Please use this identifier to cite or link to this item: https://hdl.handle.net/1959.11/27481
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dc.contributor.authorReagan, M Ken
dc.contributor.authorPearce, J Aen
dc.contributor.authorPetronotis, Ken
dc.contributor.authorAlmeev, Ren
dc.contributor.authorAvery, A Aen
dc.contributor.authorCarvallo, Cen
dc.contributor.authorChapman, Ten
dc.contributor.authorChristeson, G Len
dc.contributor.authorFerre, E Cen
dc.contributor.authorGodard, Men
dc.contributor.authorHeaton, D Een
dc.contributor.authorKirchenbaur, Men
dc.contributor.authorKurz, Wen
dc.contributor.authorKutterolf, Sen
dc.contributor.authorLi, H Yen
dc.contributor.authorLi, Yen
dc.contributor.authorMichibayashi, Ken
dc.contributor.authorMorgan, Sen
dc.contributor.authorNelson, W Ren
dc.contributor.authorPrytulak, Jen
dc.contributor.authorPython, Men
dc.contributor.authorRobertson, A H Fen
dc.contributor.authorRyan, J Gen
dc.contributor.authorSager, W Wen
dc.contributor.authorSakuyama, Ten
dc.contributor.authorShervais, J Wen
dc.contributor.authorShimizu, Ken
dc.contributor.authorWhattam, S Aen
dc.date.accessioned2019-08-27T00:12:15Z-
dc.date.available2019-08-27T00:12:15Z-
dc.date.issued2015-09-29-
dc.identifier.citationProceedings of the International Ocean Discovery Program, v.352, p. 1-49en
dc.identifier.issn2377-3189en
dc.identifier.urihttps://hdl.handle.net/1959.11/27481-
dc.description.abstractAccording to the Stern and Bloomer (1992) hypothesis being tested, the Izu-Bonin-Mariana (IBM) fore arc formed during the period of seafloor spreading that accompanied the rapid rollback and sinking of the newly subducting plate immediately following subduction initiation. According to the related hypothesis of Reagan et al. (2010), the deepest volcanic rocks should primarily be fore-arc basalt (FAB), a distinctive type of volcanic rock recovered during dredging and submersible sampling of the IBM fore arc. Both hypotheses predict that FAB is underlain by sheeted dikes, as these are characteristic of crust accreted during seafloor spreading at all but the slowest spreading rates. Reconstruction of the IBM volcanic stratigraphy also provides evidence for the inference that the FAB should be overlain by the initial products of arc volcanism, specifically by Lavas with compositions that are transitional between FAB and boninite; Boninite lavas themselves; and finally, Members of the tholeiitic and calc-alkaline series typical of “normal” island arcs (Ishizuka et al., 2011). Drilling at this site provides an important test of the lower part of this sequence.en
dc.languageenen
dc.publisherInternational Ocean Discovery Programen
dc.relation.ispartofProceedings of the International Ocean Discovery Programen
dc.relation.isversionof1en
dc.rightsAttribution 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.titleSite U1440en
dc.typeBook Chapteren
dc.identifier.doi10.14379/iodp.proc.352.104.2015en
dcterms.accessRightsGolden
local.contributor.firstnameM Ken
local.contributor.firstnameJ Aen
local.contributor.firstnameKen
local.contributor.firstnameRen
local.contributor.firstnameA Aen
local.contributor.firstnameCen
local.contributor.firstnameTen
local.contributor.firstnameG Len
local.contributor.firstnameE Cen
local.contributor.firstnameMen
local.contributor.firstnameD Een
local.contributor.firstnameMen
local.contributor.firstnameWen
local.contributor.firstnameSen
local.contributor.firstnameH Yen
local.contributor.firstnameYen
local.contributor.firstnameKen
local.contributor.firstnameSen
local.contributor.firstnameW Ren
local.contributor.firstnameJen
local.contributor.firstnameMen
local.contributor.firstnameA H Fen
local.contributor.firstnameJ Gen
local.contributor.firstnameW Wen
local.contributor.firstnameTen
local.contributor.firstnameJ Wen
local.contributor.firstnameKen
local.contributor.firstnameS Aen
local.relation.isfundedbyARCen
local.subject.for2008040304 Igneous and Metamorphic Petrologyen
local.subject.for2008040202 Inorganic Geochemistryen
local.subject.seo2008970104 Expanding Knowledge in the Earth Sciencesen
local.profile.schoolSchool of Environmental and Rural Scienceen
local.profile.emailtchapm21@une.edu.auen
local.output.categoryB1en
local.grant.numberLE140100047en
local.record.placeauen
local.record.institutionUniversity of New Englanden
local.publisher.placeTexas, United States of Americaen
local.identifier.totalchapters6en
local.format.startpage1en
local.format.endpage49en
local.series.issn2377-3189en
local.peerreviewedYesen
local.identifier.volume352en
local.access.fulltextYesen
local.contributor.lastnameReaganen
local.contributor.lastnamePearceen
local.contributor.lastnamePetronotisen
local.contributor.lastnameAlmeeven
local.contributor.lastnameAveryen
local.contributor.lastnameCarvalloen
local.contributor.lastnameChapmanen
local.contributor.lastnameChristesonen
local.contributor.lastnameFerreen
local.contributor.lastnameGodarden
local.contributor.lastnameHeatonen
local.contributor.lastnameKirchenbauren
local.contributor.lastnameKurzen
local.contributor.lastnameKutterolfen
local.contributor.lastnameLien
local.contributor.lastnameLien
local.contributor.lastnameMichibayashien
local.contributor.lastnameMorganen
local.contributor.lastnameNelsonen
local.contributor.lastnamePrytulaken
local.contributor.lastnamePythonen
local.contributor.lastnameRobertsonen
local.contributor.lastnameRyanen
local.contributor.lastnameSageren
local.contributor.lastnameSakuyamaen
local.contributor.lastnameShervaisen
local.contributor.lastnameShimizuen
local.contributor.lastnameWhattamen
dc.identifier.staffune-id:tchapm21en
local.profile.orcid0000-0002-4821-6420en
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local.identifier.unepublicationidune:1959.11/27481en
dc.identifier.academiclevelAcademicen
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local.title.maintitleSite U1440en
local.relation.fundingsourcenoteNational Science Foundation (NSF), United States; Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan; European Consortium for Ocean Research Drilling (ECORD); Ministry of Science and Technology (MOST), People’s Republic of China; Korea Institute of Geoscience and Mineral Resources (KIGAM); GNS Science, New Zealand; Australian/New Zealand Consortium (ANZIC); Ministry of Earth Sciences (MoES), India; Coordination for Improvement of Higher Education Personnel, Brazil (CAPES)en
local.output.categorydescriptionB1 Chapter in a Scholarly Booken
local.relation.grantdescriptionARC/LE140100047en
local.search.authorReagan, M Ken
local.search.authorPearce, J Aen
local.search.authorPetronotis, Ken
local.search.authorAlmeev, Ren
local.search.authorAvery, A Aen
local.search.authorCarvallo, Cen
local.search.authorChapman, Ten
local.search.authorChristeson, G Len
local.search.authorFerre, E Cen
local.search.authorGodard, Men
local.search.authorHeaton, D Een
local.search.authorKirchenbaur, Men
local.search.authorKurz, Wen
local.search.authorKutterolf, Sen
local.search.authorLi, H Yen
local.search.authorLi, Yen
local.search.authorMichibayashi, Ken
local.search.authorMorgan, Sen
local.search.authorNelson, W Ren
local.search.authorPrytulak, Jen
local.search.authorPython, Men
local.search.authorRobertson, A H Fen
local.search.authorRyan, J Gen
local.search.authorSager, W Wen
local.search.authorSakuyama, Ten
local.search.authorShervais, J Wen
local.search.authorShimizu, Ken
local.search.authorWhattam, S Aen
local.uneassociationUnknownen
local.atsiresearchNoen
local.isrevisionNoen
local.sensitive.culturalNoen
local.year.published2015en
local.fileurl.closedpublishedhttps://rune.une.edu.au/web/retrieve/4efb48f3-0e15-48f6-a2bd-f03b51b7f8feen
local.subject.for2020370503 Igneous and metamorphic petrologyen
local.subject.for2020370302 Inorganic geochemistryen
local.subject.seo2020280107 Expanding knowledge in the earth sciencesen
local.relation.worldcathttp://www.worldcat.org/oclc/1076629862en
Appears in Collections:Book Chapter
School of Environmental and Rural Science
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