georefid:2012-047433SEDIS Publication Catalogue
ana.macario@awi.de
http://sedis.iodp.org/pub-catalogue/informationpointOfContact2013-07-08T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1007/s00410-011-0680-x<gco:CharacterString>The early Miocene ( approximately 25 Ma) volcanism in the northern Kyushu-Palau Ridge, enriched mantle source injection during rifting prior to the Shikoku back-arc basin opening</gco:CharacterString>2012-01-01publicationgeorefid:2012-047433doi:10.1007/s00410-011-0680-xHaraguchi, SatoruUniversity of Tokyo, Atmosphere and Ocean Research Institute, Kashiwa, JapanauthorIshii, TeruakiFukada Geological Institute, JapanauthorKimura, Jun-IchiJapan Agency for Marine Earth Science and Technology, JapanauthorKato, YasuhiroauthorSpringer International, Heidelberg - New York, InternationalpublisherdocumentHardcopyContributions to Mineralogy and Petrology163 (3)483-504The northern Kyushu-Palau Ridge (KPR), remnant conjugate arc of the Izu-Ogasawara (Bonin)-Mariana (IBM) active arc, is dominated by basalt-andesite except for the Komahashi-Daini Seamount where acidic plutonic rocks of 38 Ma were recovered. These mafic to intermediate volcanics are produced by the rifting volcanism in the proto-IBM arc associated with spreading of the Shikoku Basin. The HFSE and HREE contents and ratios of these volcanics indicate enriched source mantle composition compared to recent volcanic front. The LILE ratios exhibit similar characteristics to reararc volcanism of the recent Izu arc, and some enriched volcanics exhibit high abundance of sediment melt inputs. Based on these observations and compilations of the published data set, the replacement event of the wedge mantle under the IBM arc occurred two times. The first event occurred between 45 and 38 Ma, with Pacific type mantle being replaced by depleted Indian type mantle. The second event occurred between 36 and 25 Ma, enriched mantle flowed from reararc side. The slab component during the proto-IBM arc rifting was a similar characteristic to recent reararc volcanism of the Izu arc, and sediment melt added in a local area. Copyright 2011 Springer-VerlagcompletedIgneous and metamorphic petrologySolid-earth geophysicsandesitesback-arc basinsbasaltsbasinsCenozoicchemical compositionenrichmentgeochemistryICP mass spectraigneous rocksIzu-Bonin ArcKomahashi-Daini SeamountKyushu-Palau RidgeLeg 126lithophile elementslithospherelower Miocenemajor elementsmantlemantle wedgesmass spectrametasomatismmid-ocean ridge basaltsMioceneNeogeneNorth PacificNorthwest PacificOcean Drilling Programocean floorsoceanic lithosphereODP Site 793Pacific OceanParece Vela BasinpetrologyPhilippine SeaPhilippine Sea Plateplate tectonicsplutonic rocksrift zonesriftingsea-floor spreadingseamountsShikoku Basinspectraspreading centersTertiarytrace elementsvolcanic rocksvolcanismWest PacificX-ray fluorescence spectraurn:org.iodp:exp:126urnlargerWorkCitationcampaignurn:org.iodp:exp:126:site:793urnlargerWorkCitationstudyurn:org.iodp:exp:126urnlargerWorkCitationcampaignEnglishgeoscientificInformation134.0000140.521711.000031.0621Kyushu-Palau RidgeIncludes appendices