Oligocene‐Miocene spreading history of the northern South Fiji Basin and implications for the evolution of the New Zealand plate boundary
Identifieur interne : 002131 ( Istex/Corpus ); précédent : 002130; suivant : 002132Oligocene‐Miocene spreading history of the northern South Fiji Basin and implications for the evolution of the New Zealand plate boundary
Auteurs : R. H. Herzer ; D. H. N. Barker ; W. R. Roest ; N. MortimerSource :
- Geochemistry, Geophysics, Geosystems [ 1525-2027 ] ; 2011-02.
Abstract
A tectonic model of the evolution of the northern half of the South Fiji Basin, including the Minerva Triple Junction and Cook Fracture Zone, is developed from regional gravity, multibeam bathymetry, and a new interpretation of magnetic anomalies pinned to radiometric dates of oceanic crust in the basin. The geometry and age of a portion of the Minerva Triple Junction and the Cook‐Minerva spreading center (the connection from the triple junction to the Cook Fracture Zone, which accommodated coeval opening of the Norfolk Basin), are resolved with multibeam bathymetry and magnetics. The South Fiji Basin opened from about 34 to 15 Ma in an anticlockwise sweep about an Euler pole located at the northern end of the present Lau Ridge. This rotation and a rigidly straight southeastward motion of the Three Kings Ridge were accommodated by the configuration of the triple junction changing from ridge‐fault‐fault to ridge‐ridge‐fault to ridge‐ridge‐ridge. During this evolution the southeastern arm of the system, the Julia Fracture Zone, underwent several transformations and the Cook‐Minerva spreading center experienced repeated ridge jumps. The kinematics of the northern South Fiji Basin dictate, to a large extent, the evolution of the southern South Fiji Basin and the Norfolk Basin. This in turn leads to the interpretation of a complex trench‐trench‐double transform fault framework at the northern New Zealand margin, which explains most aspects of the geology, structure, and arc volcanic history of the margin and provides a radical new setting for the origin of the Northland Allochthon.
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DOI: 10.1029/2010GC003291
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Roest</name><affiliation><mods:affiliation>Marine Geosciences Department, Ifremer, Centre de Bretagne, BP 70, F‐29280, Plouzané, France</mods:affiliation></affiliation></author><author><name sortKey="Mortimer, N" sort="Mortimer, N" uniqKey="Mortimer N" first="N." last="Mortimer">N. Mortimer</name><affiliation><mods:affiliation>GNS Science, 9054, Private Bag 1930, Dunedin, New Zealand</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:D68737AF9CBF523EF8D9753700B8D3F7CAB4B551</idno><date when="2011" year="2011">2011</date><idno type="doi">10.1029/2010GC003291</idno><idno type="url">https://api.istex.fr/document/D68737AF9CBF523EF8D9753700B8D3F7CAB4B551/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">002131</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">002131</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Oligocene‐Miocene spreading history of the northern South Fiji Basin and implications for the evolution of the New Zealand plate boundary</title><author><name sortKey="Herzer, R H" sort="Herzer, R H" uniqKey="Herzer R" first="R. H." last="Herzer">R. H. Herzer</name><affiliation><mods:affiliation>GNS Science, PO Box 30368, Lower Hutt 5040,, New Zealand</mods:affiliation></affiliation><affiliation><mods:affiliation>E-mail: r.herzer@gns.cri.nz</mods:affiliation></affiliation></author><author><name sortKey="Barker, D H N" sort="Barker, D H N" uniqKey="Barker D" first="D. H. N." last="Barker">D. H. N. Barker</name><affiliation><mods:affiliation>GNS Science, PO Box 30368, Lower Hutt 5040,, New Zealand</mods:affiliation></affiliation></author><author><name sortKey="Roest, W R" sort="Roest, W R" uniqKey="Roest W" first="W. R." last="Roest">W. R. Roest</name><affiliation><mods:affiliation>Marine Geosciences Department, Ifremer, Centre de Bretagne, BP 70, F‐29280, Plouzané, France</mods:affiliation></affiliation></author><author><name sortKey="Mortimer, N" sort="Mortimer, N" uniqKey="Mortimer N" first="N." last="Mortimer">N. Mortimer</name><affiliation><mods:affiliation>GNS Science, 9054, Private Bag 1930, Dunedin, New Zealand</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Geochemistry, Geophysics, Geosystems</title><title level="j" type="abbrev">Geochem. Geophys. Geosyst.</title><idno type="ISSN">1525-2027</idno><idno type="eISSN">1525-2027</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2011-02">2011-02</date><biblScope unit="volume">12</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="/">n/a</biblScope><biblScope unit="page" to="/">n/a</biblScope></imprint><idno type="ISSN">1525-2027</idno></series><idno type="istex">D68737AF9CBF523EF8D9753700B8D3F7CAB4B551</idno><idno type="DOI">10.1029/2010GC003291</idno><idno type="ArticleID">2010GC003291</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">1525-2027</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">A tectonic model of the evolution of the northern half of the South Fiji Basin, including the Minerva Triple Junction and Cook Fracture Zone, is developed from regional gravity, multibeam bathymetry, and a new interpretation of magnetic anomalies pinned to radiometric dates of oceanic crust in the basin. The geometry and age of a portion of the Minerva Triple Junction and the Cook‐Minerva spreading center (the connection from the triple junction to the Cook Fracture Zone, which accommodated coeval opening of the Norfolk Basin), are resolved with multibeam bathymetry and magnetics. The South Fiji Basin opened from about 34 to 15 Ma in an anticlockwise sweep about an Euler pole located at the northern end of the present Lau Ridge. This rotation and a rigidly straight southeastward motion of the Three Kings Ridge were accommodated by the configuration of the triple junction changing from ridge‐fault‐fault to ridge‐ridge‐fault to ridge‐ridge‐ridge. During this evolution the southeastern arm of the system, the Julia Fracture Zone, underwent several transformations and the Cook‐Minerva spreading center experienced repeated ridge jumps. The kinematics of the northern South Fiji Basin dictate, to a large extent, the evolution of the southern South Fiji Basin and the Norfolk Basin. This in turn leads to the interpretation of a complex trench‐trench‐double transform fault framework at the northern New Zealand margin, which explains most aspects of the geology, structure, and arc volcanic history of the margin and provides a radical new setting for the origin of the Northland Allochthon.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>R. H. Herzer</name><affiliations><json:string>GNS Science, PO Box 30368, Lower Hutt 5040,, New Zealand</json:string><json:string>E-mail: r.herzer@gns.cri.nz</json:string></affiliations></json:item><json:item><name>D. H. N. Barker</name><affiliations><json:string>GNS Science, PO Box 30368, Lower Hutt 5040,, New Zealand</json:string></affiliations></json:item><json:item><name>W. R. Roest</name><affiliations><json:string>Marine Geosciences Department, Ifremer, Centre de Bretagne, BP 70, F‐29280, Plouzané, France</json:string></affiliations></json:item><json:item><name>N. Mortimer</name><affiliations><json:string>GNS Science, 9054, Private Bag 1930, Dunedin, New Zealand</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>South Fiji Basin</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>back‐arc basin evolution</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>multibeam bathymetry</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>magnetic anomalies</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>gravity model</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>New Zealand plate boundary</value></json:item></subject><articleId><json:string>2010GC003291</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>A tectonic model of the evolution of the northern half of the South Fiji Basin, including the Minerva Triple Junction and Cook Fracture Zone, is developed from regional gravity, multibeam bathymetry, and a new interpretation of magnetic anomalies pinned to radiometric dates of oceanic crust in the basin. The geometry and age of a portion of the Minerva Triple Junction and the Cook‐Minerva spreading center (the connection from the triple junction to the Cook Fracture Zone, which accommodated coeval opening of the Norfolk Basin), are resolved with multibeam bathymetry and magnetics. The South Fiji Basin opened from about 34 to 15 Ma in an anticlockwise sweep about an Euler pole located at the northern end of the present Lau Ridge. This rotation and a rigidly straight southeastward motion of the Three Kings Ridge were accommodated by the configuration of the triple junction changing from ridge‐fault‐fault to ridge‐ridge‐fault to ridge‐ridge‐ridge. During this evolution the southeastern arm of the system, the Julia Fracture Zone, underwent several transformations and the Cook‐Minerva spreading center experienced repeated ridge jumps. The kinematics of the northern South Fiji Basin dictate, to a large extent, the evolution of the southern South Fiji Basin and the Norfolk Basin. This in turn leads to the interpretation of a complex trench‐trench‐double transform fault framework at the northern New Zealand margin, which explains most aspects of the geology, structure, and arc volcanic history of the margin and provides a radical new setting for the origin of the Northland Allochthon.</abstract><qualityIndicators><score>8.464</score><pdfVersion>1.4</pdfVersion><pdfPageSize>612 x 792 pts (letter)</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>1603</abstractCharCount><pdfWordCount>9804</pdfWordCount><pdfCharCount>60849</pdfCharCount><pdfPageCount>20</pdfPageCount><abstractWordCount>247</abstractWordCount></qualityIndicators><title>Oligocene‐Miocene spreading history of the northern South Fiji Basin and implications for the evolution of the New Zealand plate boundary</title><refBibs><json:item><author><json:item><name>J. C. Aitchison</name></json:item><json:item><name>G. L. Clarke</name></json:item><json:item><name>S. 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Res.</title></host><title>Evolution and interaction of migrating cross‐arc volcanism and backarc rifting: An example from the southern Havre Trough (35°20′–37°S)</title></json:item></refBibs><genre><json:string>article</json:string></genre><host><volume>12</volume><publisherId><json:string>GGGE</json:string></publisherId><pages><total>20</total><last>n/a</last><first>n/a</first></pages><issn><json:string>1525-2027</json:string></issn><issue>2</issue><subject><json:item><value>GEOMAGNETISM AND PALEOMAGNETISM</value></json:item><json:item><value>Spatial variations attributed to seafloor spreading</value></json:item><json:item><value>MARINE GEOLOGY AND GEOPHYSICS</value></json:item><json:item><value>Back‐arc basin processes</value></json:item><json:item><value>Marine magnetics and paleomagnetics</value></json:item><json:item><value>Plate tectonics</value></json:item><json:item><value>Plate tectonics</value></json:item><json:item><value>TECTONOPHYSICS</value></json:item><json:item><value>Plate motions: past</value></json:item><json:item><value>Plate boundary: general</value></json:item></subject><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1525-2027</json:string></eissn><title>Geochemistry, Geophysics, Geosystems</title><doi><json:string>10.1002/(ISSN)1525-2027</json:string></doi></host><categories><wos><json:string>science</json:string><json:string>geochemistry & geophysics</json:string></wos><scienceMetrix></scienceMetrix></categories><publicationDate>2011</publicationDate><copyrightDate>2011</copyrightDate><doi><json:string>10.1029/2010GC003291</json:string></doi><id>D68737AF9CBF523EF8D9753700B8D3F7CAB4B551</id><score>0.09925545</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/D68737AF9CBF523EF8D9753700B8D3F7CAB4B551/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/D68737AF9CBF523EF8D9753700B8D3F7CAB4B551/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/D68737AF9CBF523EF8D9753700B8D3F7CAB4B551/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Oligocene‐Miocene spreading history of the northern South Fiji Basin and implications for the evolution of the New Zealand plate boundary</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Blackwell Publishing Ltd</publisher><availability><p>Copyright 2011 by the American Geophysical Union.</p></availability><date>2011</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Oligocene‐Miocene spreading history of the northern South Fiji Basin and implications for the evolution of the New Zealand plate boundary</title><author xml:id="author-1"><persName><forename type="first">R. H.</forename><surname>Herzer</surname></persName><email>r.herzer@gns.cri.nz</email><affiliation>GNS Science, PO Box 30368, Lower Hutt 5040,, New Zealand</affiliation></author><author xml:id="author-2"><persName><forename type="first">D. H. N.</forename><surname>Barker</surname></persName><affiliation>GNS Science, PO Box 30368, Lower Hutt 5040,, New Zealand</affiliation></author><author xml:id="author-3"><persName><forename type="first">W. R.</forename><surname>Roest</surname></persName><affiliation>Marine Geosciences Department, Ifremer, Centre de Bretagne, BP 70, F‐29280, Plouzané, France</affiliation></author><author xml:id="author-4"><persName><forename type="first">N.</forename><surname>Mortimer</surname></persName><affiliation>GNS Science, 9054, Private Bag 1930, Dunedin, New Zealand</affiliation></author></analytic><monogr><title level="j">Geochemistry, Geophysics, Geosystems</title><title level="j" type="abbrev">Geochem. Geophys. Geosyst.</title><idno type="pISSN">1525-2027</idno><idno type="eISSN">1525-2027</idno><idno type="DOI">10.1002/(ISSN)1525-2027</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2011-02"></date><biblScope unit="volume">12</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="/">n/a</biblScope><biblScope unit="page" to="/">n/a</biblScope></imprint></monogr><idno type="istex">D68737AF9CBF523EF8D9753700B8D3F7CAB4B551</idno><idno type="DOI">10.1029/2010GC003291</idno><idno type="ArticleID">2010GC003291</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2011</date></creation><langUsage><language ident="en">en</language></langUsage><abstract><p>A tectonic model of the evolution of the northern half of the South Fiji Basin, including the Minerva Triple Junction and Cook Fracture Zone, is developed from regional gravity, multibeam bathymetry, and a new interpretation of magnetic anomalies pinned to radiometric dates of oceanic crust in the basin. The geometry and age of a portion of the Minerva Triple Junction and the Cook‐Minerva spreading center (the connection from the triple junction to the Cook Fracture Zone, which accommodated coeval opening of the Norfolk Basin), are resolved with multibeam bathymetry and magnetics. The South Fiji Basin opened from about 34 to 15 Ma in an anticlockwise sweep about an Euler pole located at the northern end of the present Lau Ridge. This rotation and a rigidly straight southeastward motion of the Three Kings Ridge were accommodated by the configuration of the triple junction changing from ridge‐fault‐fault to ridge‐ridge‐fault to ridge‐ridge‐ridge. During this evolution the southeastern arm of the system, the Julia Fracture Zone, underwent several transformations and the Cook‐Minerva spreading center experienced repeated ridge jumps. The kinematics of the northern South Fiji Basin dictate, to a large extent, the evolution of the southern South Fiji Basin and the Norfolk Basin. This in turn leads to the interpretation of a complex trench‐trench‐double transform fault framework at the northern New Zealand margin, which explains most aspects of the geology, structure, and arc volcanic history of the margin and provides a radical new setting for the origin of the Northland Allochthon.</p></abstract><textClass><keywords scheme="keyword"><list><head>keywords</head><item><term>South Fiji Basin</term></item><item><term>back‐arc basin evolution</term></item><item><term>multibeam bathymetry</term></item><item><term>magnetic anomalies</term></item><item><term>gravity model</term></item><item><term>New Zealand plate boundary</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>index-terms</head><item><term>GEOMAGNETISM AND PALEOMAGNETISM</term></item><item><term>Spatial variations attributed to seafloor spreading</term></item><item><term>MARINE GEOLOGY AND GEOPHYSICS</term></item><item><term>Back‐arc basin processes</term></item><item><term>Marine magnetics and paleomagnetics</term></item><item><term>Plate tectonics</term></item><item><term>Plate tectonics</term></item><item><term>TECTONOPHYSICS</term></item><item><term>Plate motions: past</term></item><item><term>Plate boundary: general</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2010-07-08">Received</change><change when="2010-11-29">Registration</change><change when="2011-02">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/D68737AF9CBF523EF8D9753700B8D3F7CAB4B551/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="ggge1838"><header><publicationMeta level="product"><doi>10.1002/(ISSN)1525-2027</doi><issn type="print">1525-2027</issn><issn type="electronic">1525-2027</issn><idGroup><id type="product" value="GGGE"></id><id type="coden" value="GGGGFR"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS">Geochemistry, Geophysics, Geosystems</title><title type="short">Geochem. 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The geometry and age of a portion of the Minerva Triple Junction and the Cook‐Minerva spreading center (the connection from the triple junction to the Cook Fracture Zone, which accommodated coeval opening of the Norfolk Basin), are resolved with multibeam bathymetry and magnetics. The South Fiji Basin opened from about 34 to 15 Ma in an anticlockwise sweep about an Euler pole located at the northern end of the present Lau Ridge. This rotation and a rigidly straight southeastward motion of the Three Kings Ridge were accommodated by the configuration of the triple junction changing from ridge‐fault‐fault to ridge‐ridge‐fault to ridge‐ridge‐ridge. During this evolution the southeastern arm of the system, the Julia Fracture Zone, underwent several transformations and the Cook‐Minerva spreading center experienced repeated ridge jumps. The kinematics of the northern South Fiji Basin dictate, to a large extent, the evolution of the southern South Fiji Basin and the Norfolk Basin. This in turn leads to the interpretation of a complex trench‐trench‐double transform fault framework at the northern New Zealand margin, which explains most aspects of the geology, structure, and arc volcanic history of the margin and provides a radical new setting for the origin of the Northland Allochthon.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Oligocene‐Miocene spreading history of the northern South Fiji Basin and implications for the evolution of the New Zealand plate boundary</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>BACK‐ARC SPREADING SOUTH FIJI BASIN</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Oligocene‐Miocene spreading history of the northern South Fiji Basin and implications for the evolution of the New Zealand plate boundary</title></titleInfo><name type="personal"><namePart type="given">R. 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Mortimer (2011), Oligocene‐Miocene spreading history of the northern South Fiji Basin and implications for the evolution of the New Zealand plate boundary, Geochem. Geophys. Geosyst., 12, Q02004, doi:10.1029/2010GC003291.</edition><copyrightDate encoding="w3cdtf">2011</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">10700</extent></physicalDescription><abstract>A tectonic model of the evolution of the northern half of the South Fiji Basin, including the Minerva Triple Junction and Cook Fracture Zone, is developed from regional gravity, multibeam bathymetry, and a new interpretation of magnetic anomalies pinned to radiometric dates of oceanic crust in the basin. The geometry and age of a portion of the Minerva Triple Junction and the Cook‐Minerva spreading center (the connection from the triple junction to the Cook Fracture Zone, which accommodated coeval opening of the Norfolk Basin), are resolved with multibeam bathymetry and magnetics. The South Fiji Basin opened from about 34 to 15 Ma in an anticlockwise sweep about an Euler pole located at the northern end of the present Lau Ridge. This rotation and a rigidly straight southeastward motion of the Three Kings Ridge were accommodated by the configuration of the triple junction changing from ridge‐fault‐fault to ridge‐ridge‐fault to ridge‐ridge‐ridge. During this evolution the southeastern arm of the system, the Julia Fracture Zone, underwent several transformations and the Cook‐Minerva spreading center experienced repeated ridge jumps. The kinematics of the northern South Fiji Basin dictate, to a large extent, the evolution of the southern South Fiji Basin and the Norfolk Basin. This in turn leads to the interpretation of a complex trench‐trench‐double transform fault framework at the northern New Zealand margin, which explains most aspects of the geology, structure, and arc volcanic history of the margin and provides a radical new setting for the origin of the Northland Allochthon.</abstract><subject><genre>keywords</genre><topic>South Fiji Basin</topic><topic>back‐arc basin evolution</topic><topic>multibeam bathymetry</topic><topic>magnetic anomalies</topic><topic>gravity model</topic><topic>New Zealand plate boundary</topic></subject><relatedItem type="host"><titleInfo><title>Geochemistry, Geophysics, Geosystems</title></titleInfo><titleInfo type="abbreviated"><title>Geochem. Geophys. Geosyst.</title></titleInfo><genre type="journal">journal</genre><subject><genre>index-terms</genre><topic authorityURI="http://psi.agu.org/taxonomy5/1500">GEOMAGNETISM AND PALEOMAGNETISM</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1550">Spatial variations attributed to seafloor spreading</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3000">MARINE GEOLOGY AND GEOPHYSICS</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3001">Back‐arc basin processes</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3005">Marine magnetics and paleomagnetics</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3040">Plate tectonics</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3040">Plate tectonics</topic><topic authorityURI="http://psi.agu.org/taxonomy5/8100">TECTONOPHYSICS</topic><topic authorityURI="http://psi.agu.org/taxonomy5/8157">Plate motions: past</topic><topic authorityURI="http://psi.agu.org/taxonomy5/8150">Plate boundary: general</topic></subject><identifier type="ISSN">1525-2027</identifier><identifier type="eISSN">1525-2027</identifier><identifier type="DOI">10.1002/(ISSN)1525-2027</identifier><identifier type="CODEN">GGGGFR</identifier><identifier type="PublisherID">GGGE</identifier><part><date>2011</date><detail type="volume"><caption>vol.</caption><number>12</number></detail><detail type="issue"><caption>no.</caption><number>2</number></detail><extent unit="pages"><start>n/a</start><end>n/a</end><total>20</total></extent></part></relatedItem><identifier type="istex">D68737AF9CBF523EF8D9753700B8D3F7CAB4B551</identifier><identifier type="DOI">10.1029/2010GC003291</identifier><identifier type="ArticleID">2010GC003291</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright 2011 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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