{"id":996,"date":"2022-01-27T18:22:56","date_gmt":"2022-01-27T18:22:56","guid":{"rendered":"https:\/\/wpd.ugr.es\/~gervilla\/?page_id=996"},"modified":"2025-11-04T18:07:28","modified_gmt":"2025-11-04T18:07:28","slug":"ophiolitic-chromitites","status":"publish","type":"page","link":"https:\/\/wpd.ugr.es\/~gervilla\/ophiolitic-chromitites\/","title":{"rendered":"Ophiolitic chromitites"},"content":{"rendered":"<p>[et_pb_section fb_built=\u00bb1&#8243; fullwidth=\u00bbon\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_fullwidth_header title=\u00bbOphiolitic chromitites\u00bb text_orientation=\u00bbcenter\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb title_font=\u00bb|600||on|||||\u00bb title_text_color=\u00bb#ffffff\u00bb background_enable_color=\u00bboff\u00bb background_image=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/wp-content\/uploads\/2020\/10\/Los-Naranjos-3.jpg\u00bb title_text_shadow_style=\u00bbpreset3&#8243; title_text_shadow_color=\u00bb#000000&#8243; global_colors_info=\u00bb{}\u00bb][\/et_pb_fullwidth_header][\/et_pb_section][et_pb_section fb_built=\u00bb1&#8243; _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb custom_padding=\u00bb0px||0px||false|false\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_row column_structure=\u00bb1_4,3_4&#8243; use_custom_gutter=\u00bbon\u00bb gutter_width=\u00bb2&#8243; make_equal=\u00bbon\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb width=\u00bb100%\u00bb max_width=\u00bb2560px\u00bb custom_margin=\u00bb0px|auto|0px|auto|false|false\u00bb custom_padding=\u00bb0px||0px||false|false\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb1_4&#8243; _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb background_color=\u00bb#565656&#8243; use_background_color_gradient=\u00bbon\u00bb background_color_gradient_direction=\u00bb90deg\u00bb background_color_gradient_stops=\u00bb#404040 9%|#8b8b8b 86%\u00bb background_color_gradient_start=\u00bb#404040&#8243; background_color_gradient_start_position=\u00bb9%\u00bb background_color_gradient_end=\u00bb#8b8b8b\u00bb background_color_gradient_end_position=\u00bb86%\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_text _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb header_2_font=\u00bb|600||on|||||\u00bb header_2_text_align=\u00bbcenter\u00bb header_2_text_color=\u00bb#ffffff\u00bb custom_margin=\u00bb65px||15px||false|false\u00bb global_colors_info=\u00bb{}\u00bb]<\/p>\n<h2><span>TOPICS<\/span><\/h2>\n<p>[\/et_pb_text][et_pb_blurb title=\u00bbRecent publications\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/publications\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb header_font=\u00bb|600|||||||\u00bb header_text_align=\u00bbleft\u00bb header_text_color=\u00bb#ffffff\u00bb header_font_size=\u00bb16px\u00bb header_line_height=\u00bb1.9em\u00bb custom_padding=\u00bb|35px||35px|false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_blurb][et_pb_blurb title=\u00bbPeridotites of the Serran\u00eda de Ronda\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/peridotites-of-the-serrania-de-ronda\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb header_font=\u00bb|600|||||||\u00bb header_text_align=\u00bbleft\u00bb header_text_color=\u00bb#ffffff\u00bb header_font_size=\u00bb16px\u00bb header_line_height=\u00bb1.3em\u00bb custom_padding=\u00bb|35px||35px|false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_blurb][et_pb_blurb title=\u00bbArsenic and PGE\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/arsenic-and-pge\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb header_font=\u00bb|600|||||||\u00bb header_text_align=\u00bbleft\u00bb header_text_color=\u00bb#ffffff\u00bb header_font_size=\u00bb16px\u00bb header_line_height=\u00bb1.9em\u00bb custom_padding=\u00bb|35px||35px|false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_blurb][et_pb_blurb title=\u00bbPlatinum-group minerals\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/platinum-group-minerals\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb header_font=\u00bb|600|||||||\u00bb header_text_align=\u00bbleft\u00bb header_text_color=\u00bb#ffffff\u00bb header_font_size=\u00bb16px\u00bb header_line_height=\u00bb1.9em\u00bb custom_padding=\u00bb|35px||35px|false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_blurb][et_pb_blurb title=\u00bbNi-Cu magmatic sulfide deposits\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/ni-cu-magmatic-sulfide-deposits\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb header_font=\u00bb|600|||||||\u00bb header_text_align=\u00bbleft\u00bb header_text_color=\u00bb#ffffff\u00bb header_font_size=\u00bb16px\u00bb header_line_height=\u00bb1.9em\u00bb custom_padding=\u00bb|35px||35px|false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_blurb][et_pb_blurb title=\u00bbOphiolitic chromitites\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/ophiolitic-chromitites\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb header_font=\u00bb|600|||on||||\u00bb header_text_align=\u00bbleft\u00bb header_text_color=\u00bb#ffffff\u00bb header_font_size=\u00bb16px\u00bb header_line_height=\u00bb1.9em\u00bb custom_padding=\u00bb|35px||35px|false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_blurb][et_pb_blurb title=\u00bbMetamorphism of chromitites\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/metamorphism-of-chromitites\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb header_font=\u00bb|600|||||||\u00bb header_text_align=\u00bbleft\u00bb header_text_color=\u00bb#ffffff\u00bb header_font_size=\u00bb16px\u00bb header_line_height=\u00bb1.9em\u00bb custom_padding=\u00bb|35px||35px|false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_blurb][et_pb_blurb title=\u00bbCo-Ni arsenides\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/co-ni-arsenides\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb header_font=\u00bb|600|||||||\u00bb header_text_align=\u00bbleft\u00bb header_text_color=\u00bb#ffffff\u00bb header_font_size=\u00bb16px\u00bb header_line_height=\u00bb1.9em\u00bb custom_padding=\u00bb|35px||35px|false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_blurb][et_pb_blurb title=\u00bbOther publications\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/other-publications\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb header_font=\u00bb|600|||||||\u00bb header_text_align=\u00bbleft\u00bb header_text_color=\u00bb#ffffff\u00bb header_font_size=\u00bb16px\u00bb header_line_height=\u00bb1.9em\u00bb custom_padding=\u00bb|35px||35px|false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_blurb][\/et_pb_column][et_pb_column type=\u00bb3_4&#8243; _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_text module_class=\u00bbpa-bullet-list-1&#8243; _builder_version=\u00bb4.27.4&#8243; _module_preset=\u00bbdefault\u00bb custom_padding=\u00bb70px|30px|35px|50px|false|false\u00bb hover_enabled=\u00bb0&#8243; global_colors_info=\u00bb{}\u00bb sticky_enabled=\u00bb0&#8243;]<\/p>\n<p><strong>Book chapters<\/strong><\/p>\n<ul>\n<li>Proenza, J<strong>.<\/strong>A., Rodr\u00edguez-Vega, A., D\u00edaz-Mart\u00ednez, R., <strong>Gervilla, F<\/strong>., Melgarejo, J.C., Ramayo, L. and Vila, A.R. (2004). Distribuci\u00f3n de elementos del grupo del platino (EGP) y Au en la faja ofiol\u00edtica Mayar\u00ed-Baracoa (Cuba oriental). En: <em>Complejos ofiol\u00edticos en Iberoam\u00e9rica: gu\u00edas de prospecci\u00f3n para metales preciosos<\/em>. Edit: E:S. Pereira, R. Castroviejo, F. Ortiz. <strong><em>Proyecto XIII.1 CYTED (Ciencia y Tecnolog\u00eda para el desarrollo)<\/em><\/strong>, pp. 309-336.<\/li>\n<li>Proenza, J.A., Castroviejo, R., Escayola, M., <strong>Gervilla, F.<\/strong>, Paladines, A., De Oliveira, D., Ortiz, F., Pereira, E.S., Rodr\u00edguez-Vega, A. Schalamuk, I. and Suita, M. (2004). Principales gu\u00edas de exploraci\u00f3n de metales nobles (elementos del grupo del platino y oro) en complejos ofiol\u00edticos. En: <em>Complejos ofiol\u00edticos en Iberoam\u00e9rica: gu\u00edas de prospecci\u00f3n para metales preciosos<\/em>. Edit: E:S. Pereira, R. Castroviejo, F. Ortiz. <strong><em>Proyecto XIII.1 CYTED (Ciencia y Tecnolog\u00eda para el desarrollo)<\/em><\/strong>, pp. 359-372.<\/li>\n<\/ul>\n<p><strong><br \/>Articles in scientific journals<\/strong><\/p>\n<ul>\n<li>Proenza, J., Melgarejo, J.C., <strong>Gervilla, F.<\/strong>, Lavaut, W., Rev\u00e9, D. and Rodr\u00edguez, G. (1998). Cromititas podiformes en la faja ofiol\u00edtica Mayar\u00ed-Baracoa (Cuba). <strong><em>Acta Geol\u00f3gica Hisp\u00e1nica<\/em><\/strong> 33 (1-4), 153-177.<br \/><a href=\"https:\/\/revistes.ub.edu\/index.php\/ActaGeologica\/article\/view\/4632\">https:\/\/revistes.ub.edu\/index.php\/ActaGeologica\/article\/view\/4632<\/a><\/li>\n<li>Proenza, J., <strong>Gervilla, F.<\/strong>, Melgarejo, J.C., Rev\u00e9, D. and Rodr\u00edguez, G. (1998). Las cromititas ofiol\u00edticas del yacimiento Mercedita (Cuba). Un ejemplo de cromititas ricas en Al en la zona de transici\u00f3n manto-corteza. <strong><em>Acta Geol\u00f3gica Hisp\u00e1nica<\/em><\/strong> 33 (1-4), 179-212.<br \/><a href=\"https:\/\/revistes.ub.edu\/index.php\/ActaGeologica\/article\/view\/4633\">https:\/\/revistes.ub.edu\/index.php\/ActaGeologica\/article\/view\/4633<\/a><\/li>\n<li>Proenza, J., <strong>Gervilla, F.<\/strong>, Melgarejo, J.C. and Bodinier, J.L. (1999). Al-rich and Cr-rich chromitites from the Mayar\u00ed-Baracoa ophiolitic belt (eastern Cuba): consequence of interaction between volatile-rich melts and peridotites in suprasubduction mantle. <strong><em>Economic Geology<\/em><\/strong>, 94, 547-566.<br \/><a href=\"https:\/\/doi.org\/10.2113\/gsecongeo.94.4.547\">https:\/\/doi.org\/10.2113\/gsecongeo.94.4.547<\/a><\/li>\n<li>Proenza, J.A., <strong>Gervilla, F.<\/strong>, Melgarejo, J.C., Vera, O., Alfonso, P. and Fallick, A.E. (2001). Genesis of sulfide-rich chromite ores by the interaction between chromitite and pegmatitic olivine-norite dikes in the Potos\u00ed Mine (Moa-Baracoa ophiolitic massif, eastern Cuba). <strong><em>Mineralium Deposita<\/em><\/strong> 36, 658-669.<br \/><a href=\"https:\/\/doi.org\/10.2113\/gsecongeo.94.4.547\">https:\/\/doi.org\/10.2113\/gsecongeo.94.4.547<\/a><\/li>\n<li>Proenza, J.A., <strong>Gervilla, F.<\/strong>, and Melgarejo J.C. (2002). Los dep\u00f3sitos de cromita en complejos ofiol\u00edticos: contrastantdo un modelo de formaci\u00f3n a trav\u00e9s de las particularidades de las cromititas de Cuba Oriental. <strong><em>Bolet\u00edn de la Sociedad Espa\u00f1ola de Mineralog\u00eda<\/em><\/strong> 25, 97-128.<br \/><a href=\"http:\/\/www.ehu.eus\/sem\/revista\/boletinSEM.htm\">http:\/\/www.ehu.eus\/sem\/revista\/boletinSEM.htm<\/a><\/li>\n<li>Proenza, J. Alfonso, P., Melgarejo, J.C., <strong>Gervilla, F.<\/strong>, Tritlla, J. and Fallick, A.E. (2003). D, O and C isotopes in podiform chromitites as fluid tracers for hidrotermal alteration proceses of the Mayar\u00ed-Baracoa Ophiolitic Belt, eastern Cuba. <strong><em>Journal of Geochemical Exploration <\/em><\/strong>78-79, 117-122.<br \/><a href=\"https:\/\/doi.org\/10.1016\/S0375-6742(03)00021-9\">https:\/\/doi.org\/10.1016\/S0375-6742(03)00021-9<\/a><\/li>\n<li>Proenza, J., Melgarejo, J.C. and <strong>Gervilla, F.<\/strong> (2003). Comments on the paper \u201cOcherous laterite: a nickel ore from Punta Gorda, Cuba\u201d by Oliveira et al. <strong><em>Journal of South American Earth Sciences<\/em><\/strong> 16, 199-202.<br \/><a href=\"https:\/\/doi.org\/10.1016\/S0895-9811(03)00024-5\">https:\/\/doi.org\/10.1016\/S0895-9811(03)00024-5<\/a><\/li>\n<li><strong>Gervilla, F.<\/strong>, Proenza, J.A., Frei, R., Gonz\u00e1lez-Jim\u00e9nez, J.M., Garrido, C.J., Melgarejo, J.C., Meibom, A., D\u00edaz-Mart\u00ednez, R. and Lavaut, W. (2005). Distribution of platinum-Group elements and Os isotopes in chromite ores from Mayar\u00ed-Baracoa Ophiolitic Belt (eastern Cuba). <strong><em>Contributions to Mineralogy and Petrology <\/em><\/strong>150, 589-607.<br \/><a href=\"https:\/\/doi.org\/10.1007\/s00410-005-0039-2\">https:\/\/doi.org\/10.1007\/s00410-005-0039-2<\/a><\/li>\n<li>Frei, R., <strong>Gervilla, F.<\/strong>, Meibom, A., Proenza, J.A. and Garrido, C.J. (2006). Os isotope heterogeneity of the upper mantle: Evidence from the Mayar\u00ed-Baracoa ophiolite belt in eastern Cuba. <strong><em>Earth and Planetary Science Letters<\/em><\/strong> 241, 466-476.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.epsl.2005.11.043\">https:\/\/doi.org\/10.1016\/j.epsl.2005.11.043<\/a><\/li>\n<li>Henares, S., <strong>Gervilla, F<\/strong>., Gonz\u00e1lez-Jim\u00e9nez., J.M., Proenza, J.A., Chang-Rodr\u00edguez, A. and Gonz\u00e1lez-Pont\u00f3n, R.B. (2010). Las cromititas del Complejo Ofiol\u00edtico de Camag\u00fcey, Cuba: un ejemplo de cromitas ricas en Al. <strong><em>Bolet\u00edn de la Sociedad Geol\u00f3gica Mexicana<\/em><\/strong> 62, 173-185.<br \/><a href=\"http:\/\/dx.doi.org\/10.18268\/BSGM2010v62n1a10\">http:\/\/dx.doi.org\/10.18268\/BSGM2010v62n1a10<\/a><\/li>\n<li>Gonz\u00e1lez-Jim\u00e9nez, J.M., Proenza, J.A., <strong>Gervilla, F.<\/strong>, Melgarejo, J.C., Blanco-Moreno, J.A., Ruiz-S\u00e1nchez, R. and Griffin, W.L. (2011). High-Cr and high-Al chromitites from the Sagua de T\u00e1namo distric, Mayar\u00ed-Cristal Ophiolitic Massif (eastern Cuba): constrains on their origin from mineralogy and geochemistry of chromian spinel and platinum-group elements. <strong><em>Lithos <\/em><\/strong>125 (1-2), 101-121.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.lithos.2011.01.016\">https:\/\/doi.org\/10.1016\/j.lithos.2011.01.016<\/a><\/li>\n<li>Marchesi, C., Gonz\u00e1lez-Jim\u00e9nez, J.M., <strong>Gervilla, F.<\/strong>, Garrido, C.J., Griffin, W.L., O\u2019Really, S., Proenza, J.A. and Pearson, N.J. (2011). In situ Re-Os isotopic analysis of platinum-group minerals from the Mayar\u00ed-Cristal ophiolitic massif (Mayar\u00ed-Baracoa Ophiolitic Belt, eastern Cuba): implications for the origin of Os-isotope heterogeneities in podiform chromitites. <strong><em>Contributions to Mineralogy and Petrology<\/em><\/strong> 161, No 6, 977-990.<span><br \/><a href=\"https:\/\/doi.org\/10.1007\/s00410-010-0575-2\">https:\/\/doi.org\/10.1007\/s00410-010-0575-2<\/a><\/span><\/li>\n<li>Gonz\u00e1lez-Jim\u00e9nez, J.M., <strong>Gervilla, F.<\/strong>, Griffin, W.L., Proenza, J.A., Aug\u00e9, T., O\u2019Really, S.Y. and Pearson, N. (2012). Os-isotope variability within sulfides from podiform chromitites. <strong><em>Chemical Geology<\/em><\/strong> 291, 224-235.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.chemgeo.2011.10.016\">https:\/\/doi.org\/10.1016\/j.chemgeo.2011.10.016<\/a><\/li>\n<li>Gonz\u00e1lez-Jim\u00e9nez, J.M., Marchesi, C., Griffin, W.L., Guti\u00e9rrez-Narbona, R., Lorand, J.P., O\u2019Reilly, S.Y., Garrido, C.J., <strong>Gervilla, F.<\/strong>, Pearson, N.J. and Hidas, K. (2013). Transfer of Os isotopic signatures from peridotite to chromitite in the subcontinental mantle: insights from in situ analysis of platinum-group and base-metal minerals (Oj\u00e9n peridotite massif, southern Spain). <strong><em>Lithos <\/em><\/strong>164-167, 74-85.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.lithos.2012.07.009\">https:\/\/doi.org\/10.1016\/j.lithos.2012.07.009<\/a><\/li>\n<li>Merinero, R., Lunar, R., Ortega, L., Pi\u00f1a, R., Monterrubio, S. and <strong>Gervilla, F.<\/strong> (2013). Hydrothermal palladium enrichment in podiform chromitites of Calzadilla de los Barros (SW Iberian Peninsula). <strong><em>Canadian Mineralogist<\/em><\/strong> 51, 387-404.<u><br \/><a href=\"https:\/\/doi.org\/10.3749\/canmin.51.3.387\">https:\/\/doi.org\/10.3749\/canmin.51.3.387<\/a><\/u><\/li>\n<li>Gonzalez-Jim\u00e9nez, J.M., Griffin, W.L.,<strong> Gervilla, F.<\/strong>, Proenza, J.A., O\u2019Reilly, S.Y. and Pearson, N.J. (2014). Chromitites in ophiolites: How, where, when, why? Part I. A review and new ideas on the origin and significance of platinum-group minerals.<strong><em> Lithos<\/em><\/strong> 189, 127-139.<br \/><a href=\"http:\/\/dx.doi.org\/10.1016\/j.lithos.2013.06.016\">http:\/\/dx.doi.org\/10.1016\/j.lithos.2013.06.016<\/a><\/li>\n<li>Gonzalez-Jim\u00e9nez, J.M., Griffin, W.L., Proenza, J.A., <strong>Gervilla, F.<\/strong>, O\u2019Reilly, S.Y., Akbulut, M., Pearson, N.J. and Arai, S. (2014). Chromitites in ophiolites: How, where, when, why? Part II. The crystallization of chromitites. <strong><em>Lithos<\/em><\/strong> 189, 140-158.<br \/><a href=\"http:\/\/dx.doi.org\/10.1016\/j.lithos.2013.09.008\">http:\/\/dx.doi.org\/10.1016\/j.lithos.2013.09.008<\/a><\/li>\n<li>Gonz\u00e1lez-Jim\u00e9nez, J.M., Barra, F., Walker, R., Reich, M. and <strong>Gervilla, F.<\/strong> (2014). Geodynamic implications of ophiolitic chromitites in the La Caba\u00f1a ultramafic bodies, Central Chile. <strong><em>International Geology Review<\/em><\/strong> 56, 1466-1483.<br \/><a href=\"https:\/\/doi.org\/10.1080\/00206814.2014.947334\">https:\/\/doi.org\/10.1080\/00206814.2014.947334<\/a><\/li>\n<li>Gonz\u00e1lez-Jim\u00e9nez, J.M., Locmelis, M., Belousova, E., Griffin, W.L., <strong>Gervilla, F.<\/strong>, Kerestedjian, T.N., O\u2019Reilly, S.Y., Pearson, N.J. and Sergeeva, I. (2015). Genesis and tectonic implications of podiform chromitites in the metamorphosed Ultramafic Massif of Dobromirtsi (Bulgaria). <strong><em>Gondwana Research<\/em><\/strong> 27 (2), 555-574.<br \/>DOI:\u00a0<a href=\"http:\/\/dx.doi.org\/10.1016\/j.gr.2013.09.020\">http:\/\/dx.doi.org\/10.1016\/j.gr.2013.09.020<\/a><\/li>\n<li>Col\u00e1s, V., Padr\u00f3n-Navarta, J.A., Gonz\u00e1lez-Jim\u00e9nez, J.M., Griffin, W.L., Fanlo, I., O&#8217;Reilly, S.Y., <strong>Gervilla, F.<\/strong>, Proenza, J.A., Pearson, N.J. and Escayola, M. (2016). Compositional effects on the solubility of minor and trace elements in oxide spinel minerals: insights from crystal-crystal partition coefficients in chromite exsolution. <strong><em>American Mineralogist <\/em><\/strong>101, 1360-1372.<br \/><span><a href=\"https:\/\/10.2138\/am-2016-5611\">https:\/\/10.2138\/am-2016-5611<\/a><\/span><\/li>\n<li>Pujol-Sol\u00e1, N., Proenza, J.A., Garc\u00eda-Casco, A., Gonz\u00e1lez-Jim\u00e9nez, J.M., Andreazini, A., Melgarejo, J.C. and <strong>Gervilla, F.<\/strong> (2018). An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba). <strong><em>Minerals<\/em><\/strong> 8, 433.<br \/><a href=\"https:\/\/doi.org\/10.3390\/min8100433\">https:\/\/doi.org\/10.3390\/min8100433<\/a><\/li>\n<li>Proenza, J., Gonz\u00e1lez-Jim\u00e9nez, J.M., Garc\u00eda-Casco, A., Belousova, E., Griffin, W.L., Talavera, C., Rojas-Agramonte, Y., Aiglsperger, T., Navarro-Ciurana, D., Pujol-Sola, N., <strong>Gervilla, F.<\/strong>, O&#8217;Reilly, S.T. and Jacob, D.E.\u00a0 \u00a0(2018). Cold plumes trigger contamination of oceanic mantle wedges with continental crust-derived sediments: evidence from chromitite zircons of eastern Cuban Ophiolites. <strong><em>Geoscience Frontiers<\/em><\/strong> 9(6), 1921-1936.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.gsf.2017.12.005\">https:\/\/doi.org\/10.1016\/j.gsf.2017.12.005<\/a><\/li>\n<li>Mendi, D.J., Gonz\u00e1lez-Jim\u00e9nez, J.M., Proenza, J.A., Urbani, F. and <strong>Gervilla, F.<\/strong> (2020). Petrogenesis of the chromitite body from the Cerro Colorado ophiolite, Paraguan\u00e1 Peninsula, Venezuela. <strong><em>Bolet\u00edn de la Sociedad Geol\u00f3gica Mexicana<\/em><\/strong> 72 (3), A280719.<br \/><a href=\"http:\/\/dx.doi.org\/10.18268\/BSGM2020v72n3a280719\">http:\/\/dx.doi.org\/10.18268\/BSGM2020v72n3a280719<\/a><\/li>\n<li>Gonz\u00e1lez-Jim\u00e9nez, J.M., Proenza, J.A., Pastor-Oliete, M., Saunders, E., Aiglsperger, T. Pujol-Sol\u00e1, N., Melgarejo, J.C., <strong>Gervilla, F.<\/strong> and Garc\u00eda-Casco, A. (2020). Precious metals in magmatic Fe-Ni-Cu sulfides from the Potos\u00ed chromitite deposit, eastern Cuba. <strong><em>Ore Geology Reviews<\/em><\/strong> 118, 103339.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.oregeorev.2020.103339\">https:\/\/doi.org\/10.1016\/j.oregeorev.2020.103339<\/a><\/li>\n<li>Pujol-Sol\u00e1, N., Proenza, J.A., Garc\u00eda-Casco, A., Gonz\u00e1lez-Jim\u00e9nez, J.M., Rom\u00e1n-Alpiste, M.J., Garrido, C.J., Melgarejo, J.C., <strong>Gervilla, F.<\/strong> and Llovet, X. (2020). Fe-Ti-Zr metasomatism in the oceanic mantle due to extreme differentiation of tholeiitic melts (Moa-Baracoa ophiolite, Cuba). <strong><em>Lithos <\/em><\/strong>105420.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.lithos.2020.105420\">https:\/\/doi.org\/10.1016\/j.lithos.2020.105420<\/a><\/li>\n<li>Pujol-Sol\u00e1, N., Proenza, J., Gonz\u00e1lez-Jim\u00e9nez, J.M., <strong>Gervilla, F.<\/strong>, Melgarejo, J.C., Marchesi, C. y Garc\u00eda-Casco, A. (2022). Comments on the paper \u201cTi-poor high-Al chromitites of the Moa-Baracoa ophiolitic massif (Eastern Cuba) formed in a nascent forearc mantle\u201d by Rui et al. (Ore Geol. Rev., 104847) <strong><em>Ore Geology Reviews <\/em><\/strong>148, 105019.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.oregeorev.2022.105019\">https:\/\/doi.org\/10.1016\/j.oregeorev.2022.105019<\/a><\/li>\n<li>Dom\u00ednguez-Carretero, D., Proenza, J.A., Pujol-Sol\u00e1, N., <strong>Gervilla, F.<\/strong>, Villanova-de-Benavent, C., Col\u00e1s, V., Nu\u00f1ez-Cambra, K., Pi\u00f1ero-P\u00e9rez, E. y Garc\u00eda-Casco, A. (2025). The gradual shift from forearc basalt-like to boninite-like magmatism during intra-oceanic subduction-initiation recorded by ophiolitic chromite deposits from Cuba. <strong><em>Mineralium Deposita<\/em><\/strong> 60, 1457-1478.<br \/><span><a href=\"http:\/\/doi.org\/10.1007\/s00126-025-01355-x\">http:\/\/doi.org\/10.1007\/s00126-025-01355-x<\/a><\/span><\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=\u00bb1&#8243; _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb background_color=\u00bb#000000&#8243; custom_padding=\u00bb||0px|||\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_row column_structure=\u00bb1_4,1_4,1_4,1_4&#8243; _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb1_4&#8243; _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_column][et_pb_column type=\u00bb1_4&#8243; _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_image src=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/wp-content\/uploads\/2020\/10\/ugr-blanco.png\u00bb title_text=\u00bbugr blanco\u00bb url=\u00bbhttps:\/\/www.ugr.es\/\u00bb url_new_window=\u00bbon\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb width=\u00bb130%\u00bb width_tablet=\u00bb\u00bb width_phone=\u00bb109%\u00bb width_last_edited=\u00bbon|phone\u00bb custom_margin=\u00bb|||-55px|false|false\u00bb custom_margin_tablet=\u00bb\u00bb custom_margin_phone=\u00bb\u00bb custom_margin_last_edited=\u00bbon|desktop\u00bb module_alignment_tablet=\u00bb\u00bb module_alignment_phone=\u00bbcenter\u00bb module_alignment_last_edited=\u00bbon|desktop\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_image][\/et_pb_column][et_pb_column type=\u00bb1_4&#8243; _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_image src=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/wp-content\/uploads\/2020\/10\/A9Rkf61lt_z3upt7_61s.png\u00bb title_text=\u00bbA9Rkf61lt_z3upt7_61s\u00bb url=\u00bbhttp:\/\/www.iact.ugr-csic.es\/\u00bb url_new_window=\u00bbon\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_image][\/et_pb_column][et_pb_column type=\u00bb1_4&#8243; _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>TOPICSBook chapters Proenza, J.A., Rodr\u00edguez-Vega, A., D\u00edaz-Mart\u00ednez, R., Gervilla, F., Melgarejo, J.C., Ramayo, L. and Vila, A.R. (2004). Distribuci\u00f3n de elementos del grupo del platino (EGP) y Au en la faja ofiol\u00edtica Mayar\u00ed-Baracoa (Cuba oriental). En: Complejos ofiol\u00edticos en Iberoam\u00e9rica: gu\u00edas de prospecci\u00f3n para metales preciosos. Edit: E:S. Pereira, R. Castroviejo, F. Ortiz. Proyecto XIII.1 [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"class_list":["post-996","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/pages\/996","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/comments?post=996"}],"version-history":[{"count":6,"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/pages\/996\/revisions"}],"predecessor-version":[{"id":1271,"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/pages\/996\/revisions\/1271"}],"wp:attachment":[{"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/media?parent=996"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}