The Tonga-Kermadec arc and Havre-Lau back-arc system : Their role in the development of tectonic and magmatic models for the western Pacific
Identifieur interne : 000194 ( PascalFrancis/Checkpoint ); précédent : 000193; suivant : 000195The Tonga-Kermadec arc and Havre-Lau back-arc system : Their role in the development of tectonic and magmatic models for the western Pacific
Auteurs : Ian E. M. Smith [Nouvelle-Zélande] ; Richard C. Price [Nouvelle-Zélande]Source :
- Journal of volcanology and geothermal research [ 0377-0273 ] ; 2006.
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- Pascal (Inist)
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Abstract
The convergent plate boundary marked by the Tonga-Kermadec arc system is one of the clearest examples of an intra-oceanic arc on the modem Earth. Arising from ground breaking research in the 1970's and continuing through the present, the arc has become a testing ground for defining and explaining models for the tectonic and magmatic evolution of intra-oceanic subduction systems. Despite its simple oceanic setting the arc shows significant variations along its length in terms of rock types and structure and because of the lack of involvement of continental crust these allow refinement of the details of or models of how arcs develop and evolve. Of particular importance are the variations in convergence rates and vectors between the major plates and the effect these have on the tectonic evolution of the arc and back-arc. The erupted rocks of the arc have provided the means of testing the contribution of subducted sediment, slab, mantle wedge and overlying crust and most recently tests of P-T-time paths for recycled sediments. Although the arc is dominated by basalts and basaltic andesites, there is increasing evidence for significant proportions of silicic magmas erupted in recent times. Silicic volcanism is also evidenced in the presence of caldera structures revealed by detailed multibeam mapping that have been a feature of research in the last decade. As we enter the 21st century, the Tonga-Kermadec arc continues as an archetypical natural laboratory for the testing of new ideas in subduction zone tectonics and petrology.
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<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">The Tonga-Kermadec arc and Havre-Lau back-arc system : Their role in the development of tectonic and magmatic models for the western Pacific</title><author><name sortKey="Smith, Ian E M" sort="Smith, Ian E M" uniqKey="Smith I" first="Ian E. M." last="Smith">Ian E. M. Smith</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Department of Geology, University of Auckland, PB92019</s1><s2>Auckland</s2><s3>NZL</s3><sZ>1 aut.</sZ></inist:fA14><country>Nouvelle-Zélande</country><wicri:noRegion>Auckland</wicri:noRegion></affiliation></author><author><name sortKey="Price, Richard C" sort="Price, Richard C" uniqKey="Price R" first="Richard C." last="Price">Richard C. Price</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>School of Science and Engineering, University of Waikato, PB3105</s1><s2>Hamilton</s2><s3>NZL</s3><sZ>2 aut.</sZ></inist:fA14><country>Nouvelle-Zélande</country><wicri:noRegion>Hamilton</wicri:noRegion></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">07-0186345</idno><date when="2006">2006</date><idno type="stanalyst">PASCAL 07-0186345 INIST</idno><idno type="RBID">Pascal:07-0186345</idno><idno type="wicri:Area/PascalFrancis/Corpus">000164</idno><idno type="wicri:Area/PascalFrancis/Curation">000171</idno><idno type="wicri:Area/PascalFrancis/Checkpoint">000194</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">The Tonga-Kermadec arc and Havre-Lau back-arc system : Their role in the development of tectonic and magmatic models for the western Pacific</title><author><name sortKey="Smith, Ian E M" sort="Smith, Ian E M" uniqKey="Smith I" first="Ian E. M." last="Smith">Ian E. M. Smith</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Department of Geology, University of Auckland, PB92019</s1><s2>Auckland</s2><s3>NZL</s3><sZ>1 aut.</sZ></inist:fA14><country>Nouvelle-Zélande</country><wicri:noRegion>Auckland</wicri:noRegion></affiliation></author><author><name sortKey="Price, Richard C" sort="Price, Richard C" uniqKey="Price R" first="Richard C." last="Price">Richard C. Price</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>School of Science and Engineering, University of Waikato, PB3105</s1><s2>Hamilton</s2><s3>NZL</s3><sZ>2 aut.</sZ></inist:fA14><country>Nouvelle-Zélande</country><wicri:noRegion>Hamilton</wicri:noRegion></affiliation></author></analytic><series><title level="j" type="main">Journal of volcanology and geothermal research</title><title level="j" type="abbreviated">J. volcanol. geotherm. res.</title><idno type="ISSN">0377-0273</idno><imprint><date when="2006">2006</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Journal of volcanology and geothermal research</title><title level="j" type="abbreviated">J. volcanol. geotherm. res.</title><idno type="ISSN">0377-0273</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Earth</term><term>Lau Basin</term><term>Tonga</term><term>basaltic andesite</term><term>basalts</term><term>calderas</term><term>continental crust</term><term>crust</term><term>magmas</term><term>mantle</term><term>models</term><term>plate boundaries</term><term>plates</term><term>refinement</term><term>slabs</term><term>subducted sediments</term><term>subduction</term><term>subduction zones</term><term>tectonics</term><term>testing</term><term>troughs</term><term>volcanism</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Tectonique</term><term>Modèle</term><term>Limite plaque</term><term>Planète Terre</term><term>Expérimentation</term><term>Subduction</term><term>Croûte continentale</term><term>Affinement</term><term>Plaque</term><term>Sédiment subducté</term><term>Dalle</term><term>Manteau</term><term>Croûte terrestre</term><term>Basalte</term><term>Andésite basaltique</term><term>Magma</term><term>Volcanisme</term><term>Caldeira</term><term>Zone subduction</term><term>Fossé</term><term>Iles Tonga</term><term>Bassin Lau</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The convergent plate boundary marked by the Tonga-Kermadec arc system is one of the clearest examples of an intra-oceanic arc on the modem Earth. Arising from ground breaking research in the 1970's and continuing through the present, the arc has become a testing ground for defining and explaining models for the tectonic and magmatic evolution of intra-oceanic subduction systems. Despite its simple oceanic setting the arc shows significant variations along its length in terms of rock types and structure and because of the lack of involvement of continental crust these allow refinement of the details of or models of how arcs develop and evolve. Of particular importance are the variations in convergence rates and vectors between the major plates and the effect these have on the tectonic evolution of the arc and back-arc. The erupted rocks of the arc have provided the means of testing the contribution of subducted sediment, slab, mantle wedge and overlying crust and most recently tests of P-T-time paths for recycled sediments. Although the arc is dominated by basalts and basaltic andesites, there is increasing evidence for significant proportions of silicic magmas erupted in recent times. Silicic volcanism is also evidenced in the presence of caldera structures revealed by detailed multibeam mapping that have been a feature of research in the last decade. As we enter the 21st century, the Tonga-Kermadec arc continues as an archetypical natural laboratory for the testing of new ideas in subduction zone tectonics and petrology.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0377-0273</s0></fA01><fA02 i1="01"><s0>JVGRDQ</s0></fA02><fA03 i2="1"><s0>J. volcanol. geotherm. res.</s0></fA03><fA05><s2>156</s2></fA05><fA06><s2>3-4</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>The Tonga-Kermadec arc and Havre-Lau back-arc system : Their role in the development of tectonic and magmatic models for the western Pacific</s1></fA08><fA09 i1="01" i2="1" l="ENG"><s1>Silicic Volcanism and Crustal Evolution in Oceanic Arcs</s1></fA09><fA11 i1="01" i2="1"><s1>SMITH (Ian E. M.)</s1></fA11><fA11 i1="02" i2="1"><s1>PRICE (Richard C.)</s1></fA11><fA12 i1="01" i2="1"><s1>TAMURA (Y.)</s1><s9>ed.</s9></fA12><fA12 i1="02" i2="1"><s1>WYSOCZANSKI (R.)</s1><s9>ed.</s9></fA12><fA14 i1="01"><s1>Department of Geology, University of Auckland, PB92019</s1><s2>Auckland</s2><s3>NZL</s3><sZ>1 aut.</sZ></fA14><fA14 i1="02"><s1>School of Science and Engineering, University of Waikato, PB3105</s1><s2>Hamilton</s2><s3>NZL</s3><sZ>2 aut.</sZ></fA14><fA15 i1="01"><s1>Institute for Research on Earth Evolution (IFREE), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-cho</s1><s2>Yokosuko, Kanagawa 237-0061</s2><s3>JPN</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></fA15><fA20><s1>315-331</s1></fA20><fA21><s1>2006</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>17236</s2><s5>354000142312200080</s5></fA43><fA44><s0>0000</s0><s1>© 2007 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>3 p.3/4</s0></fA45><fA47 i1="01" i2="1"><s0>07-0186345</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Journal of volcanology and geothermal research</s0></fA64><fA66 i1="01"><s0>NLD</s0></fA66><fC01 i1="01" l="ENG"><s0>The convergent plate boundary marked by the Tonga-Kermadec arc system is one of the clearest examples of an intra-oceanic arc on the modem Earth. Arising from ground breaking research in the 1970's and continuing through the present, the arc has become a testing ground for defining and explaining models for the tectonic and magmatic evolution of intra-oceanic subduction systems. Despite its simple oceanic setting the arc shows significant variations along its length in terms of rock types and structure and because of the lack of involvement of continental crust these allow refinement of the details of or models of how arcs develop and evolve. Of particular importance are the variations in convergence rates and vectors between the major plates and the effect these have on the tectonic evolution of the arc and back-arc. The erupted rocks of the arc have provided the means of testing the contribution of subducted sediment, slab, mantle wedge and overlying crust and most recently tests of P-T-time paths for recycled sediments. Although the arc is dominated by basalts and basaltic andesites, there is increasing evidence for significant proportions of silicic magmas erupted in recent times. Silicic volcanism is also evidenced in the presence of caldera structures revealed by detailed multibeam mapping that have been a feature of research in the last decade. As we enter the 21st century, the Tonga-Kermadec arc continues as an archetypical natural laboratory for the testing of new ideas in subduction zone tectonics and petrology.</s0></fC01><fC02 i1="01" i2="2"><s0>222A01</s0></fC02><fC02 i1="02" i2="2"><s0>001E01F01</s0></fC02><fC03 i1="01" i2="2" l="FRE"><s0>Tectonique</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="ENG"><s0>tectonics</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="SPA"><s0>Tectónico</s0><s5>01</s5></fC03><fC03 i1="02" i2="2" l="FRE"><s0>Modèle</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="ENG"><s0>models</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="SPA"><s0>Modelo</s0><s5>02</s5></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Limite plaque</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="ENG"><s0>plate boundaries</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="SPA"><s0>Límite placa</s0><s5>03</s5></fC03><fC03 i1="04" i2="2" l="FRE"><s0>Planète Terre</s0><s5>04</s5></fC03><fC03 i1="04" i2="2" l="ENG"><s0>Earth</s0><s5>04</s5></fC03><fC03 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M." last="Smith">Ian E. M. Smith</name></noRegion><name sortKey="Price, Richard C" sort="Price, Richard C" uniqKey="Price R" first="Richard C." last="Price">Richard C. Price</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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