Thermal evolution of the Scandian hinterland, Naver nappe, northern Scotland
Abstract
The Northern Highlands Terrane of Scotland hosts several thrust nappes that were deformed and metamorphosed during the Silurian Scandian orogeny. Quantitative petrological analysis of metamorphic assemblages indicates that the hinterland-positioned Naver nappe experienced decompression heating from 8–9 kbar and 600°C to 6–7 kbar and 700°C. Monazite–xenotime thermometry and geochronology delineate a detailed temperature–time history for the Naver...
Paper Details
Title
Thermal evolution of the Scandian hinterland, Naver nappe, northern Scotland
Published Date
May 28, 2019
Volume
176
Issue
4
Pages
669 - 688
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