Registros del 1 al 9 de 9 encontrados |
1.- AL- AND CR-RICH CHROMITITES FROM THE MAYARI-BARACOA OPHIOLITIC BELT (EASTERN CUBA); CONSEQUENCE OF INTERACTION BETWEEN VOLATILE-RICH MELTS AND PERIDOTITES IN SUPRASUBDUCTION MANTLE ECONOMIC GEOLOGY PUBLISHING COMPANY; LANCASTER, PA; USA; UNITED STATES, 1999 Ver registro
2.- DIVERSITY OF MAFIC ROCKS IN THE RONDA PERIDOTITE; EVIDENCE FOR PERVASIVE MELT-ROCK REACTION DURING HEATING SUBCONTINENTAL LITHOSPHERE BY UPWELLING ASTHENOSPHERE CLARENDON PRESS; OXFORD; GBR; UNITED KINGDOM, 1999 Ver registro
3.- ENRICHMENT OF HFSE IN CHLORITE-HARZBURGITE PRODUCED BY HIGH-PRESSURE DEHYDRATION OF ANTIGORITE-SERPENTINITE; IMPLICATIONS FOR SUBDUCTION MAGMATISM AMERICAN GEOPHYSICAL UNION AND THE GEOCHEMICAL SOCIETY;; USA; UNITED STATES, 2005 Ver registro
4.- INCOMPATIBLE TRACE ELEMENT PARTITIONING AND RESIDENCE IN ANHYDROUS SPINEL PERIDOTITES AND WEBSTERITES FROM THE RONDA OROGENIC PERIDOTITE ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2000 Ver registro
5.- Mantle refertilization by melts of crustal-derived garnet pyroxenite; evidence from the Ronda peridotite massif, southern Spain Elsevier; Amsterdam; NLD; Netherlands, 2013 Ver registro
6.- Origin of pyroxenite-peridotite veined mantle by refertilization reactions; evidence from the Ronda Peridotite (southern Spain) Oxford University Press; Oxford; GBR; United Kingdom, 2008 Ver registro
7.- Persistence of mantle lithospheric Re-Os signature during asthenospherization of the subcontinental lithospheric mantle; insights from in situ isotopic analysis of sulfides from the Ronda Peridotite (southern Spain) Springer International; Heidelberg - New York; III; International, 2010 Ver registro
8.- Persistence of mantle lithospheric Re-Os signature during lithosphere-asthenosphere interaction; insights from in situ isotopic analysis of sulfides from the Ronda Peridotite (S. Spain) Elsevier; New York, NY; III; International, 2009 Abstracts of the 19th annual V. M. Goldschmidt conference Ver registro
9.- THE RECRYSTALLIZATION FRONT OF THE RONDA PERIDOTITE; EVIDENCE FOR MELTING AND THERMAL EROSION OF SUBCONTINENTAL LITHOSPHERIC MANTLE BENEATH THE ALBORAN BASIN OXFORD UNIVERSITY PRESS; OXFORD; GBR; UNITED KINGDOM, 2001 OROGENIC LHERZOLITES AND MANTLE PROCESSES Ver registro
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