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- W2106544460 abstract "The composite intrusions of Drumadoon and An Cumhann crop out on the SE coast of the Isle of Arran, Scotland and form part of the larger British and Irish Palaeogene Igneous Province, a subset of the North Atlantic Igneous Province. The intrusions (shallow-level dykes and sills) comprise a central quartz–feldspar-phyric rhyolite flanked by xenocryst-bearing basaltic andesite, with an intermediate zone of dark quartz–feldspar-phyric dacite. New geochemical data provide information on the evolution of the component magmas and their relationships with each other, as well as their interaction with the crust through which they travelled. During shallow-crustal emplacement, the end-member magmas mixed. Isotopic evidence shows that both magmas were contaminated by the crust prior to mixing; the basaltic andesite magma preserves some evidence of contamination within the lower crust, whereas the rhyolite mainly records upper-crustal contamination. The Highland Boundary Fault divides Arran into two distinct terranes, the Neoproterozoic to Early Palaeozoic Grampian Terrane to the north and the Palaeozoic Midland Valley Terrane to the south. The Drumadoon Complex lies within the Midland Valley Terrane but its isotopic signatures indicate almost exclusive involvement of Grampian Terrane crust. Therefore, although the magmas originated at depth on the northern side of the Highland Boundary Fault, they have crossed this boundary during their evolution, probably just prior to emplacement." @default.
- W2106544460 created "2016-06-24" @default.
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- W2106544460 creator A5069476691 @default.
- W2106544460 date "2009-12-01" @default.
- W2106544460 modified "2023-09-23" @default.
- W2106544460 title "Magma Ascent along a Major Terrane Boundary: Crustal Contamination and Magma Mixing at the Drumadoon Intrusive Complex, Isle of Arran, Scotland" @default.
- W2106544460 cites W1965161592 @default.
- W2106544460 cites W1966917681 @default.
- W2106544460 cites W1968262450 @default.
- W2106544460 cites W1970845599 @default.
- W2106544460 cites W1973135214 @default.
- W2106544460 cites W1975280948 @default.
- W2106544460 cites W1977257921 @default.
- W2106544460 cites W1977617650 @default.
- W2106544460 cites W1978507857 @default.
- W2106544460 cites W1979537202 @default.
- W2106544460 cites W1980720218 @default.
- W2106544460 cites W1981916272 @default.
- W2106544460 cites W1982005903 @default.
- W2106544460 cites W1982781736 @default.
- W2106544460 cites W1986408395 @default.
- W2106544460 cites W1991237376 @default.
- W2106544460 cites W1992752407 @default.
- W2106544460 cites W1995838608 @default.
- W2106544460 cites W2006794166 @default.
- W2106544460 cites W2006982501 @default.
- W2106544460 cites W2007022756 @default.
- W2106544460 cites W2007297818 @default.
- W2106544460 cites W2010113056 @default.
- W2106544460 cites W2011097477 @default.
- W2106544460 cites W2011598871 @default.
- W2106544460 cites W2013907048 @default.
- W2106544460 cites W2018376581 @default.
- W2106544460 cites W2022648729 @default.
- W2106544460 cites W2023379572 @default.
- W2106544460 cites W2024419087 @default.
- W2106544460 cites W2024575502 @default.
- W2106544460 cites W2026058933 @default.
- W2106544460 cites W2033572692 @default.
- W2106544460 cites W2034161077 @default.
- W2106544460 cites W2037363360 @default.
- W2106544460 cites W2044854677 @default.
- W2106544460 cites W2046446046 @default.
- W2106544460 cites W2046902789 @default.
- W2106544460 cites W2046934910 @default.
- W2106544460 cites W2048116571 @default.
- W2106544460 cites W2048591366 @default.
- W2106544460 cites W2050930816 @default.
- W2106544460 cites W2052639254 @default.
- W2106544460 cites W2054583282 @default.
- W2106544460 cites W2056278046 @default.
- W2106544460 cites W2057810318 @default.
- W2106544460 cites W2067221143 @default.
- W2106544460 cites W2073451667 @default.
- W2106544460 cites W2073879478 @default.
- W2106544460 cites W2077959302 @default.
- W2106544460 cites W2092605103 @default.
- W2106544460 cites W2093567690 @default.
- W2106544460 cites W2096868193 @default.
- W2106544460 cites W2097100034 @default.
- W2106544460 cites W2100540137 @default.
- W2106544460 cites W2101342695 @default.
- W2106544460 cites W2103678554 @default.
- W2106544460 cites W2107738833 @default.
- W2106544460 cites W2108170961 @default.
- W2106544460 cites W2108392897 @default.
- W2106544460 cites W2109996096 @default.
- W2106544460 cites W2118315366 @default.
- W2106544460 cites W2123205123 @default.
- W2106544460 cites W2124983288 @default.
- W2106544460 cites W2127713280 @default.
- W2106544460 cites W2151802570 @default.
- W2106544460 cites W2154783705 @default.
- W2106544460 cites W2156615197 @default.
- W2106544460 cites W2156647072 @default.
- W2106544460 cites W2158445900 @default.
- W2106544460 cites W2159164485 @default.
- W2106544460 cites W2161009583 @default.
- W2106544460 cites W2164796906 @default.
- W2106544460 cites W2167669185 @default.
- W2106544460 cites W2170309512 @default.
- W2106544460 cites W2288262836 @default.
- W2106544460 cites W2331660372 @default.
- W2106544460 cites W2335115351 @default.
- W2106544460 doi "https://doi.org/10.1093/petrology/egp081" @default.
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