413-aff-0005"><personName><givenNames>Justin A.</givenNames> <familyName>Skord</familyName></personName></creator></creators><affiliationGroup><affiliation countryCode="US" type="organization" xml:id="jgrb16413-aff-0001"><orgDiv>Department of Geology and Geophysics</orgDiv><orgName>University of Minnesota‐Twin Cities</orgName><address><city>Minneapolis</city><countryPart>Minnesota</countryPart><country>USA</country></address></affiliation><affiliation countryCode="US" type="organization" xml:id="jgrb16413-aff-0002"><orgDiv>Department of Geology</orgDiv><orgName>Southern Illinois University at Carbondale</orgName><address><city>Carbondale</city><countryPart>Illinois</countryPart><country>USA</country></address></affiliation><affiliation countryCode="FR" type="organization" xml:id="jgrb16413-aff-0003"><orgDiv>G2R</orgDiv><orgName>Université Henri Poincaré Nancy 1</orgName><address><city>Vandoeuvre‐lès‐Nancy</city><country>France</country></address></affiliation><affiliation type="organization" xml:id="jgrb16413-aff-0004"><unparsedAffiliation>Now at Department of Geoscience, University of Wisconsin‐Madison, Madison, Wisconsin, USA.</unparsedAffiliation></affiliation><affiliation type="organization" xml:id="jgrb16413-aff-0005"><unparsedAffiliation>Now at Department of Geological Sciences and Engineering, University of Nevada, Reno, Reno, Nevada, USA.</unparsedAffiliation></affiliation></affiliationGroup><keywordGroup type="author"><keyword xml:id="jgrb16413-kwd-0001">migmatite</keyword><keyword xml:id="jgrb16413-kwd-0002">Naxos</keyword><keyword xml:id="jgrb16413-kwd-0003">AMS</keyword><keyword xml:id="jgrb16413-kwd-0004">magnetic</keyword><keyword xml:id="jgrb16413-kwd-0005">EBSD</keyword><keyword xml:id="jgrb16413-kwd-0006">fabric</keyword></keywordGroup><supportingInformation xml:id="jgrb16413-sup-0000"><p xml:id="jgrb16413-para-0001">Auxiliary material for this article contains three tables and two figures described in further detail and referenced in the discussion of the paper.</p><p xml:id="jgrb16413-para-0002">Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac).</p><p xml:id="jgrb16413-para-0003">Additional file information is provided in the readme.txt.</p><supportingInfoItem><mediaResource alt="supplementary data" mimeType="text/plain" href="urn-x:wiley:01480227:media:jgrb16413:jgrb16413-sup-0001-readme"></mediaResource><caption>readme.txt</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" mimeType="application/pdf" href="urn-x:wiley:01480227:media:jgrb16413:jgrb16413-sup-0002-ds01"></mediaResource><caption>Data Set S1. Low‐field anisotropy of magnetic susceptibility (LF‐AMS) data for Naxos migmatite cubic specimens.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" mimeType="application/pdf" href="urn-x:wiley:01480227:media:jgrb16413:jgrb16413-sup-0003-ts01"></mediaResource><caption>Table S1. Low‐field Anisotropy of Magnetic Susceptibility (LF‐AMS) sample averages for Naxos migmatite specimens reported in Data Set S1.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" mimeType="application/pdf" href="urn-x:wiley:01480227:media:jgrb16413:jgrb16413-sup-0004-ts02"></mediaResource><caption>Table S2. Hysteresis properties and comparison of low‐field (LF) and high‐field (HF) magnetic susceptibility for representative specimens of Naxos migmatite stations.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" mimeType="application/pdf" href="urn-x:wiley:01480227:media:jgrb16413:jgrb16413-sup-0005-fs01"></mediaResource><caption>Figure S1. Stereonets of low‐field anisotropy of magnetic susceptibility (LF‐AMS) principal susceptibility orientations and associated axial confidence ellipses for Naxos migmatite cubic specimens by station.</caption></supportingInfoItem><supportingInfoItem><mediaResource alt="supplementary data" mimeType="application/pdf" href="urn-x:wiley:01480227:media:jgrb16413:jgrb16413-sup-0006-fs02"></mediaResource><caption>Figure S2. Complete thermomagnetic and hysteresis properties of representative Naxos migmatite samples.</caption></supportingInfoItem></supportingInformation><abstractGroup><abstract type="main"><p xml:id="jgrb16413-para-0004" label="1">Many migmatites represent crystallized partially molten crust and therefore record the mechanisms and pathways of orogenic crustal flow. Field and microstructural methods may be insufficient to characterize the planar and linear elements of rock fabric in migmatites due to obscured flow fabrics or protracted deformation. In the Naxos dome (Greece), we test the anisotropy of magnetic susceptibility (AMS) as a tool for recovering mineral fabric symmetry and the kinematic axes of flow in migmatites. Measurements of 155 migmatite samples yield dominantly low values (<300 × 10<sup>−6</sup> [SI]) of bulk magnetic susceptibility (K<sub>m</sub>) consistent with biotite being the dominant carrier of the AMS. Higher values of K<sub>m</sub>, thermomagnetic, hysteresis, and microstructural data, however, suggest a ferromagnetic contribution from magnetite in a subset of samples (N = 15). Using electron backscatter diffraction (EBSD) analysis, we establish the correspondence of the biotite subfabric with the AMS and structural fabric of the Naxos migmatites. EBSD data from biotite suggests that magnetic lineation in these dominantly paramagnetic migmatites arises from a zone axis orientation of biotite crystals organized about the direction of viscoplastic flow. Over a range of spatial scales, migmatitic foliation and magnetic foliation are well correlated. The magnetic lineation recovered by AMS displays a coherent organization despite the heterogeneous structure and composition of the Naxos migmatites. These data suggest that the apparent complexity of migmatites masks a simpler flow regime controlled by bulk viscoplastic flow. Furthermore, our study demonstrates the utility of the AMS method for studying the dynamics of partially molten orogenic crust.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Viscoplastic flow in migmatites deduced from fabric anisotropy: An example from the Naxos dome, Greece</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>VISCOPLASTIC FLOW IN MIGMATITES</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Viscoplastic flow in migmatites deduced from fabric anisotropy: An example from the Naxos dome, Greece</title></titleInfo><name type="personal"><namePart type="given">Seth C.</namePart><namePart type="family">Kruckenberg</namePart><affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minneapolis, Minnesota, USA</affiliation><affiliation>Now at Department of Geoscience, University of Wisconsin‐Madison, Madison, Wisconsin, USA.</affiliation><affiliation>E-mail: seth@geology.wisc.edu</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Eric C.</namePart><namePart type="family">Ferré</namePart><affiliation>Department of Geology, Southern Illinois University at Carbondale, Illinois, Carbondale, USA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Christian</namePart><namePart type="family">Teyssier</namePart><affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Olivier</namePart><namePart type="family">Vanderhaeghe</namePart><affiliation>G2R, Université Henri Poincaré Nancy 1, Vandoeuvre‐lès‐Nancy, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Donna L.</namePart><namePart type="family">Whitney</namePart><affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Nicholas C. A.</namePart><namePart type="family">Seaton</namePart><affiliation>Department of Geology and Geophysics, University of Minnesota‐Twin Cities, Minnesota, Minneapolis, USA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Justin A.</namePart><namePart type="family">Skord</namePart><affiliation>Department of Geology, Southern Illinois University at Carbondale, Carbondale, Illinois, USA</affiliation><affiliation>Now at Department of Geological Sciences and Engineering, University of Nevada, Reno, Reno, Nevada, USA.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">2010-09</dateIssued><dateCaptured encoding="w3cdtf">2009-10-07</dateCaptured><dateValid encoding="w3cdtf">2010-03-29</dateValid><edition>Kruckenberg, S. C., E. C. Ferré, C. Teyssier, O. Vanderhaeghe, D. L. Whitney, N. C. A. Seaton, and J. A. Skord (2010), Viscoplastic flow in migmatites deduced from fabric anisotropy: An example from the Naxos dome, Greece, J. Geophys. Res., 115, B09401, doi:10.1029/2009JB007012.</edition><copyrightDate encoding="w3cdtf">2010</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="figures">11</extent><extent unit="words">10100</extent></physicalDescription><abstract>Many migmatites represent crystallized partially molten crust and therefore record the mechanisms and pathways of orogenic crustal flow. Field and microstructural methods may be insufficient to characterize the planar and linear elements of rock fabric in migmatites due to obscured flow fabrics or protracted deformation. In the Naxos dome (Greece), we test the anisotropy of magnetic susceptibility (AMS) as a tool for recovering mineral fabric symmetry and the kinematic axes of flow in migmatites. Measurements of 155 migmatite samples yield dominantly low values (<300 × 10−6 [SI]) of bulk magnetic susceptibility (Km) consistent with biotite being the dominant carrier of the AMS. Higher values of Km, thermomagnetic, hysteresis, and microstructural data, however, suggest a ferromagnetic contribution from magnetite in a subset of samples (N = 15). Using electron backscatter diffraction (EBSD) analysis, we establish the correspondence of the biotite subfabric with the AMS and structural fabric of the Naxos migmatites. EBSD data from biotite suggests that magnetic lineation in these dominantly paramagnetic migmatites arises from a zone axis orientation of biotite crystals organized about the direction of viscoplastic flow. Over a range of spatial scales, migmatitic foliation and magnetic foliation are well correlated. The magnetic lineation recovered by AMS displays a coherent organization despite the heterogeneous structure and composition of the Naxos migmatites. These data suggest that the apparent complexity of migmatites masks a simpler flow regime controlled by bulk viscoplastic flow. Furthermore, our study demonstrates the utility of the AMS method for studying the dynamics of partially molten orogenic crust.</abstract><subject><genre>keywords</genre><topic>migmatite</topic><topic>Naxos</topic><topic>AMS</topic><topic>magnetic</topic><topic>EBSD</topic><topic>fabric</topic></subject><relatedItem type="host"><titleInfo><title>Journal of Geophysical Research: Solid Earth</title></titleInfo><titleInfo type="abbreviated"><title>J. Geophys. Res.</title></titleInfo><genre type="journal">journal</genre><note type="content"> Auxiliary material for this article contains three tables and two figures described in further detail and referenced in the discussion of the paper. Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac). Additional file information is provided in the readme.txt. Auxiliary material for this article contains three tables and two figures described in further detail and referenced in the discussion of the paper. Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac). Additional file information is provided in the readme.txt. Auxiliary material for this article contains three tables and two figures described in further detail and referenced in the discussion of the paper. Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac). Additional file information is provided in the readme.txt.Supporting Info Item: readme.txt - Data Set S1. Low‐field anisotropy of magnetic susceptibility (LF‐AMS) data for Naxos migmatite cubic specimens. - Table S1. Low‐field Anisotropy of Magnetic Susceptibility (LF‐AMS) sample averages for Naxos migmatite specimens reported in Data Set S1. - Table S2. Hysteresis properties and comparison of low‐field (LF) and high‐field (HF) magnetic susceptibility for representative specimens of Naxos migmatite stations. - Figure S1. Stereonets of low‐field anisotropy of magnetic susceptibility (LF‐AMS) principal susceptibility orientations and associated axial confidence ellipses for Naxos migmatite cubic specimens by station. - Figure S2. Complete thermomagnetic and hysteresis properties of representative Naxos migmatite samples. - </note><subject><genre>index-terms</genre><topic authorityURI="http://psi.agu.org/subset/ETG">Geodesy and Gravity/Tectonophysics</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0900">EXPLORATION GEOPHYSICS</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0905">Continental structures</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1500">GEOMAGNETISM AND PALEOMAGNETISM</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1518">Magnetic fabrics and anisotropy</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3600">MINERALOGY AND PETROLOGY</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3625">Petrography, microstructures, and textures</topic><topic authorityURI="http://psi.agu.org/taxonomy5/8000">STRUCTURAL GEOLOGY</topic><topic authorityURI="http://psi.agu.org/taxonomy5/8094">Instruments and techniques</topic><topic authorityURI="http://psi.agu.org/taxonomy5/8031">Rheology: crust and lithosphere</topic><topic authorityURI="http://psi.agu.org/taxonomy5/8100">TECTONOPHYSICS</topic><topic authorityURI="http://psi.agu.org/taxonomy5/8110">Continental tectonics: general</topic><topic authorityURI="http://psi.agu.org/taxonomy5/8159">Rheology: crust and lithosphere</topic></subject><subject><genre>article-category</genre><topic>Geodesy and Gravity/Tectonophysics</topic></subject><identifier type="ISSN">0148-0227</identifier><identifier type="eISSN">2156-2202</identifier><identifier type="DOI">10.1002/(ISSN)2156-2202b</identifier><identifier type="CODEN">JGREA2</identifier><identifier type="PublisherID">JGRB</identifier><part><date>2010</date><detail type="volume"><caption>vol.</caption><number>115</number></detail><detail type="issue"><caption>no.</caption><number>B9</number></detail><extent unit="pages"><start>n/a</start><end>n/a</end><total>18</total></extent></part></relatedItem><identifier type="istex">F9A2422C72B11EA7E9C74586F1A1BC1C7FE34FDB</identifier><identifier type="DOI">10.1029/2009JB007012</identifier><identifier type="ArticleID">2009JB007012</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright 2010 by the American Geophysical Union.</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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