Microstructures and seismic properties of south Patagonian mantle xenoliths (Gobernador Gregores and Pali Aike)

The subcontinental lithospheric mantle evolves through time due to tectonic events and processes as static recrystallization and melt percolation. To constrain the extent of these processes in the South Patagonian subcontinental mantle lithosphere we performed a microstructural and Electron Backscat...

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Autor principal: Zaffarana, C.
Otros Autores: Tommasi, A., Vauchez, A., Grégoire, M.
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Publicado: Elsevier 2014
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100 1 |a Zaffarana, C. 
245 1 0 |a Microstructures and seismic properties of south Patagonian mantle xenoliths (Gobernador Gregores and Pali Aike) 
260 |b Elsevier  |c 2014 
270 1 0 |m Zaffarana, C.; Geosciences Montpellier, CNRS and Université, Montpellier 2, F-34095 Montpellier, France; email: cbzaffarana@gmail.com 
506 |2 openaire  |e Política editorial 
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520 3 |a The subcontinental lithospheric mantle evolves through time due to tectonic events and processes as static recrystallization and melt percolation. To constrain the extent of these processes in the South Patagonian subcontinental mantle lithosphere we performed a microstructural and Electron Backscattered Diffraction (EBSD) study of a suite of 35 peridotite xenoliths brought to the surface by Plio-Pleistocene alkaline volcanic rocks from Gobernador Gregores and Pali Aike. All samples show a well-developed olivine and pyroxene crystallographic preferred orientation (CPO), consistent with deformation by dislocation creep with dominant activation of [100]{0kl} in olivine. The coarse granular or tabular textures and the low density of intracrystalline deformation features indicate that deformation was followed by annealing under static conditions. The xenoliths also show microstructural evidence of multiple episodes of reactive melt percolation. Neither annealing nor melt percolation erased the olivine CPO, which has [010]-fiber, [100]-fiber and orthorhombic patterns in Pali Aike xenoliths and essentially [010]-fiber and orthorhombic patterns in Gobernador Gregores xenoliths. Seismic properties calculated based on the CPO and modal compositions are, however, rather homogeneous, with fast S-wave polarization and P-wave propagation parallel to the [100] olivine axis. The variation in the olivine CPO solely changes the minimum S-wave birefringence direction, which is normal to the foliation for axial-[010] olivine CPO. Average samples for the two localities, obtained by adding up the individual samples CPO data in a common reference frame, show, however, a 'normal' upper mantle anisotropy with a maximum S-wave birrenfringence of ca. 5% at high angle to the both the maximum [010] and [100] axes concentrations, that is in the foliation, but normal to the lineation, and a minimum birefringence at low angle to the [100] maximum, that is parallel to the lineation. © 2014 Elsevier B.V.  |l eng 
536 |a Detalles de la financiación: Conseil Régional Languedoc-Roussillon 
536 |a Detalles de la financiación: University of Rochester 
536 |a Detalles de la financiación: Centre National de la Recherche Scientifique 
536 |a Detalles de la financiación: Institut National des Sciences de l'Univers, Centre National de la Recherche Scientifique 
536 |a Detalles de la financiación: Ministère de l'Enseignement Supérieur et de la Recherche 
536 |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas, A09U01 
536 |a Detalles de la financiación: D. Mainprice is thanked for discussions and for providing softwares for analyzing/plotting CPO data and seismic properties. We also thank two anonymous reviewers whose corrections greatly improved an earlier version of the manuscript. C. Nevado and D. Delmas supplied high quality polished thin sections for EBSD measurements. CZ postdoctoral stay at Geosciences Montpellier was funded by a Bernard Houssay scholarship funded by the Ministère de l'Enseignement Supérieur et de la Recherche, France and the CONICET, Argentina . The research leading to these results was partially funded by the Ecos Sud project A09U01 “Evolution de la texture et de l’anisotropie lors de la déformation haute température des roches et des métaux”. The EBSD-SEM national facility in Montpellier is supported by the Institut National de Sciences de l'Univers (INSU) du Centre National de la Recherche Scientifique (CNRS), France and by the Conseil Régional Languedoc-Roussillon, France . 
593 |a Geosciences Montpellier, CNRS and Université, Montpellier 2, F-34095 Montpellier, France 
593 |a Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires (I.G.E.B.A.), Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Ciudad Universitaria, Intendente Güiraldes 2160, C1428EGA, Buenos Aires, Argentina 
593 |a Geosciences Environnement Toulouse, CNRS and Université de Toulouse, F-31400 Toulouse, France 
690 1 0 |a ANNEALING 
690 1 0 |a CRYSTAL PREFERRED ORIENTATIONS 
690 1 0 |a MELT PERCOLATION 
690 1 0 |a OLIVINE 
690 1 0 |a ORTHOPYROXENE 
690 1 0 |a SUBCONTINENTAL MANTLE LITHOSPHERE 
690 1 0 |a ANNEALING 
690 1 0 |a BIREFRINGENCE 
690 1 0 |a DEFORMATION 
690 1 0 |a LITHOLOGY 
690 1 0 |a OLIVINE 
690 1 0 |a SEISMOLOGY 
690 1 0 |a SHEAR WAVES 
690 1 0 |a SOLVENTS 
690 1 0 |a TECTONICS 
690 1 0 |a WAVE PROPAGATION 
690 1 0 |a CRYSTAL PREFERRED ORIENTATIONS 
690 1 0 |a CRYSTALLOGRAPHIC PREFERRED ORIENTATIONS 
690 1 0 |a ELECTRON BACK-SCATTERED DIFFRACTION 
690 1 0 |a MELT PERCOLATIONS 
690 1 0 |a ORTHOPYROXENE 
690 1 0 |a STATIC RECRYSTALLIZATION 
690 1 0 |a SUB-CONTINENTAL LITHOSPHERIC MANTLES 
690 1 0 |a SUBCONTINENTAL MANTLE 
690 1 0 |a STRUCTURAL GEOLOGY 
690 1 0 |a ANNEALING 
690 1 0 |a CONTINENTAL LITHOSPHERE 
690 1 0 |a CRYSTALLOGRAPHY 
690 1 0 |a DEFORMATION 
690 1 0 |a MANTLE STRUCTURE 
690 1 0 |a OLIVINE 
690 1 0 |a ORIENTATION 
690 1 0 |a ORTHOPYROXENE 
690 1 0 |a P-WAVE 
690 1 0 |a S-WAVE 
690 1 0 |a SEISMOLOGY 
690 1 0 |a TECTONIC EVOLUTION 
690 1 0 |a VOLCANIC ROCK 
690 1 0 |a WAVE PROPAGATION 
690 1 0 |a XENOLITH 
690 1 0 |a GOBERNADOR GREGORES 
690 1 0 |a PALI AIKE VOLCANIC FIELD 
651 4 |a ARGENTINA 
651 4 |a SANTA CRUZ [ARGENTINA] 
700 1 |a Tommasi, A. 
700 1 |a Vauchez, A. 
700 1 |a Grégoire, M. 
773 0 |d Elsevier, 2014  |g v. 621  |h pp. 175-197  |p Tectonophysics  |x 00401951  |w (AR-BaUEN)CENRE-81  |t Tectonophysics 
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856 4 0 |u https://doi.org/10.1016/j.tecto.2014.02.017  |y DOI 
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