{"id":114,"date":"2020-10-08T18:46:36","date_gmt":"2020-10-08T18:46:36","guid":{"rendered":"https:\/\/wpd.ugr.es\/~gervilla\/?page_id=114"},"modified":"2025-11-04T17:28:57","modified_gmt":"2025-11-04T17:28:57","slug":"peridotitas-de-la-serrania-de-ronda","status":"publish","type":"page","link":"https:\/\/wpd.ugr.es\/~gervilla\/peridotitas-de-la-serrania-de-ronda\/","title":{"rendered":"Peridotitas de la Serran\u00eda de Ronda"},"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=\u00bbPeridotitas de la Serran\u00eda de Ronda\u00bb text_orientation=\u00bbcenter\u00bb _builder_version=\u00bb4.16&#8243; _module_preset=\u00bbdefault\u00bb title_font=\u00bb|600||on|||||\u00bb background_enable_color=\u00bboff\u00bb background_image=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/wp-content\/uploads\/2020\/10\/Peridotitas-de-la-Serrania-de-Ronda.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>TEM\u00c1TICA<\/span><\/h2>\n<p>[\/et_pb_text][et_pb_blurb title=\u00bbPublicaciones recientes\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/publicaciones\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=\u00bbPeridotitas de la Serran\u00eda de Ronda\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/peridotitas-de-la-serrania-de-ronda\/\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=\u00bb1.3em\u00bb custom_padding=\u00bb|35px||35px|false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_blurb][et_pb_blurb title=\u00bbArsenico y EGP\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/arsenico-y-egp\/\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=\u00bbMinerales del grupo del platino\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/minerales-del-grupo-del-platino\/\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=\u00bbYacimientos de Ni-Cu\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/yacimientos-de-ni-cu\/\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=\u00bbCromititas ofiol\u00edticas\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/cromititas-ofioliticas\/\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=\u00bbMetamorfismo de cromititas\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/metamorfismo-de-cromititas\/\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=\u00bbArseniuros de Co-Ni\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/arseniuros-de-co-ni\/\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=\u00bbOtras publicaciones\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/otras-publicaciones\/\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>Libros<\/strong><\/p>\n<ul>\n<li><strong>Gervilla, F.<\/strong> (1990). Mineralizaciones magm\u00e1ticas ligadas a la evoluci\u00f3n de las rocas ultram\u00e1ficas de la Serran\u00eda de Ronda (M\u00e1laga, Espa\u00f1a). Edit. <strong><em> Mineralog\u00eda y Petrolog\u00eda. Universidad de Granada<\/em><\/strong>. 189p.<\/li>\n<li><strong>Gervilla, F.,<\/strong> Gonz\u00e1lez-Jim\u00e9nez, J.M., Hidas, K., Marchesi, C. y Pi\u00f1a, R. (2019). Geology and metallogeny of the upper mantle rocks from the Serran\u00eda de Ronda. Publicaciones de la <strong><em>Sociedad Espa\u00f1ola de Mineralog\u00eda<\/em><\/strong> (ISBN: 978-84-15588-30-6), 122 p.<br \/><a href=\"http:\/\/www.semineral.es\/websem\/PdfServlet?mod=archivos&amp;subMod=publicaciones&amp;archivo=Gervilla.et.al.2019.Geology.metallogeny.Ronda.peridotites.pdf\">http:\/\/www.semineral.es\/websem\/PdfServlet?mod=archivos&amp;subMod=publicaciones&amp;archivo=Gervilla.et.al.2019.Geology.metallogeny.Ronda.peridotites.pdf<\/a><\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<p><strong>Cap\u00edtulos de libros<\/strong><\/p>\n<ul>\n<li>Leblanc, M. y <strong>Gervilla-Linares, F. <\/strong>(1988). Platinum-Group Elements and Au distribution in Ni arsenide-chromite veins from the rifo-betic lherzolite massifs (Morocco-Spain). <em>Geoplatinum`87<\/em>, Eds: Prichard et al. <strong><em>Elsevier Applied Science<\/em><\/strong>, 181-198.<\/li>\n<li><strong>Gervilla, F. <\/strong>(1992). Dep\u00f3sitos de cromita-arseniuros de Ni-(Au-EGP) y de sulfuros de Fe-Ni-Cu y grafito asociados a las rocas ultram\u00e1ficas del sur de Espa\u00f1a. En: <em>Recursos Minerales de Espa\u00f1a<\/em>, Edit: J. Garc\u00eda Guinea y J. Mart\u00ednez Frias. <strong><em>C.S.I.C. Colecci\u00f3n:\u00bbTextos Universitarios\u00bb<\/em><\/strong> vol. 15, 275-289.<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<p><strong>Publicaciones en revistas<\/strong><\/p>\n<ul>\n<li>Leblanc, M., <strong>Gervilla, F.<\/strong> y Jedwab, J. (1990). Noble metals segregation and fractionation in magmatic ores from Ronda and Beni Bousera lherzolite massifs (Spain, Morocco). <strong><em>Mineralogy &amp; Petrology<\/em><\/strong>, 42 (1-4), 133-248.<br \/><a href=\"https:\/\/doi.org\/10.1007\/BF01162693\">https:\/\/doi.org\/10.1007\/BF01162693<\/a><\/li>\n<li><strong>Gervilla, F.<\/strong> y Leblanc, M. (1990). Magmatic ores in high-temperature alpine-type lherzolite massifs (Ronda, Spain, and Beni Bousera, Morocco). <strong><em>Economic Geology<\/em><\/strong><em>,<\/em> 85, 112-132.<br \/><u><a href=\"https:\/\/doi.org\/10.2113\/gsecongeo.85.1.112\">https:\/\/doi.org\/10.2113\/gsecongeo.85.1.112<\/a><\/u><strong><\/strong><\/li>\n<li><strong>Gervilla, F. <\/strong>y R\u00f8nsbo, J. (1992). New Data on (Ni, Fe, Co) diarsenides and sulpharsenides in chromite-niccolite ores from M\u00e1laga province, south Spain. <strong><em>Neues Jahbr. Mineralogie Mh.<\/em><\/strong>, H.5, 193-206.<\/li>\n<li>Torres-Ruiz, J., Garuti, G., Gazzoti, M., <strong>Gervilla, F.<\/strong> y Fenoll Hach-Al\u00ed, P. (1996). Platinum-group minerals in chromitites from the Oj\u00e9n lherzolite massif (Serran\u00eda de Ronda, Betic Cordillera, Southern Spain). <strong><em>Mineralogy and Petrology<\/em><\/strong>, 56, 25-50.<br \/><span><a href=\"https:\/\/doi.org\/10.1007\/BF01162656\">https:\/\/doi.org\/10.1007\/BF01162656<\/a><\/span><\/li>\n<li><span><\/span>Lenoir, X., Garrido, C.J., Bodinier, J.-L., Dautria, J.-M. y <strong>Gervilla, F.<\/strong> (2001). The recrystallization front of the Ronda peridotite: Evidence for melting and thermal erosion of subcontinental lithospheric mantle beneath the Albor\u00e1n basin. <strong><em>Journal of Petrology,<\/em><\/strong> 42 (1), 141-158.<br \/><a href=\"https:\/\/doi.org\/10.1093\/petrology\/42.1.141\">https:\/\/doi.org\/10.1093\/petrology\/42.1.141<\/a><\/li>\n<li>Morishita, T., Arai, S. y <strong>Gervilla, F.<\/strong> (2001). High-pressure aluminous mafic rocks from the Ronda peridotite massif, Southern Spain: significance of sapphirine- and corundum-bearing mineral assemblages. <strong><em>Lithos, <\/em><\/strong>57, 143-161.<br \/><a href=\"https:\/\/doi.org\/10.1016\/S0024-4937(01)00036-6\">https:\/\/doi.org\/10.1016\/S0024-4937(01)00036-6<\/a><\/li>\n<li>Hem, S.R., Makovicky, E. y <strong>Gervilla, F.<\/strong> (2001). Compositional trends in Fe, Co and Ni sulfarsenides and their crystal chemical implications: results from the Arroyo de la Cueva deposits, Ronda Peridotite, South Spain. <strong><em>The Canadian Mineralogist, <\/em><\/strong>39 (3), 831-854.<br \/><u><a href=\"https:\/\/doi.org\/10.2113\/gscanmin.39.3.831\">https:\/\/doi.org\/10.2113\/gscanmin.39.3.831<\/a><\/u><strong><\/strong><\/li>\n<li><strong>Gervilla, F., <\/strong>Guti\u00e9rrez-Narbona, R. y Fenoll-Hach-Al\u00ed, P. (2002). The origin of different types of magmatic mineralizations from small-volume melts in the lherzolite massifs of the Serran\u00eda de Ronda. <strong><em>Bolet\u00edn de la Sociedad Espa\u00f1ola de Mineralog\u00eda <\/em><\/strong>25, 79-96<br \/><a href=\"https:\/\/wpd.ugr.es\/~gervilla\/wp-content\/uploads\/2020\/10\/Gervilla-et-al.2002_BSEM.pdf\" target=\"_blank\" rel=\"noopener noreferrer\">Gervilla et al.2002_BSEM.pdf<\/a><\/li>\n<li>Morishita, T., Arai, S., <strong>Gervilla, F.<\/strong> y Green, D.H. (2003). Closed-system geochemical recycling of crustal materials in alpine-type peridotite. <strong><em>Geochimica et Cosmochimica Acta <\/em><\/strong>67 (2), 303-310.<br \/><a href=\"https:\/\/doi.org\/10.1016\/S0016-7037(02)01079-7\">https:\/\/doi.org\/10.1016\/S0016-7037(02)01079-7<\/a><\/li>\n<li>Guti\u00e9rrez-Narbona, R., Lorand, J.P., <strong>Gervilla, F.<\/strong> y Gros, M. (2003). New data on base metal mineralogy and platinum-group minerals in the Oj\u00e9n chromitites (Serran\u00eda de Ronda, Betic Cordillera, Southern Spain). <strong><em>Neues Jahbr. Mineralogie Abh.<\/em><\/strong>179 (2), 143-173.<br \/><a href=\"https:\/\/doi.org\/10.1127\/0077-7757\/2003\/0179-0143\">https:\/\/doi.org\/10.1127\/0077-7757\/2003\/0179-0143<\/a><\/li>\n<li>Villasante-Marcos, V., Osete, M.L., <strong>Gervilla, F.<\/strong> y Garc\u00eda-Due\u00f1as, V. (2003). Paleomagnetic study of the Ronda peridotites (Betic Cordillera, Southern Spain). <strong><em>Tectonophysics <\/em><\/strong>377, 119-141.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.tecto.2003.08.023\">https:\/\/doi.org\/10.1016\/j.tecto.2003.08.023<\/a><\/li>\n<li>Crespo, E., Luque, F.J., Rodas, M., Wada, H. y <strong>Gervilla, F<\/strong>. (2006). Graphite-sulfide veins in Ronda and Beni Bousera orogenic lherzolites (Spain and Morocco) and the origin of Carbon in mantle-derived rocks. <strong><em>Gondwana Research<\/em><\/strong> 9, 279-290.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.gr.2005.10.003\">https:\/\/doi.org\/10.1016\/j.gr.2005.10.003<\/a><\/li>\n<li>Bodinier, J.-L., Garrido, C.J., Chanefo, I. Bruguier, O. y <strong>Gervilla, F.<\/strong> (2008). Origin of pyroxenite-peridotite veined mantle by refertilization reactions: Evidence from the Ronda Peridotite (S. Spain). <strong><em>Journal of Petrology<\/em><\/strong>, 49, 999-1025.<br \/><a href=\"https:\/\/doi.org\/10.1093\/petrology\/egn014\">https:\/\/doi.org\/10.1093\/petrology\/egn014<\/a><\/li>\n<li>Morishita, T., Arai, S., Ishida, Y., Tamura, A. y <strong>Gervilla, F.<\/strong> (2009). Constraints on the evolutionary history of aluminous mafic rocks in the Ronda peridotite massif (Spain) from trace-element compositions of clinopyroxene and garnet. <strong><em>Geochemical Journal<\/em><\/strong> 43 (3), 191-206.<br \/><a href=\"http:\/\/www.terrapub.co.jp\/journals\/GJ\/pdf\/4303\/43030191.pdf\">http:\/\/www.terrapub.co.jp\/journals\/GJ\/pdf\/4303\/43030191.pdf<\/a><\/li>\n<li>Marchesi, C., Garrido, C.J., Bosh, D., Bodinier, J.L., Hidas, K., Padr\u00f3n-Navarta, J.A. y <strong>Gervilla, F.<\/strong> (2012). A late Oligocene supra-subduction setting in the westernmost Mediterranean revealed by intrusive pyroxenite dykes in the Ronda peridotite (southern Spain). <strong><em>Journal of Geology<\/em><\/strong> 120 (2), 237-247.<br \/><a href=\"https:\/\/doi.org\/10.1086\/663875\">https:\/\/doi.org\/10.1086\/663875<\/a><\/li>\n<li>Marchesi, C., Garrido, C.J., Bosch, D., Bodinier, J.L., <strong>Gervilla, F.<\/strong> y Hidas, K. (2013). Mantle refertilization by melts of crustal-derived garnet pyroxenite: Evidence from the Ronda peridotite massif, southern Spain. <strong><em>Earth and Planetary Science Letters<\/em><\/strong> 362, 66-75.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.epsl.2012.11.047\">https:\/\/doi.org\/10.1016\/j.epsl.2012.11.047<\/a><\/li>\n<li>Pi\u00f1a, R., <strong>Gervilla, F.<\/strong>, Barnes, S.-J., Ortega, L. y Lunar, R. (2013). Partition coefficients of platinum-group and chalcophile elements between arsenide and sulfide phases as determined in the Amasined sulfide-graphite mineralization (Beni Bousera, North Morocco). <strong><em>Economic Geology<\/em><\/strong> 108, 935-951.<br \/><u><a href=\"https:\/\/doi.org\/10.2113\/econgeo.108.5.935\">https:\/\/doi.org\/10.2113\/econgeo.108.5.935<\/a><\/u><\/li>\n<li>Marchesi, C. Dale, C.W., Garrido, C.J., Pearson, D.G., Bosh, D., Bodinier, J.L. <strong>Gervilla, F.<\/strong> y Hidas, K. (2014). Fractionation of highly siderophile elements in refertilized mantle: implications for the Os isotope composition of basalts. <strong><em>Earth and Planetary Science Letters<\/em><\/strong> 400, 33-44.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.epsl.2014.05.025\">https:\/\/doi.org\/10.1016\/j.epsl.2014.05.025<\/a><\/li>\n<li>Pi\u00f1a, R., <strong>Gervilla, F.<\/strong>, Barnes, S.-J, Ortega, L. y Lunar, R. (2015). Liquid immiscibility between arsenide and sulfide melts: evidence from LA-ICP-MS study in magmatic deposits from Serran\u00eda de Ronda (Spain). <strong><em>Mineralium Deposita<\/em><\/strong> 50, 265-279.<br \/>DOI:\u00a0<a href=\"http:\/\/dx.doi.org\/10.1007\/s00126-014-0534-3\">http:\/\/dx.doi.org\/10.1007\/s00126-014-0534-3<\/a><\/li>\n<li>Gonz\u00e1lez-Jim\u00e9nez, J.M., Marchesi, C., Griffin, W.L., <strong>Gervilla, F.<\/strong>, Belousova, E.A., Garrido, C.J., Romero, R., Talavera, C., Leisen, M., O\u2019Reilly, S.Y., Barra, F. y Martin, L. (2017). Zircon recycling and crystallization during formation of chromite- and Ni-arsenide ores in the subcontinental lithospheric mantle (Serran\u00eda de Ronda, Spain). <strong><em>Ore Geology Reviews<\/em><\/strong> 90, 193-209.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.oregeorev.2017.02.012\">https:\/\/doi.org\/10.1016\/j.oregeorev.2017.02.012<\/a><\/li>\n<li>Baurier-Aymat, S., Jim\u00e9nez-Franco, A., Roqu\u00e9-Rosell, J., Gonz\u00e1lez-Jim\u00e9nez, J.M., <strong>Gervilla, F.<\/strong>, Proenza, J.A., Mendoza, J. y Nieto, F. (2019). Nanoscale Structure of Zoned Laurites from the Oj\u00e9n Ultramafic Massif, Southern Spain. <strong><em>Minerals <\/em><\/strong>9, 288.<br \/><a href=\"https:\/\/10.3390\/min9050288\">https:\/\/10.3390\/min9050288<\/a><\/li>\n<li>Neuveck, A., Broman, C., Ivarson, M., Holm, N.G., Whitehouse, M., Nilsson, S., Geppert, W. y <strong>Gervilla, F.<\/strong> (2020). Isotopic signatures of carbon in the \u201cLos Pobres\u201d graphite mine, Ronda, Spain. <strong><em>Journal of Petrology<\/em><\/strong> 61 (4), egaa042.<br \/><a href=\"https:\/\/doi.org\/10.1093\/petrology\/egaa042\">https:\/\/doi.org\/10.1093\/petrology\/egaa042<\/a><\/li>\n<li>Lorand, J.P., Pont, S., Gutierez-Narbona, R. y Gervilla, F. (2021). Chalcophile-siderophile element systematics and regional-scale magmatic percolation in the Ronda peridotite massif (Spain). <strong><em>Lithos<\/em><\/strong>, 105901.<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.lithos.2020.105901\">https:\/\/doi.org\/10.1016\/j.lithos.2020.105901<\/a><\/li>\n<li>Gonz\u00e1lez-P\u00e9rez, I., Gonz\u00e1lez-Jim\u00e9nez, J.M., Dare, S.A.S., Schettino, E., Pi\u00f1a, R., Marchesi, C., Yesares, L. y <strong>Gervilla, F.<\/strong> (2024). Li enrichment in peridotites and chromitites tracks mantle-crust interaction. <strong><em>Lithos <\/em><\/strong>488-489,<br \/><a href=\"https:\/\/doi.org\/10.1016\/j.lithos.2024.107819\">https:\/\/doi.org\/10.1016\/j.lithos.2024.107819<\/a><\/li>\n<li>Gonz\u00e1lez-P\u00e9rez, I., Gonz\u00e1lez-Jim\u00e9nez, J.M., Llopis, J. y <strong>Gervilla, F.<\/strong> (2024). Micro-to-nano-size solid inclusions in magnetite record skarn-reactions. <strong><em>European Journal of Mineralogy<\/em><\/strong> 36, 925-941.<br \/><a href=\"https:\/\/doi.org\/10.5194\/ejm-36-925-2024\">https:\/\/doi.org\/10.5194\/ejm-36-925-2024<\/a><\/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>TEM\u00c1TICALibros Gervilla, F. (1990). Mineralizaciones magm\u00e1ticas ligadas a la evoluci\u00f3n de las rocas ultram\u00e1ficas de la Serran\u00eda de Ronda (M\u00e1laga, Espa\u00f1a). Edit. Mineralog\u00eda y Petrolog\u00eda. Universidad de Granada. 189p. Gervilla, F., Gonz\u00e1lez-Jim\u00e9nez, J.M., Hidas, K., Marchesi, C. y Pi\u00f1a, R. (2019). Geology and metallogeny of the upper mantle rocks from the Serran\u00eda de Ronda. Publicaciones [&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-114","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/pages\/114","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=114"}],"version-history":[{"count":9,"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/pages\/114\/revisions"}],"predecessor-version":[{"id":1259,"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/pages\/114\/revisions\/1259"}],"wp:attachment":[{"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/media?parent=114"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}