WebNov 3, 2011 · The Dalradian rocks of the Lecht, NE Scotland: stratigraphy, faulting, geochemistry and mineralisation - Volume 80 Issue 2. Skip to main content Accessibility help We use cookies to distinguish you from other users and to provide you with a better experience on our websites. WebNov 3, 2011 · The Dalradian rocks of the Lecht, NE Scotland: stratigraphy, faulting, geochemistry and mineralisation - Volume 80 Issue 2. Skip to main content Accessibility …
Grampian & Argyll – Scotland – the home of geology
WebJan 1, 2013 · The Dalradian rocks of Scotland: an introduction. The Dalradian Supergroup and its basement rocks, together with younger plutons, underpin most of the Grampian Highlands and the islands of the Inner Hebrides between the Highland Boundary and Great Glen faults. The Dalradian is a mid-Neoproterozoic to early-Ordovician … WebSandwiched between the Dalradian and Midland Valley rocks lies a third, exotic group of rocks known as the “Highland Border Complex”. It forms narrow slivers along the Highland Boundary Fault. Some of these rocks resemble those found under the ocean floor: they include serpentine and marble of Ordovician in age, perhaps as old as 470 ... sighthill edinburgh postcode
Sedimentary affiliations and stratigraphic correlation of the Dalradian …
WebSep 15, 2015 · 7. Conclusions. The results of this study indicate that significant mobility of Au, As, and Sb occurred during metamorphism of the Dalradian metasedimentary rocks of Scotland. Sillimanite zone samples have an average mass loss of 62 ± 14%, 94 ± 4% and 74 ± 14% for Au, As, and Sb respectively. WebFeb 22, 2024 · The Tonian–Cambrian Dalradian Supergroup in Scotland is a siliciclastic–carbonate succession that can be up to 10 km thick. The consensus view is that its lower part, the mid- to late Tonian Grampian and Appin groups, formed in rift basins: the deep marine turbidites of the Grampian Group infilled rift depocentres, whereas the … WebThe Dalradian rocks were folded and metamorphosed during the Caledonian orogeny, which reached its acme at about 490–470 Ma. Four phases of folding and deformation, … sighthill edinburgh college