Matches in SemOpenAlex for { <https://semopenalex.org/work/W4308752104> ?p ?o ?g. }
- W4308752104 endingPage "591" @default.
- W4308752104 startingPage "569" @default.
- W4308752104 abstract "Abstract Detailed mineralogical and textural studies, combined with sequential X-ray diffraction and geochemical modeling, helped to solve the “copper pitch/wad” enigma in the Exótica deposit located downstream of the Chuquicamata porphyry copper deposit. Copper pitch and copper wad are essentially chrysocolla with co-precipitated Mn oxides, mainly birnessite, as well as pseudo-amorphous Mn oxide/oxyhydroxides. Linking the mineralogical, geochemical, and textural evidences with the geological, tectonic, and climatic evolution of the Chuquicamata–Calama area, a four-step genetic model for the evolution of the Exótica deposit is presented: (A) formation of a mature supergene enrichment profile at Chuquicamata (~ 30–25 Ma to ~ 15 Ma) during an erosion-dominated regime (∼900 m of erosion) which was accompanied by acidic (pH ∼2–4) Cu-Mn-Si-dominated rock drainage (ARD) with fluid flow southwards through the Exótica valley towards the Calama Basin, resulting in a strongly kaolinized and chrysocolla/copper wad-impregnated bedrock of the Exótica deposit; (B) deposition of the Fortuna gravels in the Exótica valley (starting ∼19 Ma) intercepted the Cu-Mn-Si-dominated ARD, triggering the main chrysocolla, copper pitch/wad mineralization as syn-sedimentary mineralization by chiefly surficial flow in strongly altered gravels; (C) tectonic freezing and onset of hyper-aridity (∼15–11 Ma) exposed the enriched chalcocite blanket of Chuquicamata to oxidation, resulting in acidic (pH ~ 2–4) and Cu-Si-dominated solutions with less Mn. These solutions percolated in a slightly more reducing groundwater flow path and mineralized relatively unaltered gravels with pure chrysocolla; and (D) ingression of confined chloride-rich groundwater in the upper oxidation zone of Chuquicamata, most likely between 6 and 3 Ma, is responsible for the atacamite/brochantite mineralization (pH ~ 5.5–7) of mainly unaltered gravels in the northern and central part of the Exótica deposit." @default.
- W4308752104 created "2022-11-15" @default.
- W4308752104 creator A5018148767 @default.
- W4308752104 creator A5029872460 @default.
- W4308752104 creator A5059683184 @default.
- W4308752104 date "2022-11-09" @default.
- W4308752104 modified "2023-10-06" @default.
- W4308752104 title "Genesis of the exotic chrysocolla — “copper pitch/wad” — atacamite/brochantite ore at the Exótica (Mina Sur) deposit, Chuquicamata, Chile" @default.
- W4308752104 cites W1251722559 @default.
- W4308752104 cites W1493276631 @default.
- W4308752104 cites W1966379292 @default.
- W4308752104 cites W1970852258 @default.
- W4308752104 cites W1985437050 @default.
- W4308752104 cites W1990173800 @default.
- W4308752104 cites W1994141623 @default.
- W4308752104 cites W1998282979 @default.
- W4308752104 cites W2000053414 @default.
- W4308752104 cites W2005252461 @default.
- W4308752104 cites W2005341647 @default.
- W4308752104 cites W2007216548 @default.
- W4308752104 cites W2008202850 @default.
- W4308752104 cites W2009347896 @default.
- W4308752104 cites W2009633732 @default.
- W4308752104 cites W2015089428 @default.
- W4308752104 cites W2017674019 @default.
- W4308752104 cites W2021022939 @default.
- W4308752104 cites W2025084080 @default.
- W4308752104 cites W2025127061 @default.
- W4308752104 cites W2028952055 @default.
- W4308752104 cites W2030491571 @default.
- W4308752104 cites W2031975542 @default.
- W4308752104 cites W2045385221 @default.
- W4308752104 cites W2047919013 @default.
- W4308752104 cites W2048411058 @default.
- W4308752104 cites W2054327178 @default.
- W4308752104 cites W2063079305 @default.
- W4308752104 cites W2082568683 @default.
- W4308752104 cites W2087395343 @default.
- W4308752104 cites W2088591746 @default.
- W4308752104 cites W2095237431 @default.
- W4308752104 cites W2099568524 @default.
- W4308752104 cites W2104627768 @default.
- W4308752104 cites W2112747287 @default.
- W4308752104 cites W2114514935 @default.
- W4308752104 cites W2125900060 @default.
- W4308752104 cites W2126145881 @default.
- W4308752104 cites W2134062393 @default.
- W4308752104 cites W2140513964 @default.
- W4308752104 cites W2160147971 @default.
- W4308752104 cites W2160866493 @default.
- W4308752104 cites W2168693702 @default.
- W4308752104 cites W2315673757 @default.
- W4308752104 cites W2317682131 @default.
- W4308752104 cites W2461019936 @default.
- W4308752104 cites W2520777900 @default.
- W4308752104 cites W2605364278 @default.
- W4308752104 cites W2740340687 @default.
- W4308752104 cites W2767990587 @default.
- W4308752104 cites W2772331667 @default.
- W4308752104 cites W2981154952 @default.
- W4308752104 cites W3005762344 @default.
- W4308752104 cites W3011131404 @default.
- W4308752104 cites W3109261278 @default.
- W4308752104 cites W4309490214 @default.
- W4308752104 doi "https://doi.org/10.1007/s00126-022-01147-7" @default.
- W4308752104 hasPublicationYear "2022" @default.
- W4308752104 type Work @default.
- W4308752104 citedByCount "2" @default.
- W4308752104 countsByYear W43087521042022 @default.
- W4308752104 countsByYear W43087521042023 @default.
- W4308752104 crossrefType "journal-article" @default.
- W4308752104 hasAuthorship W4308752104A5018148767 @default.
- W4308752104 hasAuthorship W4308752104A5029872460 @default.
- W4308752104 hasAuthorship W4308752104A5059683184 @default.
- W4308752104 hasBestOaLocation W43087521041 @default.
- W4308752104 hasConcept C111696902 @default.
- W4308752104 hasConcept C127313418 @default.
- W4308752104 hasConcept C145761182 @default.
- W4308752104 hasConcept C151730666 @default.
- W4308752104 hasConcept C156622251 @default.
- W4308752104 hasConcept C159390177 @default.
- W4308752104 hasConcept C159750122 @default.
- W4308752104 hasConcept C17409809 @default.
- W4308752104 hasConcept C179319051 @default.
- W4308752104 hasConcept C191897082 @default.
- W4308752104 hasConcept C192562407 @default.
- W4308752104 hasConcept C199289684 @default.
- W4308752104 hasConcept C2776062231 @default.
- W4308752104 hasConcept C2776152364 @default.
- W4308752104 hasConcept C2776161269 @default.
- W4308752104 hasConcept C2776268066 @default.
- W4308752104 hasConcept C2778188036 @default.
- W4308752104 hasConcept C544778455 @default.
- W4308752104 hasConceptScore W4308752104C111696902 @default.
- W4308752104 hasConceptScore W4308752104C127313418 @default.
- W4308752104 hasConceptScore W4308752104C145761182 @default.
- W4308752104 hasConceptScore W4308752104C151730666 @default.
- W4308752104 hasConceptScore W4308752104C156622251 @default.