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• W2112292068 endingPage "310" @default.
• W2112292068 startingPage "281" @default.
• W2112292068 abstract "Raul-Condestable is a >32 million metric ton (Mt) iron oxide-copper-gold (IOCG) deposit located on the Peruvian coast, 90 km south of Lima. The ore occurs as veins, replacement “mantos,” and disseminations consisting of a chalcopyrite-pyrite-pyrrhotite-magnetite-amphibole mineral association. The geology of the studied area comprises a series of superposed volcanic edifices of Late Jurassic to Early Cretaceous age, which are part of a larger volcanic island to continental arc system. Particularly good exposures of the tilted host sequence allow the mapping of the Raul-Condestable IOCG deposit in a nearly complete oblique cross section, from its associated volcanic edifice down to a paleodepth of about 6 km.U-Pb zircon ages indicate that in the deposit area felsic magmatic activity took place between 116.7 ± 0.4 and 114.5 ± 1 Ma, defining a new Raul-Condestable superunit, the oldest so far, of the Peruvian Coastal batholith. This superunit is located west of the main part of the batholith and includes a dacite-andesite volcanic dome and a subvolcanic quartz-diorite porphyry sill-dike complex that were emplaced at 116.7 ± 0.4 and 116.4 ±0.3 Ma, respectively, followed by tonalite stocks and dikes emplaced between 115.1 ± 0.4 and 114.5 ± 1 Ma. All these rocks contain hornblende and/or biotite but no pyroxene and correspond to silica- and water-rich magmas following a calcic differentiation trend. Hf isotope data on zircons (eHf(115 Ma) = 5.2–7.5) and Pb isotope data on whole rock, combined with lithogeochemical results, suggest that magmas were generated by partial melting of the upper mantle, enriched through hydrous metasomatism and/or melting of subducted pelagic sediments. The lack of zircon inheritance suggests that there was no direct involvement of continental crust.The Raul-Condestable IOCG deposit is connected in space and time with the magmatism of the Raul-Condestable superunit. The mineralization was emplaced in the core of the dacite-andesite volcanic dome at a paleodepth of 2 to 3 km, surrounding two tonalitic intrusions formed at 115.1 ± 0.4 and 114.8 ± 0.4 Ma. The U-Pb age of hydrothermal titanite from IOCG veins at 115.2 ± 0.3 Ma indicates that the mineralization was coeval with (or more probably just followed) the emplacement of the tonalites. Re-Os geochronology on molybdenite did not yield reliable ages due to apparent Re loss. Copper ore is associated with a zoned alteration pattern, which surrounds the tonalite intrusions. It consists of a core of biotite alteration and quartz stockwork, grading outward to actinolite (±magnetite, ±chlorite, ±titanite, ±scapolite, ±albite, ±epidote) and upward to sericite + Fe chlorite alteration. An upper distal alteration halo consisting of hematite-chlorite surrounds the sericite + Fe chlorite and actinolite alterations laterally. Most of the ore is spatially associated with the actinolite alteration and, to a lesser extent, with the sericite + Fe chlorite alteration.The results of this study confirm that the 110 to 120 Ma age range was a productive time period for Andean IOCG deposits. The characterization of the hydrous intermediate magmatism related to the mineralization, as well as the subvolcanic position of the deposit and its related alteration pattern provides further criteria that may be used when exploring for IOCG deposits in a convergent plate tectonic setting." @default.
• W2112292068 created "2016-06-24" @default.
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• W2112292068 date "2006-03-01" @default.
• W2112292068 modified "2023-10-14" @default.
• W2112292068 title "Geology, Geochronology, and Hf and Pb Isotope Data of the Raul-Condestable Iron Oxide-Copper-Gold Deposit, Central Coast of Peru" @default.
• W2112292068 cites W1463933811 @default.
• W2112292068 cites W1487925322 @default.
• W2112292068 cites W1840617620 @default.
• W2112292068 cites W1966256034 @default.
• W2112292068 cites W1967781858 @default.
• W2112292068 cites W1972298961 @default.
• W2112292068 cites W1979226709 @default.
• W2112292068 cites W1979350315 @default.
• W2112292068 cites W1979840893 @default.
• W2112292068 cites W1986560096 @default.
• W2112292068 cites W1990479851 @default.
• W2112292068 cites W1993118225 @default.
• W2112292068 cites W1997554728 @default.
• W2112292068 cites W1997620033 @default.
• W2112292068 cites W1998788737 @default.
• W2112292068 cites W1999448338 @default.
• W2112292068 cites W2003320318 @default.
• W2112292068 cites W2007105153 @default.
• W2112292068 cites W2016346688 @default.
• W2112292068 cites W2018932028 @default.
• W2112292068 cites W2021027438 @default.
• W2112292068 cites W2022443246 @default.
• W2112292068 cites W2036174339 @default.
• W2112292068 cites W2037717521 @default.
• W2112292068 cites W2039475184 @default.
• W2112292068 cites W2052431885 @default.
• W2112292068 cites W2053483240 @default.
• W2112292068 cites W2058374690 @default.
• W2112292068 cites W2068872642 @default.
• W2112292068 cites W2072011734 @default.
• W2112292068 cites W2082735341 @default.
• W2112292068 cites W2084049583 @default.
• W2112292068 cites W2084158493 @default.
• W2112292068 cites W2084165122 @default.
• W2112292068 cites W2088496938 @default.
• W2112292068 cites W2090206242 @default.
• W2112292068 cites W2090782858 @default.
• W2112292068 cites W2093369526 @default.
• W2112292068 cites W2097419136 @default.
• W2112292068 cites W2099690139 @default.
• W2112292068 cites W2108971421 @default.
• W2112292068 cites W2123103778 @default.
• W2112292068 cites W2126950045 @default.
• W2112292068 cites W2141870408 @default.
• W2112292068 cites W2145087726 @default.
• W2112292068 cites W2145191782 @default.
• W2112292068 cites W2151802570 @default.
• W2112292068 cites W2152640919 @default.
• W2112292068 cites W2157099954 @default.
• W2112292068 cites W2158440327 @default.
• W2112292068 cites W2161212300 @default.
• W2112292068 cites W2164886516 @default.
• W2112292068 cites W2169061213 @default.
• W2112292068 cites W2171268542 @default.
• W2112292068 cites W2172005127 @default.
• W2112292068 cites W2337978405 @default.
• W2112292068 cites W2339962540 @default.
• W2112292068 cites W2402024000 @default.
• W2112292068 cites W2472665562 @default.
• W2112292068 cites W2474587399 @default.
• W2112292068 cites W2480318151 @default.
• W2112292068 cites W2482154883 @default.
• W2112292068 cites W2486739643 @default.
• W2112292068 cites W2487469852 @default.
• W2112292068 cites W2494237538 @default.
• W2112292068 cites W2494499189 @default.
• W2112292068 cites W2494613522 @default.
• W2112292068 cites W2495009811 @default.
• W2112292068 cites W2502297619 @default.
• W2112292068 cites W2504775913 @default.
• W2112292068 cites W2505358784 @default.
• W2112292068 cites W2782851545 @default.
• W2112292068 cites W2797914455 @default.
• W2112292068 cites W2977803073 @default.
• W2112292068 cites W3143976556 @default.
• W2112292068 cites W382344604 @default.
• W2112292068 cites W83901612 @default.
• W2112292068 doi "https://doi.org/10.2113/gsecongeo.101.2.281" @default.
• W2112292068 hasPublicationYear "2006" @default.
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