{"id":3584,"date":"2017-10-14T09:43:15","date_gmt":"2017-10-14T09:43:15","guid":{"rendered":"http:\/\/webfe10.fe.cpd.local\/caribbeanlithos\/?p=3584"},"modified":"2026-03-04T15:31:29","modified_gmt":"2026-03-04T15:31:29","slug":"2017-the-recycling-of-chromitites-in-ophiolites-from-southwestern-north-america","status":"publish","type":"post","link":"https:\/\/caribbeanlithos.ub.edu\/?p=3584","title":{"rendered":"2017: The recycling of chromitites in ophiolites from southwestern North America"},"content":{"rendered":"

The recycling of chromitites in ophiolites from southwestern North America<\/strong><\/p>\n

Podiform chromitites occur in mantle peridotites of the Late Triassic Puerto Nuevo Ophiolite, Baja California Sur State, Mexico. These are high-Cr chromitites [Cr# (Cr\/Cr\u00a0+\u00a0Al atomic ratio\u00a0=\u00a00.61\u20130.69] that contain a range of minor- and trace-elements and show whole-rock enrichment in IPGE (Os, Ir, Ru). These features are similar to those of high-Cr ophiolitic chromitites crystallised from melts similar to high-Mg island-arc tholeiites (IAT) and boninites in supra-subduction-zone mantle wedges. Crystallisation of these chromitites from S-undersaturated melts is consistent with the presence of abundant inclusions of platinum-group minerals (PGM) such as laurite (RuS2<\/sub>)-erlichmanite (OsS2<\/sub>), osmium and irarsite (IrAsS) in chromite, that yield T<\/em>MA<\/sub>\u00a0\u2248\u00a0T<\/em>RD<\/sub> model ages peaking at ~\u00a0325 Ma. Thirty-three xenocrystic zircons recovered from mineral concentrates of these chromitites yield ages (2263\u00a0\u00b1\u00a044\u00a0Ma to 278\u00a0\u00b1\u00a04\u00a0Ma) and Hf-O compositions [\u025bHf<\/sub>(t)\u00a0=\u00a0\u2212\u00a018.7 to +\u00a09.1 and 18<\/sup>O values <\u00a012.4\u2030] that broadly match those of zircons reported in nearby exposed crustal blocks of southwestern North America. We interpret these chromitite zircons as remnants of partly digested continental crust or continent-derived sediments on oceanic crust delivered into the mantle via subduction. They were captured by the parental melts of the chromitites when the latter formed in a supra-subduction zone mantle wedge polluted with crustal material. In addition, the Puerto Nuevo chromites have clinopyroxene lamellae with preferred crystallographic orientation, which we interpret as evidence that chromitites have experienced high-temperature and ultra high-pressure conditions (<\u00a012\u00a0GPa and ~\u00a01600 \u00b0C). We propose a tectonic scenario that involves the formation of chromitite in the supra-subduction zone mantle wedge underlying the Vizcaino intra-oceanic arc ca<\/em> 250\u00a0Ma ago, deep-mantle recycling, and subsequent diapiric exhumation in the intra-oceanic basin (the San Hip\u00f3lito marginal sea) generated during an extensional stage of the Vizcaino intra-oceanic arc ca<\/em> 221\u00a0Ma ago. The T<\/em>RD<\/sub> ages at ~\u00a0325 Ma record a partial melting event in the mantle prior to the construction of the Vizcaino intra-oceanic arc, which is probably related to the Permian continental subduction, dated at ~ 311\u00a0Ma.<\/p>\n

Keywords:<\/strong> Chromitite; zircon; UHP conditions; mantle recycling; Baja California<\/p>\n

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To Cite this article:<\/strong> \u00a0Gonz\u00e1lez-Jim\u00e9nez, J.M., Camprub\u00ed, A., Col\u00e1s, V., Griffin, W.L., Proenza, J.A., O'Reilly, S.Y., Centeno-Garc\u00eda,E., Garc\u00eda-Casco,A., Belousova, E., Talavera, C., Farr\u00e9-de-Pablo, J., Satsukawa, T., (2017). The recycling of chromitites in ophiolites from southwestern North America. Lithos<\/em>, (In Press)<\/p>\n

DOI<\/strong>: 10.1016\/j.lithos.2017.09.020<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"The recycling of chromitites in ophiolites from southwestern North America Podiform chromitites occur in mantle peridotites of the Late Triassic Puerto Nuevo Ophiolite, Baja California Sur State, Mexico. These are high-Cr chromitites [Cr# (Cr\/Cr\u00a0+\u00a0Al atomic ratio\u00a0=\u00a00.61\u20130.69] that contain a range of minor- and trace-elements and show whole-rock enrichment in IPGE (Os, Ir, Ru). These features are similar to those of Continue Reading<\/a>","protected":false},"author":3,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[127,50,44],"tags":[],"class_list":["post-3584","post","type-post","status-publish","format-standard","hentry","category-publications2017","category-mexico","category-publications","cat-127-id","cat-50-id","cat-44-id"],"_links":{"self":[{"href":"https:\/\/caribbeanlithos.ub.edu\/index.php?rest_route=\/wp\/v2\/posts\/3584","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/caribbeanlithos.ub.edu\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/caribbeanlithos.ub.edu\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/caribbeanlithos.ub.edu\/index.php?rest_route=\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/caribbeanlithos.ub.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=3584"}],"version-history":[{"count":1,"href":"https:\/\/caribbeanlithos.ub.edu\/index.php?rest_route=\/wp\/v2\/posts\/3584\/revisions"}],"predecessor-version":[{"id":3585,"href":"https:\/\/caribbeanlithos.ub.edu\/index.php?rest_route=\/wp\/v2\/posts\/3584\/revisions\/3585"}],"wp:attachment":[{"href":"https:\/\/caribbeanlithos.ub.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=3584"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/caribbeanlithos.ub.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=3584"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/caribbeanlithos.ub.edu\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=3584"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}