untitled
<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd>
<responseDate>2018-01-17T12:15:58Z</responseDate>
<request identifier=oai:HAL:hal-01685628v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request>
<GetRecord>
<record>
<header>
<identifier>oai:HAL:hal-01685628v1</identifier>
<datestamp>2018-01-17</datestamp>
<setSpec>type:ART</setSpec>
<setSpec>subject:sdu</setSpec>
<setSpec>subject:sde</setSpec>
<setSpec>collection:CNRS</setSpec>
<setSpec>collection:UNIV-AG</setSpec>
<setSpec>collection:SDE</setSpec>
<setSpec>collection:MNHN</setSpec>
<setSpec>collection:ALLINSP</setSpec>
<setSpec>collection:GM</setSpec>
<setSpec>collection:UPMC</setSpec>
<setSpec>collection:AGROPOLIS</setSpec>
<setSpec>collection:GIP-BE</setSpec>
<setSpec>collection:IMPMC</setSpec>
<setSpec>collection:B3ESTE</setSpec>
<setSpec>collection:UNIV-MONTPELLIER</setSpec>
<setSpec>collection:INSU</setSpec>
</header>
<metadata><dc>
<publisher>HAL CCSD</publisher>
<title lang=en>Subduction initiation and ophiolite crust: new insights from IODP drilling</title>
<creator>Reagan, Mark K.</creator>
<creator>Pearce, Julian a.</creator>
<creator>Petronotis, Katerina</creator>
<creator>Almeev, Renat R.</creator>
<creator>Avery, Aaron j.</creator>
<creator>Carvallo, C.</creator>
<creator>Chapman, Timothy</creator>
<creator>Christeson, Gail l.</creator>
<creator>Ferre, Eric c.</creator>
<creator>GODARD, Marguerite</creator>
<creator>Heaton, Daniel e.</creator>
<creator>Kirchenbaur, Maria</creator>
<creator>Kurz, Walter</creator>
<creator>Kutterolf, Steffen</creator>
<creator>Li, Hongyan</creator>
<creator>Li, Yibing</creator>
<creator>Michibayashi, Katsuyoshi</creator>
<creator>Morgan, Sally</creator>
<creator>Nelson, Wendy R.</creator>
<creator>Prytulak, Julie</creator>
<creator>Python, Marie</creator>
<creator>Robertson, Alastair h. f.</creator>
<creator>Ryan, Jeffrey g.</creator>
<creator>Sager, William w.</creator>
<creator>Sakuyama, Tetsuya</creator>
<creator>Shervais, John w.</creator>
<creator>Shimizu, Kenji</creator>
<creator>Whattam, Scott a.</creator>
<contributor>University of Iowa [Iowa]</contributor>
<contributor>Cardiff University</contributor>
<contributor>A&M University, College Station</contributor>
<contributor>Institut fur Mineralogy, Hannovre</contributor>
<contributor>Florida State University</contributor>
<contributor>Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC) ; Muséum National d'Histoire Naturelle (MNHN) - Université Pierre et Marie Curie - Paris 6 (UPMC) - Institut de recherche pour le développement [IRD] : UR206 - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>University of Sydney</contributor>
<contributor>University of Texas</contributor>
<contributor>Southern Illinois University</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Oregon State University</contributor>
<contributor>Universitat Koln</contributor>
<contributor>University of Edinburgh</contributor>
<contributor>Guangzhou Institute of Geochemistry</contributor>
<contributor>Institute of geology, Beijing</contributor>
<contributor>Shizuoka University</contributor>
<contributor>University of Leicester</contributor>
<contributor>Towson University</contributor>
<contributor>Imperial College London</contributor>
<contributor>Hokkaido University</contributor>
<contributor>University of south Florida</contributor>
<contributor>University of Houston</contributor>
<contributor>Osaka University</contributor>
<contributor>Utah State University</contributor>
<contributor>JAMSTEC</contributor>
<contributor>Korea University, Seoul</contributor>
<description>International audience</description>
<source>ISSN: 0020-6814</source>
<source>International Geology Review</source>
<publisher>Taylor & Francis</publisher>
<identifier>hal-01685628</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01685628</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01685628</source>
<source>International Geology Review, Taylor & Francis, 2017, 59 (11), pp.1439-1450. 〈10.1080/00206814.2016.1276482〉</source>
<identifier>DOI : 10.1080/00206814.2016.1276482</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1080/00206814.2016.1276482</relation>
<language>en</language>
<subject lang=en>boninite</subject>
<subject lang=en>Izu-Bonin</subject>
<subject lang=en>basalt</subject>
<subject lang=en>drilling</subject>
<subject lang=en>International Ocean Discovery Program</subject>
<subject lang=en>Expedition 352</subject>
<subject lang=en>Site U1439</subject>
<subject lang=en>Site U1440</subject>
<subject lang=en>Site U1441</subject>
<subject lang=en>Site U1442</subject>
<subject lang=en>ophiolite</subject>
<subject lang=en>subduction initiation</subject>
<subject lang=en>Philippine plate</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>nternational Ocean Discovery Program (IODP) Expedition 352 recovered a high-fidelity record of volcanism related to subduction initiation in the Bonin fore-arc. Two sites (U1440 and U1441) located in deep water nearer to the trench recovered basalts and related rocks; two sites (U1439 and U1442) located in shallower water further from the trench recovered boninites and related rocks. Drilling in both areas ended in dolerites inferred to be sheeted intrusive rocks. The basalts apparently erupted immediately after subduction initiation and have compositions similar to those of the most depleted basalts generated by rapid sea-floor spreading at mid-ocean ridges, with little or no slab input. Subsequent melting to generate boninites involved more depleted mantle and hotter and deeper subducted components as subduction progressed and volcanism migrated away from the trench. This volcanic sequence is akin to that recorded by many ophiolites, supporting a direct link between subduction initiation, fore-arc spreading, and ophiolite genesis.</description>
<date>2017</date>
</dc>
</metadata>
</record>
</GetRecord>
</OAI-PMH>
