FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2078996970> ?p ?o ?g. }

• W2078996970 endingPage "36" @default.
• W2078996970 startingPage "27" @default.
• W2078996970 abstract "This contribution presents the first detailed three-dimensional (3D) in situ analysis of samples from the Platinova Reef using high-resolution X-ray computed tomography (HRXCT) and 3D image processing and quantification coupled with microscopic and mineralogical investigations. Our HRXCT analyses reveal the complex textural relationships between Cu-rich sulfides (bulk composition close to bornite), skaergaardite (PdCu), Au-rich phases, silicates and Fe–Ti oxides and provide unequivocal textural evidences, not observed previously. The association in 3D between Cu-rich sulfide globules, PdCu alloy and ilmenite is inconsistent with a hydrothermal origin of the Cu–Pd mineralization. In contrast, our results combined with phase diagrams strongly support a primary magmatic origin for the Cu–Pd mineralization where Cu and Pd-rich, Fe-poor sulfide liquid represents a cumulus phase that forms by in-situ nucleation. These sulfide droplets and attached skaergaardite grains were trapped during the formation and crystallization of the Fe–Ti oxides. Subsequent, post-cumulus processes led to the partial to total dissolution of the sulfide not entirely enclosed by the Fe–Ti oxides (i.e., not protected from reaction) leading to the observed variability in Cu and Pd composition at the aggregate (sulfide + PdCu) scale and to the occurrence of free PdCu alloys. In contrast to the PdCu alloy, gold-bearing minerals are never observed entirely enclosed within the Fe–Ti oxide. Two hypotheses can be envisaged for the formation of the gold enriched layer in the upper part of the section. Gold may have either precipitated from high-temperature late magmatic Cl-rich fluids. Alternatively, gold may have been enriched during fractional crystallization after sulfide had been suppressed from the liquidus after the Pd layer crystallized and then deposited along redox barriers." @default.
• W2078996970 created "2016-06-24" @default.
• W2078996970 creator A5003263764 @default.
• W2078996970 creator A5021493186 @default.
• W2078996970 creator A5024616951 @default.
• W2078996970 creator A5062486950 @default.
• W2078996970 creator A5066725570 @default.
• W2078996970 date "2014-03-01" @default.
• W2078996970 modified "2023-10-11" @default.
• W2078996970 title "New constraints on the origin of the Skaergaard intrusion Cu–Pd–Au mineralization: Insights from high-resolution X-ray computed tomography" @default.
• W2078996970 cites W1966271824 @default.
• W2078996970 cites W1968887232 @default.
• W2078996970 cites W1978220312 @default.
• W2078996970 cites W1988212575 @default.
• W2078996970 cites W1988983585 @default.
• W2078996970 cites W1990495548 @default.
• W2078996970 cites W1996694420 @default.
• W2078996970 cites W2010238900 @default.
• W2078996970 cites W2018827851 @default.
• W2078996970 cites W2019940244 @default.
• W2078996970 cites W2027411519 @default.
• W2078996970 cites W2048225899 @default.
• W2078996970 cites W2053890542 @default.
• W2078996970 cites W2056309858 @default.
• W2078996970 cites W2067686007 @default.
• W2078996970 cites W2073172102 @default.
• W2078996970 cites W2074294092 @default.
• W2078996970 cites W2078638796 @default.
• W2078996970 cites W2086041827 @default.
• W2078996970 cites W2086341988 @default.
• W2078996970 cites W2088516428 @default.
• W2078996970 cites W2093756915 @default.
• W2078996970 cites W2098066044 @default.
• W2078996970 cites W2101749172 @default.
• W2078996970 cites W2118309612 @default.
• W2078996970 cites W2124378120 @default.
• W2078996970 cites W2128405318 @default.
• W2078996970 cites W2144115675 @default.
• W2078996970 cites W2150313486 @default.
• W2078996970 cites W2156496998 @default.
• W2078996970 cites W2159059589 @default.
• W2078996970 cites W2162799868 @default.
• W2078996970 cites W2164050431 @default.
• W2078996970 cites W2165143147 @default.
• W2078996970 cites W2312708266 @default.
• W2078996970 cites W2317619881 @default.
• W2078996970 cites W2322073502 @default.
• W2078996970 cites W4248561747 @default.
• W2078996970 doi "https://doi.org/10.1016/j.lithos.2013.11.019" @default.
• W2078996970 hasPublicationYear "2014" @default.
• W2078996970 type Work @default.
• W2078996970 sameAs 2078996970 @default.
• W2078996970 citedByCount "29" @default.
• W2078996970 countsByYear W20789969702013 @default.
• W2078996970 countsByYear W20789969702015 @default.
• W2078996970 countsByYear W20789969702016 @default.
• W2078996970 countsByYear W20789969702017 @default.
• W2078996970 countsByYear W20789969702019 @default.
• W2078996970 countsByYear W20789969702020 @default.
• W2078996970 countsByYear W20789969702021 @default.
• W2078996970 crossrefType "journal-article" @default.
• W2078996970 hasAuthorship W2078996970A5003263764 @default.
• W2078996970 hasAuthorship W2078996970A5021493186 @default.
• W2078996970 hasAuthorship W2078996970A5024616951 @default.
• W2078996970 hasAuthorship W2078996970A5062486950 @default.
• W2078996970 hasAuthorship W2078996970A5066725570 @default.
• W2078996970 hasConcept C111696902 @default.
• W2078996970 hasConcept C127313418 @default.
• W2078996970 hasConcept C147789679 @default.
• W2078996970 hasConcept C156622251 @default.
• W2078996970 hasConcept C159390177 @default.
• W2078996970 hasConcept C159750122 @default.
• W2078996970 hasConcept C165205528 @default.
• W2078996970 hasConcept C16876290 @default.
• W2078996970 hasConcept C17409809 @default.
• W2078996970 hasConcept C178790620 @default.
• W2078996970 hasConcept C185592680 @default.
• W2078996970 hasConcept C191897082 @default.
• W2078996970 hasConcept C192562407 @default.
• W2078996970 hasConcept C199289684 @default.
• W2078996970 hasConcept C203036418 @default.
• W2078996970 hasConcept C2776989079 @default.
• W2078996970 hasConcept C2777335606 @default.
• W2078996970 hasConcept C2778188036 @default.
• W2078996970 hasConcept C2780026712 @default.
• W2078996970 hasConcept C2780596425 @default.
• W2078996970 hasConcept C544778455 @default.
• W2078996970 hasConcept C61048295 @default.
• W2078996970 hasConcept C88380143 @default.
• W2078996970 hasConceptScore W2078996970C111696902 @default.
• W2078996970 hasConceptScore W2078996970C127313418 @default.
• W2078996970 hasConceptScore W2078996970C147789679 @default.
• W2078996970 hasConceptScore W2078996970C156622251 @default.
• W2078996970 hasConceptScore W2078996970C159390177 @default.
• W2078996970 hasConceptScore W2078996970C159750122 @default.
• W2078996970 hasConceptScore W2078996970C165205528 @default.
• W2078996970 hasConceptScore W2078996970C16876290 @default.
• W2078996970 hasConceptScore W2078996970C17409809 @default.

• next