FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2769465744> ?p ?o ?g. }

• W2769465744 endingPage "211" @default.
• W2769465744 startingPage "200" @default.
• W2769465744 abstract "The 40Ar/39Ar ages of metamorphic micas that crystallized at high temperatures are commonly interpreted as cooling ages, with grains considered to have lost 40Ar via thermally-driven diffusion into the grain boundary network. Recently reported laser-ablation data suggest that the spatial distribution of Ar in metamorphic micas does not always conform to the patterns predicted by diffusion theory and that despite high metamorphic temperatures, argon was not removed efficiently from the local system during metamorphic evolution. In the Western Gneiss Region (WGR), Norway, felsic gneisses preserve microtextural evidence for the breakdown of phengite to biotite and plagioclase symplectites during near isothermal decompression from c. 20–25 to c. 8–12 kbar at ~ 700 °C. These samples provide an ideal natural laboratory to assess whether the complete replacement of one K-bearing mineral by another at high temperatures completely ‘resets’ the Ar clock, or whether there is some inheritance of 40Ar in the neocrystallized phase. The timing of the high-temperature portion of the WGR metamorphic cycle has been well constrained in previous studies. However, the timing of cooling following the overprint is still much debated. In-situ laser ablation spot dating in phengite, biotite-plagioclase symplectites and coarser, texturally later biotite yielded 40Ar/39Ar ages that span much of the metamorphic cycle. Together these data show that despite residence at temperatures of ~ 700 °C, Ar is not completely removed by diffusive loss or during metamorphic recrystallization. Instead, Ar released during phengite breakdown appears to be partially reincorporated into the newly crystallizing biotite and plagioclase (or is trapped in fluid inclusions in those phases) within a close system. Our data show that the microtextural and petrographic evolution of the sample being dated provides a critical framework in which local 40Ar recycling can be tracked, thus potentially allowing 40Ar/39Ar dates to be linked more accurately to metamorphic history." @default.
• W2769465744 created "2017-12-04" @default.
• W2769465744 creator A5009356764 @default.
• W2769465744 creator A5031073379 @default.
• W2769465744 creator A5070173469 @default.
• W2769465744 creator A5073233344 @default.
• W2769465744 creator A5075775010 @default.
• W2769465744 date "2018-02-01" @default.
• W2769465744 modified "2023-09-26" @default.
• W2769465744 title "Recycling argon through metamorphic reactions: The record in symplectites" @default.
• W2769465744 cites W1503086493 @default.
• W2769465744 cites W1601824667 @default.
• W2769465744 cites W1605368522 @default.
• W2769465744 cites W1767843502 @default.
• W2769465744 cites W1776478061 @default.
• W2769465744 cites W1830358639 @default.
• W2769465744 cites W1964212620 @default.
• W2769465744 cites W1965340427 @default.
• W2769465744 cites W1972684097 @default.
• W2769465744 cites W1975557703 @default.
• W2769465744 cites W1977271515 @default.
• W2769465744 cites W1979476030 @default.
• W2769465744 cites W1981344517 @default.
• W2769465744 cites W1991332592 @default.
• W2769465744 cites W1991861266 @default.
• W2769465744 cites W1992145404 @default.
• W2769465744 cites W1992616066 @default.
• W2769465744 cites W1994855356 @default.
• W2769465744 cites W1998977948 @default.
• W2769465744 cites W2003365780 @default.
• W2769465744 cites W2004633554 @default.
• W2769465744 cites W2007800343 @default.
• W2769465744 cites W2012067626 @default.
• W2769465744 cites W2016431160 @default.
• W2769465744 cites W2019877001 @default.
• W2769465744 cites W2019899106 @default.
• W2769465744 cites W2020129047 @default.
• W2769465744 cites W2021778941 @default.
• W2769465744 cites W2024390287 @default.
• W2769465744 cites W2036488570 @default.
• W2769465744 cites W2038641155 @default.
• W2769465744 cites W2040549377 @default.
• W2769465744 cites W2044065690 @default.
• W2769465744 cites W2045434219 @default.
• W2769465744 cites W2050712935 @default.
• W2769465744 cites W2053381713 @default.
• W2769465744 cites W2057162185 @default.
• W2769465744 cites W2057650749 @default.
• W2769465744 cites W2063765008 @default.
• W2769465744 cites W2066688058 @default.
• W2769465744 cites W2071369893 @default.
• W2769465744 cites W2071506355 @default.
• W2769465744 cites W2081479644 @default.
• W2769465744 cites W2081823524 @default.
• W2769465744 cites W2082844473 @default.
• W2769465744 cites W2093041656 @default.
• W2769465744 cites W2093179570 @default.
• W2769465744 cites W2100411277 @default.
• W2769465744 cites W2105662998 @default.
• W2769465744 cites W2107012155 @default.
• W2769465744 cites W2112139658 @default.
• W2769465744 cites W2115177642 @default.
• W2769465744 cites W2117018064 @default.
• W2769465744 cites W2125270986 @default.
• W2769465744 cites W2131817581 @default.
• W2769465744 cites W2141412884 @default.
• W2769465744 cites W2153123329 @default.
• W2769465744 cites W2156576514 @default.
• W2769465744 cites W2297758669 @default.
• W2769465744 cites W2300928107 @default.
• W2769465744 cites W2415806974 @default.
• W2769465744 cites W2502729337 @default.
• W2769465744 cites W2522156330 @default.
• W2769465744 cites W4233848018 @default.
• W2769465744 cites W4238765793 @default.
• W2769465744 cites W4378211144 @default.
• W2769465744 doi "https://doi.org/10.1016/j.lithos.2017.11.028" @default.
• W2769465744 hasPublicationYear "2018" @default.
• W2769465744 type Work @default.
• W2769465744 sameAs 2769465744 @default.
• W2769465744 citedByCount "14" @default.
• W2769465744 countsByYear W27694657442019 @default.
• W2769465744 countsByYear W27694657442020 @default.
• W2769465744 countsByYear W27694657442021 @default.
• W2769465744 countsByYear W27694657442022 @default.
• W2769465744 countsByYear W27694657442023 @default.
• W2769465744 crossrefType "journal-article" @default.
• W2769465744 hasAuthorship W2769465744A5009356764 @default.
• W2769465744 hasAuthorship W2769465744A5031073379 @default.
• W2769465744 hasAuthorship W2769465744A5070173469 @default.
• W2769465744 hasAuthorship W2769465744A5073233344 @default.
• W2769465744 hasAuthorship W2769465744A5075775010 @default.
• W2769465744 hasBestOaLocation W27694657441 @default.
• W2769465744 hasConcept C127313418 @default.
• W2769465744 hasConcept C151730666 @default.
• W2769465744 hasConcept C171701179 @default.
• W2769465744 hasConcept C173347748 @default.
• W2769465744 hasConcept C17409809 @default.

• next