FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2334913409> ?p ?o ?g. }

• W2334913409 endingPage "27" @default.
• W2334913409 startingPage "11" @default.
• W2334913409 abstract "Abstract Cobaltite-rich mineralization from the iron skarns of the Traversella magnetite mine (Western Alps, Italy) was studied by reflected-light microscopy, scanning electron microscopy and electron microprobe analysis. Cobaltite is found in carbonate-chlorite-rich rocks at the margins of the main magnetite masses, where it forms disseminations and metasomatic veinlets that postdate the formation of magnetite. The paragenesis includes cobaltite (± arsenopyrite), bismuthinite, pyrrhotite and/or pyrite, chalcopyrite, carbonates, talc, chlorite and native gold, and is indicative of a low-sulfidation environment. The sulfarsenides show oscillatory and sector zoning, which indicates disequilibrium during crystal growth. Compositional variations are mainly due to variations in the Co/Fe ratio of arsenopyrite and in either the Co/Fe or the Ni/(Fe + Co) ratios of the coexisting cobaltite. The Ni contents are low to very low in the cobaltites (<2.4 wt.%) and very low in the arsenopyrites (<0.16 wt.%). The As/S molar ratios in the cobaltites are highly variable (0.59−1.00) and show a broad negative correlation with the Fe contents. The formation of cobaltite is related to circulation of relatively low-temperature (<∼300°C), (Co,As,Bi)-rich fluids during the retrograde sulfidation stage which followed the formation of magnetite. The apparent restriction of cobaltite (+ bismuthinite ± arsenopyrite) to the margins of the main magnetite columns may reflect the establishment of thermochemical gradients around the main direction of infiltration of the retrograde metasomatic fluids." @default.
• W2334913409 created "2016-06-24" @default.
• W2334913409 creator A5011366005 @default.
• W2334913409 creator A5052169725 @default.
• W2334913409 creator A5081283663 @default.
• W2334913409 date "2014-02-01" @default.
• W2334913409 modified "2023-09-27" @default.
• W2334913409 title "Cobaltite-rich mineralization in the iron skarn deposit of Traversella (Western Alps, Italy)" @default.
• W2334913409 cites W1552987301 @default.
• W2334913409 cites W1622613714 @default.
• W2334913409 cites W1742186271 @default.
• W2334913409 cites W1768668241 @default.
• W2334913409 cites W1840966411 @default.
• W2334913409 cites W1857091209 @default.
• W2334913409 cites W1978344910 @default.
• W2334913409 cites W1982563599 @default.
• W2334913409 cites W1986091094 @default.
• W2334913409 cites W1989154693 @default.
• W2334913409 cites W2014555977 @default.
• W2334913409 cites W2031034433 @default.
• W2334913409 cites W2034325628 @default.
• W2334913409 cites W2037209502 @default.
• W2334913409 cites W2038386308 @default.
• W2334913409 cites W2043570922 @default.
• W2334913409 cites W2064681627 @default.
• W2334913409 cites W2069155653 @default.
• W2334913409 cites W2075611904 @default.
• W2334913409 cites W2076292928 @default.
• W2334913409 cites W2079433871 @default.
• W2334913409 cites W2088655856 @default.
• W2334913409 cites W2095570691 @default.
• W2334913409 cites W2108901033 @default.
• W2334913409 cites W2124375364 @default.
• W2334913409 cites W2125848658 @default.
• W2334913409 cites W2131202135 @default.
• W2334913409 cites W2148515586 @default.
• W2334913409 cites W2154854395 @default.
• W2334913409 cites W2164925786 @default.
• W2334913409 cites W2169891700 @default.
• W2334913409 cites W2486094809 @default.
• W2334913409 cites W2980495961 @default.
• W2334913409 cites W3176590998 @default.
• W2334913409 cites W4239182258 @default.
• W2334913409 doi "https://doi.org/10.1180/minmag.2014.078.1.02" @default.
• W2334913409 hasPublicationYear "2014" @default.
• W2334913409 type Work @default.
• W2334913409 sameAs 2334913409 @default.
• W2334913409 citedByCount "8" @default.
• W2334913409 countsByYear W23349134092015 @default.
• W2334913409 countsByYear W23349134092016 @default.
• W2334913409 countsByYear W23349134092017 @default.
• W2334913409 countsByYear W23349134092019 @default.
• W2334913409 countsByYear W23349134092020 @default.
• W2334913409 countsByYear W23349134092021 @default.
• W2334913409 countsByYear W23349134092022 @default.
• W2334913409 countsByYear W23349134092023 @default.
• W2334913409 crossrefType "journal-article" @default.
• W2334913409 hasAuthorship W2334913409A5011366005 @default.
• W2334913409 hasAuthorship W2334913409A5052169725 @default.
• W2334913409 hasAuthorship W2334913409A5081283663 @default.
• W2334913409 hasConcept C127313418 @default.
• W2334913409 hasConcept C151730666 @default.
• W2334913409 hasConcept C154401813 @default.
• W2334913409 hasConcept C167919410 @default.
• W2334913409 hasConcept C17409809 @default.
• W2334913409 hasConcept C191897082 @default.
• W2334913409 hasConcept C192562407 @default.
• W2334913409 hasConcept C195843664 @default.
• W2334913409 hasConcept C199289684 @default.
• W2334913409 hasConcept C26687426 @default.
• W2334913409 hasConcept C2776152364 @default.
• W2334913409 hasConcept C2776230739 @default.
• W2334913409 hasConcept C2777781897 @default.
• W2334913409 hasConcept C2778188036 @default.
• W2334913409 hasConcept C2778420536 @default.
• W2334913409 hasConcept C2778635928 @default.
• W2334913409 hasConcept C2778998827 @default.
• W2334913409 hasConcept C2779870107 @default.
• W2334913409 hasConcept C2780364934 @default.
• W2334913409 hasConcept C2780756512 @default.
• W2334913409 hasConcept C544778455 @default.
• W2334913409 hasConcept C67236022 @default.
• W2334913409 hasConceptScore W2334913409C127313418 @default.
• W2334913409 hasConceptScore W2334913409C151730666 @default.
• W2334913409 hasConceptScore W2334913409C154401813 @default.
• W2334913409 hasConceptScore W2334913409C167919410 @default.
• W2334913409 hasConceptScore W2334913409C17409809 @default.
• W2334913409 hasConceptScore W2334913409C191897082 @default.
• W2334913409 hasConceptScore W2334913409C192562407 @default.
• W2334913409 hasConceptScore W2334913409C195843664 @default.
• W2334913409 hasConceptScore W2334913409C199289684 @default.
• W2334913409 hasConceptScore W2334913409C26687426 @default.
• W2334913409 hasConceptScore W2334913409C2776152364 @default.
• W2334913409 hasConceptScore W2334913409C2776230739 @default.
• W2334913409 hasConceptScore W2334913409C2777781897 @default.
• W2334913409 hasConceptScore W2334913409C2778188036 @default.
• W2334913409 hasConceptScore W2334913409C2778420536 @default.
• W2334913409 hasConceptScore W2334913409C2778635928 @default.

• next