RechercherTitres

untitled
<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T15:42:09Z</responseDate> <request identifier=oai:HAL:hal-00405803v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00405803v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Oligocene-Miocene tectonic evolution of the South Fiji Basin and Northland Plateau, SW Pacific Ocean: Evidence from. petrology and dating of dredged rocks</title> <creator>Mortimer, N.</creator> <creator>Herzer, R. H.</creator> <creator>Gans, P. B.</creator> <creator>Laporte-Magoni, C.</creator> <creator>Calvert, A. T.</creator> <creator>Bosch, Delphine</creator> <contributor>GNS Science, Private Bag 1930, Dunedin ; Université du Québec</contributor> <contributor>GNS Science, PO Box 30368, Lower Hutt ; Université du Québec</contributor> <contributor>Department of Geological Sciences, University of California, Santa Barbara ; Université du Québec</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> <source>ISSN: 0025-3227</source> <source>Marine Geology</source> <publisher>Elsevier</publisher> <identifier>hal-00405803</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00405803</identifier> <source>https://hal.archives-ouvertes.fr/hal-00405803</source> <source>Marine Geology, Elsevier, 2007, 237 (1-2), pp.1-24. 〈10.1016/j.margeo.2006.10.033〉</source> <identifier>DOI : 10.1016/j.margeo.2006.10.033</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.margeo.2006.10.033</relation> <language>en</language> <subject lang=en>petrology</subject> <subject lang=en>geochemistry</subject> <subject lang=en>geochronology</subject> <subject lang=en>subduction</subject> <subject lang=en>back-arc basins</subject> <subject lang=en>shoshonite</subject> <subject lang=en>South Fiji Basin</subject> <subject lang=en>New Zealand</subject> <subject>[SDU.STU.PE] Sciences of the Universe [physics]/Earth Sciences/Petrography</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>We present new analytical data from lavas and associated rocks dredged and/or drilled from the South Fiji Basin, Northland Plateau, Colville Ridge and Havre Trough. These results provide much-needed ground truth about the geology, age and tectonic evolution of the Cenozoic submarine ridges and basins between the active intraoceanic Tonga–Kermadec arc, and rifted continental borderlands of New Zealand, the Norfolk Ridge and New Caledonia. Key results from this study include: (1) Ar–Ar dates on Minerva Abyssal Plain oceanic crust suggest that the ages of magnetic anomalies in the South Fiji Basin have been overestimated by earlier workers; (2) subduction-related lavas are widespread across the region, are not presently organised into arc-like chains, and cluster in the age range 22–18 Ma (Early Miocene); (3) the oldest subduction-related lavas occur in the western part of the region (32–26 Ma: Norfolk and Three Kings Ridge); (4) shoshonites, interpreted as rifted arc lavas, were erupted in a narrow 20–21 Ma interval over a wide area. Put together, these results indicate high magmatic flux and large and rapid horizontal tectonic translations and basin opening from 18–23 Ma in the region immediately north of New Zealand. We explain the Miocene tectonomagmatic development of the region by a model of rapid rollback of a single, east-facing Pacific arc–trench system that became established after Northland Allochthon emplacement. Critical testing of this, versus other, tectonic models must await drilling and dating of thus-far unsampled Kupe Abyssal Plain crust.</description> <date>2007</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>