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<datestamp>2018-01-11</datestamp>
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<title lang=en>Strain Localization in Pyroxenite by Reaction-Enhanced Softening in the Shallow Subcontinental Lithospheric Mantle</title>
<creator>Hidas, Karoly</creator>
<creator>Garrido, Carlos J.</creator>
<creator>TOMMASI, Andréa</creator>
<creator>Padron-Navarta, Jose Alberto</creator>
<creator>Thielmann, Marcel</creator>
<creator>Konc, Zoltan</creator>
<creator>FRETS, Erwin</creator>
<creator>Marchesi, Claudio</creator>
<contributor>Instituto Andaluz de Ciencias de la Tierra (IACT) ; Universidad de Granada (UGR) - Consejo Superior de Investigaciones Científicas [Spain] (CSIC)</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>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>Institut für Geophysik [Zürich] ; Eidgenössische Technische Hochschule [Zürich] (ETH Zürich)</contributor>
<description>International audience</description>
<source>ISSN: 0022-3530</source>
<source>EISSN: 1460-2415</source>
<source>Journal of Petrology</source>
<publisher>Oxford University Press (OUP)</publisher>
<identifier>hal-00941293</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00941293</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00941293</source>
<source>Journal of Petrology, Oxford University Press (OUP), 2013, 54 (10), pp.1997-2031. 〈10.1093/petrology/egt039〉</source>
<identifier>DOI : 10.1093/petrology/egt039</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1093/petrology/egt039</relation>
<language>en</language>
<subject lang=en>mylonite shear zone</subject>
<subject lang=en>pyroxenite</subject>
<subject lang=en>Ronda Peridotite massif</subject>
<subject lang=en>strain localization</subject>
<subject lang=en>synkinematic reaction</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 report structural evidence of ductile strain localization in mantle pyroxenite from the spinel to plagioclase websterite transition in the Ronda Peridotite (southern Spain). Mapping shows that, in this domain, small-scale shear zones occurring at the base of the lithospheric section are systematically located within thin pyroxenite layers, suggesting that the pyroxenite was locally weaker than the host peridotite. Strain localization is associated with a sudden decrease of grain size and increasing volume fractions of plagioclase and amphibole as a result of a spinel to plagioclase phase transformation reaction during decompression. This reaction also fostered hydrogen extraction ('dehydroxylation') from clinopyroxene producing effective fluid saturation that catalyzed the synkinematic net-transfer reaction. This reaction produced fine-grained olivine and plagioclase, allowing the onset of grain-size sensitive creep and further strain localization in these pyroxenite bands. The strain localization in the pyroxenites is thus explained by their more fertile composition, which allowed earlier onset of the phase transition reactions. Geothermobarometry undertaken on compositionally zoned constituent minerals suggests that this positive feedback between reactions and deformation is associated with cooling from at least 1000°C to 700°C and decompression from 1*0 to 0*5 GPa.</description>
<date>2013-10</date>
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