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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T18:33:54Z</responseDate> <request identifier=oai:HAL:hal-00858243v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00858243v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:phys</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Scientific Drilling and Related Research in the Samail Ophiolite, Sultanate of Oman</title> <creator>Kelemen, Peter</creator> <creator>Rajhi, A.A.</creator> <creator>Godard, Marguerite</creator> <creator>Ildefonse, Benoit</creator> <creator>Koepke, J.</creator> <creator>Macleod, Christopher J.</creator> <creator>Manning, C.</creator> <creator>Michibayashi, K.</creator> <creator>Nasir, S.</creator> <creator>Shock, E.</creator> <creator>Takazawa, Eiichi</creator> <creator>Teagle, Damon</creator> <contributor>Lamont-Doherty Earth Observatory (LDEO) ; Columbia University [New York]</contributor> <contributor>Department of Earth and Environmental Sciences [Columbia] (EESC) ; Columbia University [New York]</contributor> <contributor>Manteau et Interfaces ; 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) - 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>Institut für Mineralogie [Hannover] ; Leibniz Universität Hannover [Hannover] (LUH)</contributor> <contributor>School of Earth and Ocean Sciences [Cardiff] ; Cardiff University [Cardiff]</contributor> <contributor>Institute of Geosciences [Shizuoka] ; University of Shizuoka</contributor> <contributor>Niigata University</contributor> <contributor>National Oceanography Centre [Southampton] (NOC) ; University of Southampton [Southampton]</contributor> <source>ISSN: 1816-8957</source> <source>Scientific Drilling</source> <publisher>Copernicus Publications</publisher> <identifier>hal-00858243</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00858243</identifier> <source>https://hal.archives-ouvertes.fr/hal-00858243</source> <source>Scientific Drilling, Copernicus Publications, 2011, 15, pp.64-71. 〈10.2204/iodp.sd.15.10.2013〉</source> <identifier>DOI : 10.2204/iodp.sd.15.10.2013</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.2204/iodp.sd.15.10.2013</relation> <language>en</language> <subject lang=en>Scientific Drilling</subject> <subject lang=en>Samail ophiolite</subject> <subject lang=en>Oman</subject> <subject>[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]</subject> <subject>[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]</subject> <subject>[SDE.MCG] Environmental Sciences/Global Changes</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>This workshop report describes plans for scientific drilling in the Samail ophiolite in Oman in the context of past, current, and future research. Long-standing plans to study formation and evolution of the Samail crust and upper mantle, involving igneous and metamorphic processes at an oceanic spreading center, have been augmented by recent interest in ongoing, low temperature processes. These include alteration and weathering, and the associated sub-surface biosphere supported by chemical potential energy due to disequilibrium between mantle peridotite and water near the surface. This interest is motivated in part by the possibility of geological carbon capture and storage via engineered, accelerated mineral carbonation in Oman.</description> <date>2011-03-01</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>