 | Kawai, T., Windley, B.F., Shibuya, T., Omori, S., Sawaki, Y., Maruyama, S. (2008) Large P–T gap between Ballantrae blueschist/garnet pyroxenite and surrounding ophiolite, southern Scotland, UK: Diapiric exhumation of a Caledonian serpentinite mélange. Lithos, 104 (1) 337-354 doi:10.1016/j.lithos.2008.01.005 | Journal (article/letter/editorial) | | pyroxenite and surrounding ophiolite, southern Scotland, UK: Diapiric exhumation of a Caledonian serpentinite... The University of Leicester, Leicester LE1 7RH, UK Received 25 July 2007; accepted 29 January 2008 Available...Abstract The Ballantrae ophiolite in southern Scotland includes a NEE–SWW-trending serpentinite mélange...501 ± 12 Ma volcanic arc belt extends for 3 km south of the serpentinite mélange. We suggest that ridge...created arc-related gabbro (483 ± 4 Ma) at Byne Hill and within-plate gabbro (487 ± 8 Ma) at Millenderdale |  | | Report (issue) | | above O.D. Byne Hill 15 214 0-10 0 10-50 50-100 2 kiJometres 0 " 100-150 Gg"f Hill 150-200 / ...& Pinbain Hill ·224 200-250 >250 .' "1,,llte ( 0 90 1och Hill 187 A Knockormal Hill 215 85 ...Ballantrae area and its location in south west Scotland 11 Stranraer 0 Mull of Galloway 10 km Classical...phenocrysts in basalt of the Mains Hill Agglomerate Formation 62 of the Byne Hill gabbro trondhjemite and Arenig...variation within coarse gabbro pegm.atite 13 6 Craig Hill Breccia Formation 59 2 4 Banded gabbro in the northern |
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