FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2026923685> ?p ?o ?g. }

• W2026923685 endingPage "90" @default.
• W2026923685 startingPage "73" @default.
• W2026923685 abstract "article An extensive data set on the compositional variation of tourmaline from granitic pegmatites, from migmatitic gneisses and from various types of hydrothermal veins from the Schwarzwald, Germany, is provided. The investigated tourmalines are members of the alkali and X-vacant groups representing mostly dravite- schorl solid solutions with some analyses belonging to the foitite-Mg-foitite series. Oxygen isotope data on quartz-tourmaline pairs indicate formation temperatures between 550 and 350 °C for most of the quartz-tourmaline veins. Most of the tourmalines show strong sector zonation, fractionating certain major (e.g., Na, Mg), minor (e.g., Ti, Ca) and trace elements (e.g., Sr, Pb, REE) among the different crystallographic sectors of the crystals. We conclude that comparison of tourmaline compositions for petrogenetic interpretations must be based on the concentrations in the neutral a sector in order to eliminate the effects of intra-crystalline fractionation. Most trace element contents vary over several orders of magnitude with median concentrations generally be- tween 0.1 and 10 μg/g. The highest concentrations are found for Zn, V, Sr, Sc, Sn and Li (median concentrations of several tens to hundreds of μg/g) whereas very low median concentrations (b0.1 μg/g) were found for U, Th, Bi, Tl and Cs. The concentration of several trace elements (e.g., Sr, REE, Co) correlates with the major element composition of the tourmaline, which implies potential crystal chemical effects on their incorporation. Conse- quently, the general assumption that tourmaline is a passive monitor for the chemical compositions of the melts or fluids from which it crystallizes has to be questioned. Nevertheless, our study demonstrates that the trace element composition of tourmaline allows to distinguish between geochemically distinct fluid sources, and the trace element composition of tourmaline may therefore be used to unravel the chemical complexity of granite-related hydrothermal systems." @default.
• W2026923685 created "2016-06-24" @default.
• W2026923685 creator A5014031413 @default.
• W2026923685 creator A5015336500 @default.
• W2026923685 creator A5031751266 @default.
• W2026923685 creator A5052895107 @default.
• W2026923685 creator A5057276671 @default.
• W2026923685 creator A5063361556 @default.
• W2026923685 creator A5069015609 @default.
• W2026923685 creator A5078970573 @default.
• W2026923685 date "2013-04-01" @default.
• W2026923685 modified "2023-10-01" @default.
• W2026923685 title "Trace element systematics of tourmaline in pegmatitic and hydrothermal systems from the Variscan Schwarzwald (Germany): The importance of major element composition, sector zoning, and fluid or melt composition" @default.
• W2026923685 cites W1657551646 @default.
• W2026923685 cites W1963978511 @default.
• W2026923685 cites W1966189692 @default.
• W2026923685 cites W1966638191 @default.
• W2026923685 cites W1979365798 @default.
• W2026923685 cites W1980333019 @default.
• W2026923685 cites W1982560803 @default.
• W2026923685 cites W1983497683 @default.
• W2026923685 cites W1985626288 @default.
• W2026923685 cites W1990028416 @default.
• W2026923685 cites W1990581568 @default.
• W2026923685 cites W1993307882 @default.
• W2026923685 cites W1994542106 @default.
• W2026923685 cites W1995813894 @default.
• W2026923685 cites W1999810686 @default.
• W2026923685 cites W2003655297 @default.
• W2026923685 cites W2008575948 @default.
• W2026923685 cites W2011556934 @default.
• W2026923685 cites W2013611498 @default.
• W2026923685 cites W2015002933 @default.
• W2026923685 cites W2016097466 @default.
• W2026923685 cites W2018872939 @default.
• W2026923685 cites W2019537189 @default.
• W2026923685 cites W2021635268 @default.
• W2026923685 cites W2022460640 @default.
• W2026923685 cites W2025267246 @default.
• W2026923685 cites W2025645292 @default.
• W2026923685 cites W2030153642 @default.
• W2026923685 cites W2036056983 @default.
• W2026923685 cites W2039728532 @default.
• W2026923685 cites W2040196332 @default.
• W2026923685 cites W2045486459 @default.
• W2026923685 cites W2045986371 @default.
• W2026923685 cites W2046009013 @default.
• W2026923685 cites W2052352503 @default.
• W2026923685 cites W2054706405 @default.
• W2026923685 cites W2056994161 @default.
• W2026923685 cites W2068055529 @default.
• W2026923685 cites W2074461112 @default.
• W2026923685 cites W2082583308 @default.
• W2026923685 cites W2092829775 @default.
• W2026923685 cites W2093740880 @default.
• W2026923685 cites W2095429679 @default.
• W2026923685 cites W2102285738 @default.
• W2026923685 cites W2102468129 @default.
• W2026923685 cites W2102811433 @default.
• W2026923685 cites W2119823796 @default.
• W2026923685 cites W2123014101 @default.
• W2026923685 cites W2124782245 @default.
• W2026923685 cites W2125124496 @default.
• W2026923685 cites W2137141094 @default.
• W2026923685 cites W2137242057 @default.
• W2026923685 cites W2143525524 @default.
• W2026923685 cites W2153309939 @default.
• W2026923685 cites W2164033639 @default.
• W2026923685 cites W2169988458 @default.
• W2026923685 cites W2312624277 @default.
• W2026923685 cites W2323214655 @default.
• W2026923685 cites W2325090410 @default.
• W2026923685 cites W2326962883 @default.
• W2026923685 cites W2328605559 @default.
• W2026923685 cites W2336552296 @default.
• W2026923685 cites W2503091589 @default.
• W2026923685 cites W2581834115 @default.
• W2026923685 cites W3158883608 @default.
• W2026923685 doi "https://doi.org/10.1016/j.chemgeo.2013.02.025" @default.
• W2026923685 hasPublicationYear "2013" @default.
• W2026923685 type Work @default.
• W2026923685 sameAs 2026923685 @default.
• W2026923685 citedByCount "75" @default.
• W2026923685 countsByYear W20269236852014 @default.
• W2026923685 countsByYear W20269236852015 @default.
• W2026923685 countsByYear W20269236852016 @default.
• W2026923685 countsByYear W20269236852017 @default.
• W2026923685 countsByYear W20269236852018 @default.
• W2026923685 countsByYear W20269236852019 @default.
• W2026923685 countsByYear W20269236852020 @default.
• W2026923685 countsByYear W20269236852021 @default.
• W2026923685 countsByYear W20269236852022 @default.
• W2026923685 countsByYear W20269236852023 @default.
• W2026923685 crossrefType "journal-article" @default.
• W2026923685 hasAuthorship W2026923685A5014031413 @default.
• W2026923685 hasAuthorship W2026923685A5015336500 @default.
• W2026923685 hasAuthorship W2026923685A5031751266 @default.
• W2026923685 hasAuthorship W2026923685A5052895107 @default.

• next