FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W944680052> ?p ?o ?g. }

• W944680052 endingPage "918" @default.
• W944680052 startingPage "903" @default.
• W944680052 abstract "Abstract Fluid inclusions in quartz, sulfides from quartz veins, and quartz, garnet, plagioclase, and orthoclase from granulites of the Bogunai gold deposit located in the granulites of the Angara–Kan block of the Yenisei Ridge were studied by thermobarometry, gas chromatography, chromato-mass-spectrometry, Raman spectroscopy, and mass spectrometry with inductively coupled plasma. The formation temperatures (850–950 °C) and pressures (8.5–9.0 kbar) of minerals of the granulite metamorphic facies are much higher than the crystallization temperatures (220–420 °C) and pressures (0.1–1.6 kbar) of gold–quartz veins of the Bogunai deposit. These veins formed with the participation of H2O–CO2–hydrocarbon fluids with a salt (predominantly MgCl2) concentration of 2–19 wt.% NaCl equiv. The gas phase of fluid inclusions from quartz, pyrite, chalcopyrite, galena, and sphalerite contains not only H2O, CO2, CH4, and N2 but also the first found compounds of sulfur (CS2, O2S, COS, C2H6S2) and nitrogen (C3H7N, C3H7NO, C4H8N2O) and numerous hydrocarbons of different classes (paraffins, arenes, naphthenes, alcohols, aldehydes, ketones, carbonic acids, and furans). The age of the Krasnoyarsk mineralized zone, one of the sites of the Bogunai deposit, is 466 ± 3.2–461.6 ± 3.1 Ma, which is almost 1400 Ma younger than the age of granulite metamorphism and 255 Ma younger than the age of diaphthoresis but is close to the age of the Lower Kan granitoid pluton (455.7 ± 3.4 Ma). The sulfur isotope ratios (δ34S) of sulfides (pyrite, chalcopyrite, sphalerite, and galena) are close to the mantle values, 0.8 to 3.5%c, and are in the range of the granitoid values, which indicates the crustal source of the fluid sulfur. Gold of the Bogunai deposit accumulated with the participation of H2O–CO2–hydrocarbon fluids generated both in deep-fault zones and in granitoid intrusions." @default.
• W944680052 created "2016-06-24" @default.
• W944680052 creator A5002579033 @default.
• W944680052 creator A5008436587 @default.
• W944680052 creator A5013250062 @default.
• W944680052 creator A5015276308 @default.
• W944680052 creator A5016009776 @default.
• W944680052 creator A5023290599 @default.
• W944680052 date "2015-06-01" @default.
• W944680052 modified "2023-09-24" @default.
• W944680052 title "P–T–X parameters of metamorphogene and hydrothermal fluids, isotopy and age of the Bogunai gold deposit, southern Yenisei Ridge (Russia)" @default.
• W944680052 cites W1964259713 @default.
• W944680052 cites W1964349654 @default.
• W944680052 cites W1966320954 @default.
• W944680052 cites W1970449974 @default.
• W944680052 cites W1972342782 @default.
• W944680052 cites W1973969335 @default.
• W944680052 cites W1974064297 @default.
• W944680052 cites W1976650786 @default.
• W944680052 cites W1981252101 @default.
• W944680052 cites W1981507034 @default.
• W944680052 cites W1985827600 @default.
• W944680052 cites W1994146455 @default.
• W944680052 cites W2003035853 @default.
• W944680052 cites W2017202826 @default.
• W944680052 cites W2022304725 @default.
• W944680052 cites W2022448496 @default.
• W944680052 cites W2024391936 @default.
• W944680052 cites W2031949647 @default.
• W944680052 cites W2044496537 @default.
• W944680052 cites W2056820586 @default.
• W944680052 cites W2058625346 @default.
• W944680052 cites W2059105368 @default.
• W944680052 cites W2064706665 @default.
• W944680052 cites W2073127548 @default.
• W944680052 cites W2076521030 @default.
• W944680052 cites W2091183834 @default.
• W944680052 cites W2114014773 @default.
• W944680052 cites W2120247061 @default.
• W944680052 cites W2120270131 @default.
• W944680052 cites W2121976325 @default.
• W944680052 cites W2146459089 @default.
• W944680052 cites W2148808419 @default.
• W944680052 cites W2158847234 @default.
• W944680052 cites W2162646945 @default.
• W944680052 cites W2163241987 @default.
• W944680052 cites W2591859236 @default.
• W944680052 cites W4243715129 @default.
• W944680052 doi "https://doi.org/10.1016/j.rgg.2015.05.007" @default.
• W944680052 hasPublicationYear "2015" @default.
• W944680052 type Work @default.
• W944680052 sameAs 944680052 @default.
• W944680052 citedByCount "10" @default.
• W944680052 countsByYear W9446800522016 @default.
• W944680052 countsByYear W9446800522017 @default.
• W944680052 countsByYear W9446800522018 @default.
• W944680052 countsByYear W9446800522019 @default.
• W944680052 countsByYear W9446800522020 @default.
• W944680052 countsByYear W9446800522021 @default.
• W944680052 countsByYear W9446800522022 @default.
• W944680052 countsByYear W9446800522023 @default.
• W944680052 crossrefType "journal-article" @default.
• W944680052 hasAuthorship W944680052A5002579033 @default.
• W944680052 hasAuthorship W944680052A5008436587 @default.
• W944680052 hasAuthorship W944680052A5013250062 @default.
• W944680052 hasAuthorship W944680052A5015276308 @default.
• W944680052 hasAuthorship W944680052A5016009776 @default.
• W944680052 hasAuthorship W944680052A5023290599 @default.
• W944680052 hasConcept C109007969 @default.
• W944680052 hasConcept C112764850 @default.
• W944680052 hasConcept C127313418 @default.
• W944680052 hasConcept C146588470 @default.
• W944680052 hasConcept C151730666 @default.
• W944680052 hasConcept C17409809 @default.
• W944680052 hasConcept C178790620 @default.
• W944680052 hasConcept C18142444 @default.
• W944680052 hasConcept C185592680 @default.
• W944680052 hasConcept C199289684 @default.
• W944680052 hasConcept C26687426 @default.
• W944680052 hasConcept C2776062231 @default.
• W944680052 hasConcept C2776152364 @default.
• W944680052 hasConcept C2776268066 @default.
• W944680052 hasConcept C2778188036 @default.
• W944680052 hasConcept C2779870107 @default.
• W944680052 hasConcept C2780416900 @default.
• W944680052 hasConcept C544778455 @default.
• W944680052 hasConceptScore W944680052C109007969 @default.
• W944680052 hasConceptScore W944680052C112764850 @default.
• W944680052 hasConceptScore W944680052C127313418 @default.
• W944680052 hasConceptScore W944680052C146588470 @default.
• W944680052 hasConceptScore W944680052C151730666 @default.
• W944680052 hasConceptScore W944680052C17409809 @default.
• W944680052 hasConceptScore W944680052C178790620 @default.
• W944680052 hasConceptScore W944680052C18142444 @default.
• W944680052 hasConceptScore W944680052C185592680 @default.
• W944680052 hasConceptScore W944680052C199289684 @default.
• W944680052 hasConceptScore W944680052C26687426 @default.
• W944680052 hasConceptScore W944680052C2776062231 @default.

• next