Melting of peridotite to 140 gigapascals

Science

Volumn 329, Issue 5998, 2010, Pages 1516-1518

  Fiquet, G ^a   Auzende, A L ^a   Siebert, J ^a   Corgne, A ^a,b   Bureau, H ^a   Ozawa, H ^a,c   Garbarino, G ^d  

^a UNIVERSITÉ PIERRE ET MARIE CURIE   (France)

^b IRAP   (France)

^c UMR CNRS 5562 ^*  (Japan)

^d EUROPEAN SYNCHROTRON RADIATION FACILITY   (France)

Author keywords

[No Author keywords available]

Indexed keywords

DIAMOND; MINERAL; PERIDOTITE; UNCLASSIFIED DRUG;

CORE-MANTLE BOUNDARY; DIAMOND ANVIL CELL; LOWER MANTLE; MANTLE CHEMISTRY; PARTIAL MELTING; PERIDOTITE; PRESSURE GRADIENT; SEISMIC VELOCITY;

ARTICLE; ASTRONOMY; ATMOSPHERIC PRESSURE; CHEMICAL COMPOSITION; GEOCHEMISTRY; HEATING; LASER; LIQUID; MEASUREMENT; MELTING POINT; PHASE PARTITIONING; PRIORITY JOURNAL; ROCK; SOLID STATE; TEMPERATURE; VELOCITY;

EID: 77956703017     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1192448     Document Type: Article

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34. We thank L. Hennet and G. Ona Nguema for experimental assistance. X-ray diffraction plots were made using DATLAB software developed by K. Syassen. A.L.A. acknowledges support from Institut National des Sciences de l'Univers (INSU) program "PNP, theme SEDI-TPS," and A.C. acknowledges support from the European Research Council (ERC) under the European Community's Seventh Framework Programme (FP7/2007-2013)/ERC grant agreement 207467. The Focused Ion Beam (FIB) and Scanning Electron Microscope (SEM) facility of the Institut de Minéralogie et de Physique des Milieux Condensés is supported by Région Ile de France grant SESAME 2006 NoI-07-593/R, INSU-CNRS, Institut de Physique (INP)-CNRS, University Pierre et Marie Curie-Paris 6, and by the French National Research Agency (ANR) grant ANR-07-BLAN-0124-01.