Instituto Geológico y Minero de España

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Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del 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
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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
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