FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2052783267> ?p ?o ?g. }

• W2052783267 endingPage "440" @default.
• W2052783267 startingPage "423" @default.
• W2052783267 abstract "The Mengku iron deposit (110 Mt at 44% Fe) in the eastern extension of the Rudnyi Altai mineral belt, Xinjiang, NW China, is hosted in an Early Devonian volcano-sedimentary sequence affected by prograde skarn formation (clinopyroxene, garnet, scapolite and albite) and retrograde alteration (actinolite, epidote, chlorite and apatite). Ore minerals are magnetite, with minor chalcopyrite, pyrrhotite and pyrite. Gangue minerals include predominantly diopside, andradite, epidote, chlorite, quartz and calcite. Fluid inclusions in garnet and clinopyroxene yield homogenization temperatures (Th) of 241–500 °C, and salinities of 9.6–13.0 wt.% NaCl equivalent. Fluid inclusions in quartz consist of two varieties: (1) liquid–vapor–solid inclusions with (Th) of 348–458 °C and salinities of 38.2–57.1 wt.%, and (2) two-phase inclusions with (Th) of 166–382 °C and salinities of 9.6–13.0 wt.% NaCl equivalent. Two-phase inclusions in calcite vary from 145 to 265 °C, with salinities of 1.2–9.6 wt.% NaCl equivalent. The fluid evolution progressed from high temperature and moderate salinity (prograde skarn stage) to moderate T and salinity (retrograde stage), to low T and salinity (sulfide stage). Stable isotope data of quartz and calcite (−84‰ to −110‰ δD, 5.5–7.0‰ δ18OSMOW, and −3.8‰ to −6.1‰ δ13CPDB) reflect late-stage interaction of meteoric water with granitic rocks. Skarn formation was likely related to a Late Devonian tonalite (378 ± 7 Ma, U–Pb zircon age). The geological and geochemical evidence suggests magnetite skarn formation from granite-related fluids which reacted with andesitic to mafic volcanics and their intercalated carbonate beds and lenses, contrary to earlier interpretations of the deposit as of synsedimentary-exhalative origin or related to iron–oxide magma." @default.
• W2052783267 created "2016-06-24" @default.
• W2052783267 creator A5036493852 @default.
• W2052783267 creator A5039955400 @default.
• W2052783267 creator A5045190155 @default.
• W2052783267 creator A5045840456 @default.
• W2052783267 creator A5048297380 @default.
• W2052783267 date "2010-10-01" @default.
• W2052783267 modified "2023-10-11" @default.
• W2052783267 title "Geology, geochemistry and age constraints on the Mengku skarn iron deposit in Xinjiang Altai, NW China" @default.
• W2052783267 cites W1964276781 @default.
• W2052783267 cites W1971284558 @default.
• W2052783267 cites W1985570636 @default.
• W2052783267 cites W1989068278 @default.
• W2052783267 cites W2008281306 @default.
• W2052783267 cites W2018006495 @default.
• W2052783267 cites W2025925515 @default.
• W2052783267 cites W2027857855 @default.
• W2052783267 cites W2030696126 @default.
• W2052783267 cites W2038449935 @default.
• W2052783267 cites W2044496537 @default.
• W2052783267 cites W2047807381 @default.
• W2052783267 cites W2065065857 @default.
• W2052783267 cites W2068202901 @default.
• W2052783267 cites W2080273792 @default.
• W2052783267 cites W2080522683 @default.
• W2052783267 cites W2089096123 @default.
• W2052783267 cites W2090757504 @default.
• W2052783267 cites W2092778941 @default.
• W2052783267 cites W2092868748 @default.
• W2052783267 cites W2103942973 @default.
• W2052783267 cites W2127456773 @default.
• W2052783267 cites W2132769552 @default.
• W2052783267 cites W2141599763 @default.
• W2052783267 cites W2145604970 @default.
• W2052783267 cites W2156540401 @default.
• W2052783267 cites W2164925786 @default.
• W2052783267 cites W2994817661 @default.
• W2052783267 cites W2995482781 @default.
• W2052783267 cites W3094394634 @default.
• W2052783267 cites W4243196258 @default.
• W2052783267 doi "https://doi.org/10.1016/j.jseaes.2010.04.005" @default.
• W2052783267 hasPublicationYear "2010" @default.
• W2052783267 type Work @default.
• W2052783267 sameAs 2052783267 @default.
• W2052783267 citedByCount "31" @default.
• W2052783267 countsByYear W20527832672012 @default.
• W2052783267 countsByYear W20527832672013 @default.
• W2052783267 countsByYear W20527832672014 @default.
• W2052783267 countsByYear W20527832672015 @default.
• W2052783267 countsByYear W20527832672017 @default.
• W2052783267 countsByYear W20527832672018 @default.
• W2052783267 countsByYear W20527832672019 @default.
• W2052783267 countsByYear W20527832672020 @default.
• W2052783267 countsByYear W20527832672021 @default.
• W2052783267 crossrefType "journal-article" @default.
• W2052783267 hasAuthorship W2052783267A5036493852 @default.
• W2052783267 hasAuthorship W2052783267A5039955400 @default.
• W2052783267 hasAuthorship W2052783267A5045190155 @default.
• W2052783267 hasAuthorship W2052783267A5045840456 @default.
• W2052783267 hasAuthorship W2052783267A5048297380 @default.
• W2052783267 hasConcept C127313418 @default.
• W2052783267 hasConcept C151730666 @default.
• W2052783267 hasConcept C156622251 @default.
• W2052783267 hasConcept C15785431 @default.
• W2052783267 hasConcept C165205528 @default.
• W2052783267 hasConcept C17409809 @default.
• W2052783267 hasConcept C195843664 @default.
• W2052783267 hasConcept C199289684 @default.
• W2052783267 hasConcept C2776152364 @default.
• W2052783267 hasConcept C2777844515 @default.
• W2052783267 hasConcept C2778357522 @default.
• W2052783267 hasConcept C2779870107 @default.
• W2052783267 hasConcept C2780191791 @default.
• W2052783267 hasConcept C2781366471 @default.
• W2052783267 hasConcept C92720285 @default.
• W2052783267 hasConceptScore W2052783267C127313418 @default.
• W2052783267 hasConceptScore W2052783267C151730666 @default.
• W2052783267 hasConceptScore W2052783267C156622251 @default.
• W2052783267 hasConceptScore W2052783267C15785431 @default.
• W2052783267 hasConceptScore W2052783267C165205528 @default.
• W2052783267 hasConceptScore W2052783267C17409809 @default.
• W2052783267 hasConceptScore W2052783267C195843664 @default.
• W2052783267 hasConceptScore W2052783267C199289684 @default.
• W2052783267 hasConceptScore W2052783267C2776152364 @default.
• W2052783267 hasConceptScore W2052783267C2777844515 @default.
• W2052783267 hasConceptScore W2052783267C2778357522 @default.
• W2052783267 hasConceptScore W2052783267C2779870107 @default.
• W2052783267 hasConceptScore W2052783267C2780191791 @default.
• W2052783267 hasConceptScore W2052783267C2781366471 @default.
• W2052783267 hasConceptScore W2052783267C92720285 @default.
• W2052783267 hasIssue "5" @default.
• W2052783267 hasLocation W20527832671 @default.
• W2052783267 hasOpenAccess W2052783267 @default.
• W2052783267 hasPrimaryLocation W20527832671 @default.
• W2052783267 hasRelatedWork W1965704369 @default.
• W2052783267 hasRelatedWork W1991871589 @default.
• W2052783267 hasRelatedWork W2018840380 @default.

• next