{"id":160,"date":"2020-10-15T00:01:39","date_gmt":"2020-10-15T00:01:39","guid":{"rendered":"https:\/\/wpd.ugr.es\/~gervilla\/?page_id=160"},"modified":"2022-01-28T12:49:12","modified_gmt":"2022-01-28T12:49:12","slug":"arsenico-y-egp","status":"publish","type":"page","link":"https:\/\/wpd.ugr.es\/~gervilla\/arsenico-y-egp\/","title":{"rendered":"Arsenico y EGP"},"content":{"rendered":"<p>[et_pb_section fb_built=\u00bb1&#8243; fullwidth=\u00bbon\u00bb _builder_version=\u00bb4.6.5&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_fullwidth_header title=\u00bbArsenico y EGP\u00bb text_orientation=\u00bbcenter\u00bb _builder_version=\u00bb4.6.5&#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\/Bandeado-Cr-Ni-S.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=\u00bb4.6.5&#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=\u00bb4.6.5&#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=\u00bb4.6.5&#8243; _module_preset=\u00bbdefault\u00bb background_color=\u00bb#565656&#8243; use_background_color_gradient=\u00bbon\u00bb background_color_gradient_start=\u00bb#404040&#8243; background_color_gradient_end=\u00bb#8b8b8b\u00bb background_color_gradient_direction=\u00bb90deg\u00bb background_color_gradient_start_position=\u00bb9%\u00bb background_color_gradient_end_position=\u00bb86%\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_text _builder_version=\u00bb4.6.5&#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=\u00bb4.13.0&#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=\u00bb4.13.0&#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=\u00bbArsenico y EGP\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/arsenico-y-egp\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.13.0&#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=\u00bbMinerales del grupo del platino\u00bb url=\u00bbhttps:\/\/wpd.ugr.es\/~gervilla\/minerales-del-grupo-del-platino\/\u00bb icon_placement=\u00bbleft\u00bb _builder_version=\u00bb4.13.0&#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=\u00bb4.13.0&#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=\u00bb4.13.0&#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=\u00bb4.13.0&#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=\u00bb4.13.0&#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=\u00bb4.13.0&#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=\u00bb4.6.5&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_text module_class=\u00bbpa-bullet-list-1&#8243; _builder_version=\u00bb4.14.7&#8243; _module_preset=\u00bbdefault\u00bb custom_padding=\u00bb70px|30px|35px|50px|false|false\u00bb global_colors_info=\u00bb{}\u00bb]<\/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 \/><span><a href=\"https:\/\/doi.org\/10.1007\/BF01162693\">https:\/\/doi.org\/10.1007\/BF01162693<\/a><\/span><\/li>\n<li><span><\/span><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.<u><br \/><a href=\"https:\/\/doi.org\/10.2113\/gsecongeo.85.1.112\">https:\/\/doi.org\/10.2113\/gsecongeo.85.1.112<\/a><\/u><\/li>\n<li><strong>Gervilla, F<\/strong>., Makovicky, E., Makovicky, M. y Rose-Hansen, J. (1994). The system Pd-Ni-As at 790\u00b0 and 450\u00b0C. <strong><em>Economic Geology<\/em><\/strong>, 89, 1630-1639.<u><br \/><a href=\"https:\/\/doi.org\/10.2113\/gsecongeo.89.7.1630\">https:\/\/doi.org\/10.2113\/gsecongeo.89.7.1630<\/a><\/u><\/li>\n<li><strong>Gervilla, F.<\/strong>, Leblanc, M., Torres-Ruiz, J. y Fenoll Hach-Al\u00ed, P. (1996). Immiscibility between arsenide and sulfide melts: a mechanism for the concentration of noble metals. <strong><em>The<\/em><\/strong> <strong><em>Canadian Mineralogist<\/em><\/strong>, 34, 485-502.<span><u><br \/><a href=\"http:\/\/www.canmin.org\/\">http:\/\/www.canmin.org\/<\/a><\/u><\/span><\/li>\n<li><strong>Gervilla, F.<\/strong>, Papunen, H.,\u00a0 Kojonen, K. y Johanson, B. (1998). Platinum-, palladium- and gold-rich arsenide ores from the Kylm\u00e4koski Ni-Cu deposit (Vammala Nickel Belt, SW Finland). <strong><em>Mineralogy and Petrology, <\/em><\/strong>64, 163-185.<br \/><a href=\"https:\/\/doi.org\/10.1007\/BF01226568\">https:\/\/doi.org\/10.1007\/BF01226568<\/a><\/li>\n<li><strong>Gervilla, F.<\/strong> (1999). El papel del ars\u00e9nico como colector de elementos del grupo del platino en los yacimientos de Ni-Cu. <strong><em>Bolet\u00edn de la Sociedad Espa\u00f1ola de Mineralog\u00eda<\/em><\/strong> 22, 29-53.<br \/><a href=\"http:\/\/www.ehu.eus\/sem\/revista\/boletinSEM.htm?CSRT=4179275922304365326\">http:\/\/www.ehu.eus\/sem\/revista\/boletinSEM.htm?CSRT=4179275922304365326<\/a><\/li>\n<li><strong>Gervilla, F., <\/strong>Cabri, L.J., Kojonen, K., Oberth\u00fcr, T., Weiser, T.W., Johanson, B., Sie, S.H., Campbell, J.L., Teesdale, W.J. y Laflamme, J.H.G. (2004). Platinum-group element distribution in some ore deposits: results of EPMA and micro-PIXE analyses. <strong><em>Microchimica Acta<\/em><\/strong> 147, 163-173.<br \/><a href=\"https:\/\/doi.org\/10.1007\/s00604-004-0187-5\">https:\/\/doi.org\/10.1007\/s00604-004-0187-5<\/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.<u><br \/><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>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>Pi\u00f1a, R., <strong>Gervilla, F.<\/strong>, Helmy, H., Fonseca, R.O.C. y Ballhaus, C. (2020). Partition behaviour of platinum-group elements during the segregation of arsenide melts from sulfide magma. <strong><em>American Mineralogist<\/em><\/strong> 105, 1889-1897.<br \/><a href=\"https:\/\/doi.org\/10.2138\/am-2020-7477\">https:\/\/doi.org\/10.2138\/am-2020-7477<\/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=\u00bb4.6.5&#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=\u00bb4.6.5&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb1_4&#8243; _builder_version=\u00bb4.6.5&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_column][et_pb_column type=\u00bb1_4&#8243; _builder_version=\u00bb4.6.5&#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=\u00bb4.6.5&#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=\u00bb4.6.5&#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=\u00bb4.6.5&#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=\u00bb4.6.5&#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\u00c1TICAPublicaciones en revistas Leblanc, M., Gervilla, F. y Jedwab, J. (1990). Noble metals segregation and fractionation in magmatic ores from Ronda and Beni Bousera lherzolite massifs (Spain, Morocco). Mineralogy &amp; Petrology, 42 (1-4), 133-248.https:\/\/doi.org\/10.1007\/BF01162693 Gervilla, F. y Leblanc, M. (1990). Magmatic ores in high-temperature alpine-type lherzolite massifs (Ronda, Spain, and Beni Bousera, Morocco). Economic Geology, [&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":"<!-- wp:divi\/placeholder \/-->","_et_gb_content_width":"","footnotes":""},"class_list":["post-160","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/pages\/160","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=160"}],"version-history":[{"count":5,"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/pages\/160\/revisions"}],"predecessor-version":[{"id":1176,"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/pages\/160\/revisions\/1176"}],"wp:attachment":[{"href":"https:\/\/wpd.ugr.es\/~gervilla\/wp-json\/wp\/v2\/media?parent=160"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}