FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2045835024> ?p ?o ?g. }

• W2045835024 endingPage "131" @default.
• W2045835024 startingPage "120" @default.
• W2045835024 abstract "Chlorine stable isotope compositions of two sedimentary sequences and their metamorphic equivalents were measured in order to study fractionation effects during prograde metamorphism and devolatilization. Protoliths (n=25) were collected from a 50 m section of Triassic fluvial and playa-lake strata and Jurassic (Liassic) marine black shales in a well-characterized quarry. Low greenschist to middle amphibolite facies equivalents (n>80) were collected from the Glarus Alps, Urseren Zone, and Lucomagno region. Bulk δ37Cl values are constant within individual sedimentary layers, but vary from −2.0 to +2.4‰ in Triassic rocks and from −3.0 to 0‰ in the black shales. Dolomitic and gypsiferous samples have positive δ37Cl values, but marls and shales are isotopically negative. Bulk Cl contents show only small declines during the earliest stages of metamorphism. Metamorphic equivalents of the Triassic and Liassic protoliths record the same overall ranges in δ37Cl as their protoliths. Samples with highly correlated bulk compositions but different metamorphic grade show no statistically significant difference in δ37Cl. These data lead to the following conclusions: (1) Terrestrial and marine sedimentary rocks display large primary heterogeneities in chlorine isotope composition. As a result, an unambiguous “sedimentary signature” does not exist in the chlorine stable isotope system. (2) No isotopic fractionation is discernable during metamorphic devolatilization, even at low temperatures. Alpine-style metamorphism thus has little to no effect on bulk chlorine isotopic compositions, despite significant devolatilization. (3) Cl is largely retained in the rocks during devolatilization, contrary to the normally assumed hydrophilic behavior of chlorine. Continuous release of mixed-volatile C–O–H fluids likely affected Cl partitioning between fluid and minerals and allowed chlorine to remain in the rocks. (4) There is no evidence for fluid communication across (meta)sedimentary layers except within the Urseren shear zone. These data contribute to a relatively closed-system view of metamorphic devolatilization from anchizone through mid-amphibolite facies conditions." @default.
• W2045835024 created "2016-06-24" @default.
• W2045835024 creator A5036070265 @default.
• W2045835024 creator A5050386353 @default.
• W2045835024 date "2015-05-01" @default.
• W2045835024 modified "2023-09-26" @default.
• W2045835024 title "Chlorine isotope behavior during prograde metamorphism of sedimentary rocks" @default.
• W2045835024 cites W131291834 @default.
• W2045835024 cites W1549196579 @default.
• W2045835024 cites W1922562631 @default.
• W2045835024 cites W1933683414 @default.
• W2045835024 cites W1968448747 @default.
• W2045835024 cites W1970826704 @default.
• W2045835024 cites W1977472551 @default.
• W2045835024 cites W1978884469 @default.
• W2045835024 cites W1979238741 @default.
• W2045835024 cites W1981489021 @default.
• W2045835024 cites W1983281222 @default.
• W2045835024 cites W1985917712 @default.
• W2045835024 cites W1987086207 @default.
• W2045835024 cites W1988761694 @default.
• W2045835024 cites W1999992665 @default.
• W2045835024 cites W2007635292 @default.
• W2045835024 cites W2010139381 @default.
• W2045835024 cites W2019651860 @default.
• W2045835024 cites W2021179993 @default.
• W2045835024 cites W2021898492 @default.
• W2045835024 cites W2022310331 @default.
• W2045835024 cites W2035890251 @default.
• W2045835024 cites W2038174752 @default.
• W2045835024 cites W2039915597 @default.
• W2045835024 cites W2041510827 @default.
• W2045835024 cites W2044278455 @default.
• W2045835024 cites W2049558762 @default.
• W2045835024 cites W2053262105 @default.
• W2045835024 cites W2054327178 @default.
• W2045835024 cites W2056860684 @default.
• W2045835024 cites W2062831705 @default.
• W2045835024 cites W2065466674 @default.
• W2045835024 cites W2066423371 @default.
• W2045835024 cites W2069479235 @default.
• W2045835024 cites W2075132449 @default.
• W2045835024 cites W2075618665 @default.
• W2045835024 cites W2078468681 @default.
• W2045835024 cites W2080545551 @default.
• W2045835024 cites W2082691438 @default.
• W2045835024 cites W2090874544 @default.
• W2045835024 cites W2091735272 @default.
• W2045835024 cites W2094928570 @default.
• W2045835024 cites W2106480267 @default.
• W2045835024 cites W2109354102 @default.
• W2045835024 cites W2128146362 @default.
• W2045835024 cites W2133107219 @default.
• W2045835024 cites W2161217786 @default.
• W2045835024 cites W2321943981 @default.
• W2045835024 cites W2750496111 @default.
• W2045835024 doi "https://doi.org/10.1016/j.epsl.2015.02.030" @default.
• W2045835024 hasPublicationYear "2015" @default.
• W2045835024 type Work @default.
• W2045835024 sameAs 2045835024 @default.
• W2045835024 citedByCount "30" @default.
• W2045835024 countsByYear W20458350242015 @default.
• W2045835024 countsByYear W20458350242016 @default.
• W2045835024 countsByYear W20458350242017 @default.
• W2045835024 countsByYear W20458350242018 @default.
• W2045835024 countsByYear W20458350242019 @default.
• W2045835024 countsByYear W20458350242020 @default.
• W2045835024 countsByYear W20458350242021 @default.
• W2045835024 countsByYear W20458350242022 @default.
• W2045835024 countsByYear W20458350242023 @default.
• W2045835024 crossrefType "journal-article" @default.
• W2045835024 hasAuthorship W2045835024A5036070265 @default.
• W2045835024 hasAuthorship W2045835024A5050386353 @default.
• W2045835024 hasConcept C109007969 @default.
• W2045835024 hasConcept C112764850 @default.
• W2045835024 hasConcept C127313418 @default.
• W2045835024 hasConcept C146588470 @default.
• W2045835024 hasConcept C151730666 @default.
• W2045835024 hasConcept C17409809 @default.
• W2045835024 hasConcept C26687426 @default.
• W2045835024 hasConcept C37045145 @default.
• W2045835024 hasConcept C6494504 @default.
• W2045835024 hasConcept C79927612 @default.
• W2045835024 hasConcept C95628711 @default.
• W2045835024 hasConceptScore W2045835024C109007969 @default.
• W2045835024 hasConceptScore W2045835024C112764850 @default.
• W2045835024 hasConceptScore W2045835024C127313418 @default.
• W2045835024 hasConceptScore W2045835024C146588470 @default.
• W2045835024 hasConceptScore W2045835024C151730666 @default.
• W2045835024 hasConceptScore W2045835024C17409809 @default.
• W2045835024 hasConceptScore W2045835024C26687426 @default.
• W2045835024 hasConceptScore W2045835024C37045145 @default.
• W2045835024 hasConceptScore W2045835024C6494504 @default.
• W2045835024 hasConceptScore W2045835024C79927612 @default.
• W2045835024 hasConceptScore W2045835024C95628711 @default.
• W2045835024 hasFunder F4320306076 @default.
• W2045835024 hasLocation W20458350241 @default.
• W2045835024 hasOpenAccess W2045835024 @default.

• next