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Lista de artículos
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B. Debret, N. Olfan Casanova, J. Padrón Navarta, F. Martin Hernandez, M. Andreani, C.J. Garrido Marin, V. López Sánchez-Vizcaíno, M. Gómez-Puigniare, M. Muñoz
and
N. Trcera,
"Redox state of iron during high-pressure serpentinite dehydration"
, vol.169, 1-18, 2015
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V. Colás , J.M. González Jiménez, W.L. Griffin , I. Fanlo, F. Gervilla Linares, S.Y. O Reilly, N.J. Pearson , T. Kerestedjian
and
J.A. Proenza,
"FINGERPRINTS OF METAMORPHISM IN CHROMITE: NEW INSIGHTS FROM MINOR AND TRACE ELEMENTS", "Chemical Geology"
, -, 2014
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J. Harvey , C.J. Garrido Marin, I. Savov, S. Agostini, J.A. Padrón Navarta, C. Marchesi, V. Lopez Sanchez-Vizcaino
and
M.T. Gomez Pugnaire,
"B-11-rich fluids in subduction zones: The role of antigorite dehydration in subducting slabs and boron isotope heterogeneity in the mantle", "Chemical Geology"
, vol.376, 20-30, 2014
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R. Piña, F. Gervilla Linares, S.-.J. Barnes, L. Ortega
and
R. Lunar,
"LIQUID IMMISCIBILITY BETWEEN ARSENIDE AND SULFIDE MELTS: EVIDENCE FROM LA-ICP-MS STUDY IN MAGMATIC DEPOSITS FROM SERRANIA DE RONDA (SPAIN)", "Mineralium Deposita"
, -, 2014
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J.A. Padrón Navarta, A. Tomassi
and
C.J. Garrido Marin,
"Dehydration-driven topotaxy in subduction zones", "Geophysical Research Abstracts"
, vol.16, EGU2014-14493-, 2014
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J.M. González Jiménez, W.L. Griffin , F. Gervilla Linares, J.A. Proenza, S.Y. Oreilly
and
N.J. Pearson ,
"CHROMITITES IN OPHIOLITES: HOW, WHERE, WHEN, WHY? PART I. A REVIEW AND NEW IDEAS ON THE ORIGIN AND SIGNIFICANCE OF PLATINUM-GROUP MINERALS", "Lithos"
, vol.189, 127-139, 2014
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F. Barra, F. Gervilla Linares, E. Hernández, M. Reich, J.A. Padrón Navarta
and
J.M. González Jiménez,
"Alteration patterns of chromian spinels from La Cabaña peridotite, south central Chile ", "Mineralogy and Petrology"
, -, 2014
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J.M. González Jiménez, W.L. Griffin , J.A. Proenza, F. Gervilla Linares, S.Y. O¿reilly, M. Akbulut, N.J. Pearson
and
S. Arai,
"CHROMITITES IN OPHIOLITES: HOW, WHERE, WHEN, WHY? PART II. THE CRYSTALLIZATION OF CHROMITITES", "Lithos"
, vol.189, 140-158, 2014
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