FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2086695643> ?p ?o ?g. }

• W2086695643 endingPage "331" @default.
• W2086695643 startingPage "306" @default.
• W2086695643 abstract "The Aitik Cu–Au–Ag deposit in the Gällivare area in northern Sweden is Sweden's largest sulphide mine with an annual production of 35 Mt of ore, and the biggest open pit operation in northern Europe. It is proposed in the present study that the Aitik deposit represents a Palaeoproterozoic, strongly metamorphosed porphyry copper deposit that was affected ca. 100 Ma later by a regional IOCG-type hydrothermal event. Consequently, the Aitik deposit might represent a mixed ore system where an early copper mineralisation of porphyry type has been overprinted by later regional IOCG mineralisation. Several attempts have previously been made to genetically classify the Aitik Cu–Au–Ag deposit as a distinct ore type. New geochemical, petrographic, structural, and fluid inclusion results combined with published data have provided the opportunity to present new ideas on the genesis and evolution of the Aitik Cu–Au–Ag deposit. The emplacement of a ca. 1.9 Ga quartz monzodiorite that host the ore at Aitik was related to subduction processes and volcanic arc formation, and synchronous with quartz vein stockwork formation and porphyry copper mineralisation. Highly saline aqueous (38 wt.% NaCl) fluid inclusions in the stockwork veins suggest entrapment at 300 °C and a pressure of nearly 3 kbar, a high pressure for a typical porphyry copper ore, but consistent with conditions at associated deep root zones of intrusion-related magmatic–hydrothermal systems. The highly saline fluid formed disseminated and vein-type ore of mainly chalcopyrite and pyrite within comagmatic volcaniclastic rocks, and caused potassic alteration (biotite, microcline) of the host rocks. The early porphyry copper mineralising event was followed, and largely overprinted, by CO2 and aqueous medium- to high-salinity (16–57 wt.% salts) fluids related to a ca. 1.8 Ga tectonic and metamorphic event (peak conditions 500–600 °C and 4–5 kbar). Extensive deformation of rocks and redistribution of metals occurred. Magnetite enrichment locally found within late veins, and late amphibole–scapolite and K feldspar alterations within the deposit, are some of the features at Aitik implying that aqueous fluids responsible for IOCG-mineralisation (200–500 °C and ~ 1 kbar) and extensive Na–Ca alteration in the region during the 1.8 Ga tectonic event also affected the Aitik rocks, possibly leading to addition of copper ± gold." @default.
• W2086695643 created "2016-06-24" @default.
• W2086695643 creator A5010874009 @default.
• W2086695643 creator A5038414423 @default.
• W2086695643 creator A5053004584 @default.
• W2086695643 creator A5058047476 @default.
• W2086695643 date "2012-10-01" @default.
• W2086695643 modified "2023-10-04" @default.
• W2086695643 title "Modification of a Palaeoproterozoic porphyry-like system: Integration of structural, geochemical, petrographic, and fluid inclusion data from the Aitik Cu–Au–Ag deposit, northern Sweden" @default.
• W2086695643 cites W1983070632 @default.
• W2086695643 cites W1985738992 @default.
• W2086695643 cites W1986234848 @default.
• W2086695643 cites W1986513808 @default.
• W2086695643 cites W1992540434 @default.
• W2086695643 cites W1993069350 @default.
• W2086695643 cites W1994707220 @default.
• W2086695643 cites W1995585326 @default.
• W2086695643 cites W1995836922 @default.
• W2086695643 cites W1999726370 @default.
• W2086695643 cites W2004860018 @default.
• W2086695643 cites W2006254307 @default.
• W2086695643 cites W2007554608 @default.
• W2086695643 cites W2011570175 @default.
• W2086695643 cites W2019213549 @default.
• W2086695643 cites W2020161194 @default.
• W2086695643 cites W2026295157 @default.
• W2086695643 cites W2032281091 @default.
• W2086695643 cites W2033962780 @default.
• W2086695643 cites W2035130206 @default.
• W2086695643 cites W2035396352 @default.
• W2086695643 cites W2036136099 @default.
• W2086695643 cites W2044537972 @default.
• W2086695643 cites W2053678543 @default.
• W2086695643 cites W2061839670 @default.
• W2086695643 cites W2062520073 @default.
• W2086695643 cites W2063092772 @default.
• W2086695643 cites W2073722995 @default.
• W2086695643 cites W2074192572 @default.
• W2086695643 cites W2076153543 @default.
• W2086695643 cites W2076378393 @default.
• W2086695643 cites W2084771003 @default.
• W2086695643 cites W2091694423 @default.
• W2086695643 cites W2102905140 @default.
• W2086695643 cites W2107722941 @default.
• W2086695643 cites W2108971421 @default.
• W2086695643 cites W2130304433 @default.
• W2086695643 cites W2133632958 @default.
• W2086695643 cites W2137318766 @default.
• W2086695643 cites W2153415869 @default.
• W2086695643 cites W2165394332 @default.
• W2086695643 cites W2317337219 @default.
• W2086695643 cites W4243899842 @default.
• W2086695643 doi "https://doi.org/10.1016/j.oregeorev.2012.05.002" @default.
• W2086695643 hasPublicationYear "2012" @default.
• W2086695643 type Work @default.
• W2086695643 sameAs 2086695643 @default.
• W2086695643 citedByCount "37" @default.
• W2086695643 countsByYear W20866956432013 @default.
• W2086695643 countsByYear W20866956432014 @default.
• W2086695643 countsByYear W20866956432015 @default.
• W2086695643 countsByYear W20866956432016 @default.
• W2086695643 countsByYear W20866956432017 @default.
• W2086695643 countsByYear W20866956432018 @default.
• W2086695643 countsByYear W20866956432019 @default.
• W2086695643 countsByYear W20866956432020 @default.
• W2086695643 countsByYear W20866956432021 @default.
• W2086695643 countsByYear W20866956432022 @default.
• W2086695643 countsByYear W20866956432023 @default.
• W2086695643 crossrefType "journal-article" @default.
• W2086695643 hasAuthorship W2086695643A5010874009 @default.
• W2086695643 hasAuthorship W2086695643A5038414423 @default.
• W2086695643 hasAuthorship W2086695643A5053004584 @default.
• W2086695643 hasAuthorship W2086695643A5058047476 @default.
• W2086695643 hasBestOaLocation W20866956431 @default.
• W2086695643 hasConcept C127313418 @default.
• W2086695643 hasConcept C140167661 @default.
• W2086695643 hasConcept C151730666 @default.
• W2086695643 hasConcept C17409809 @default.
• W2086695643 hasConcept C178790620 @default.
• W2086695643 hasConcept C179319051 @default.
• W2086695643 hasConcept C185592680 @default.
• W2086695643 hasConcept C2776152364 @default.
• W2086695643 hasConcept C2778188036 @default.
• W2086695643 hasConcept C2779870107 @default.
• W2086695643 hasConcept C544778455 @default.
• W2086695643 hasConcept C59235061 @default.
• W2086695643 hasConcept C62074269 @default.
• W2086695643 hasConcept C69883797 @default.
• W2086695643 hasConcept C7145564 @default.
• W2086695643 hasConceptScore W2086695643C127313418 @default.
• W2086695643 hasConceptScore W2086695643C140167661 @default.
• W2086695643 hasConceptScore W2086695643C151730666 @default.
• W2086695643 hasConceptScore W2086695643C17409809 @default.
• W2086695643 hasConceptScore W2086695643C178790620 @default.
• W2086695643 hasConceptScore W2086695643C179319051 @default.
• W2086695643 hasConceptScore W2086695643C185592680 @default.
• W2086695643 hasConceptScore W2086695643C2776152364 @default.
• W2086695643 hasConceptScore W2086695643C2778188036 @default.

• next