Matches in SemOpenAlex for { <https://semopenalex.org/work/W2573382091> ?p ?o ?g. }
- W2573382091 endingPage "497" @default.
- W2573382091 startingPage "486" @default.
- W2573382091 abstract "U–Pb zircon ages obtained from the late- to post-tectonic ‘Newer Granite’ suite in Shetland, northernmost Scottish Caledonides, indicate a significantly more protracted intrusion history than was inferred previously from K–Ar data. Emplacement of the Brae Complex ( c. 465 Ma), Graven Complex ( c. 440 Ma) and the Muckle Roe Granophyre ( c. 438 Ma) followed regional deformation and metamorphism of metasedimentary successions during the Grampian orogenic event, and is attributed to NW-directed subduction beneath Laurentia. The almost complete absence of plutons of this age along-strike in mainland Scotland suggests a change in subduction angle and/or the distance between the subduction zone and the Laurentian margin. Intrusion of the Ronas Hill Granite ( c. 427 Ma) was approximately coeval with displacement on the Moine Thrust in mainland Scotland, and therefore probably occurred during Baltica–Laurentia collision. A gap of c. 35 myr followed before emplacement of the Mangaster Voe Intrusion and Eastern Granophyre ( c. 390 Ma), and a further gap of c. 20 myr before emplacement of the Sandsting Complex ( c. 370 Ma). Both periods of magmatism are attributed to pulses of localized lithospheric melting in the vicinity of the Walls Boundary Fault during Devonian sinistral relative displacements between Laurentia and Baltica. Supplementary material: Petrological details, full analytical methods and data tables are available at https://doi.org/10.6084/m9.figshare.c.3655706" @default.
- W2573382091 created "2017-01-26" @default.
- W2573382091 creator A5011319690 @default.
- W2573382091 creator A5018703843 @default.
- W2573382091 creator A5038411305 @default.
- W2573382091 creator A5039217621 @default.
- W2573382091 creator A5056720815 @default.
- W2573382091 creator A5089331334 @default.
- W2573382091 date "2017-01-18" @default.
- W2573382091 modified "2023-09-30" @default.
- W2573382091 title "U–Pb zircon geochronology and geodynamic significance of ‘Newer Granite’ plutons in Shetland, northernmost Scottish Caledonides" @default.
- W2573382091 cites W1840464923 @default.
- W2573382091 cites W1881869950 @default.
- W2573382091 cites W1944698830 @default.
- W2573382091 cites W1964322474 @default.
- W2573382091 cites W1965623611 @default.
- W2573382091 cites W1974669670 @default.
- W2573382091 cites W1977179325 @default.
- W2573382091 cites W1980002621 @default.
- W2573382091 cites W1982589593 @default.
- W2573382091 cites W1982668279 @default.
- W2573382091 cites W1992616066 @default.
- W2573382091 cites W1996444308 @default.
- W2573382091 cites W2003346600 @default.
- W2573382091 cites W2005731114 @default.
- W2573382091 cites W2007895138 @default.
- W2573382091 cites W2014384293 @default.
- W2573382091 cites W2014821720 @default.
- W2573382091 cites W2015623306 @default.
- W2573382091 cites W2018943563 @default.
- W2573382091 cites W2021307259 @default.
- W2573382091 cites W2022380505 @default.
- W2573382091 cites W2025781670 @default.
- W2573382091 cites W2026361439 @default.
- W2573382091 cites W2028863977 @default.
- W2573382091 cites W2029179895 @default.
- W2573382091 cites W2031707676 @default.
- W2573382091 cites W2033997711 @default.
- W2573382091 cites W2037555983 @default.
- W2573382091 cites W2038873527 @default.
- W2573382091 cites W2039179152 @default.
- W2573382091 cites W2039848826 @default.
- W2573382091 cites W2052095461 @default.
- W2573382091 cites W2052275511 @default.
- W2573382091 cites W2053040522 @default.
- W2573382091 cites W2055233433 @default.
- W2573382091 cites W2056588067 @default.
- W2573382091 cites W2061721984 @default.
- W2573382091 cites W2065817340 @default.
- W2573382091 cites W2066514819 @default.
- W2573382091 cites W2068108401 @default.
- W2573382091 cites W2070217390 @default.
- W2573382091 cites W2070473630 @default.
- W2573382091 cites W2070727611 @default.
- W2573382091 cites W2073712159 @default.
- W2573382091 cites W2079049513 @default.
- W2573382091 cites W2091784688 @default.
- W2573382091 cites W2092533078 @default.
- W2573382091 cites W2092540357 @default.
- W2573382091 cites W2093841681 @default.
- W2573382091 cites W2096820045 @default.
- W2573382091 cites W2098167024 @default.
- W2573382091 cites W2105214965 @default.
- W2573382091 cites W2109421543 @default.
- W2573382091 cites W2114714926 @default.
- W2573382091 cites W2116943890 @default.
- W2573382091 cites W2117964460 @default.
- W2573382091 cites W2119808203 @default.
- W2573382091 cites W2122790267 @default.
- W2573382091 cites W2124563601 @default.
- W2573382091 cites W2127080702 @default.
- W2573382091 cites W2131489724 @default.
- W2573382091 cites W2133272619 @default.
- W2573382091 cites W2135414479 @default.
- W2573382091 cites W2138242101 @default.
- W2573382091 cites W2147992226 @default.
- W2573382091 cites W2157609597 @default.
- W2573382091 cites W2169394717 @default.
- W2573382091 cites W2274023072 @default.
- W2573382091 cites W2300896766 @default.
- W2573382091 cites W2303005318 @default.
- W2573382091 cites W2328097201 @default.
- W2573382091 cites W2331762685 @default.
- W2573382091 cites W946337192 @default.
- W2573382091 doi "https://doi.org/10.1144/jgs2016-106" @default.
- W2573382091 hasPublicationYear "2017" @default.
- W2573382091 type Work @default.
- W2573382091 sameAs 2573382091 @default.
- W2573382091 citedByCount "18" @default.
- W2573382091 countsByYear W25733820912017 @default.
- W2573382091 countsByYear W25733820912018 @default.
- W2573382091 countsByYear W25733820912019 @default.
- W2573382091 countsByYear W25733820912020 @default.
- W2573382091 countsByYear W25733820912021 @default.
- W2573382091 countsByYear W25733820912022 @default.
- W2573382091 countsByYear W25733820912023 @default.
- W2573382091 crossrefType "journal-article" @default.
- W2573382091 hasAuthorship W2573382091A5011319690 @default.