Abstract
SummaryAn earliest Llanvirn age is established on micropalaeontological grounds for the interbedded lava–pelite sequence at the base of the Binsey Volcanic Formation in the northern Lake District. The northern volcanic sequence, here termed the Eycott Volcanic Group, is earlier than, and chemically distinct from, the main Borrowdale Volcanic Group. The evidence precludes a regional unconformity between the Skiddaw Slates and the overlying volcanic rocks, but is compatible with the hypothesis that the vulcanicity occurred in an island arc environment.
Publisher
Cambridge University Press (CUP)
Reference22 articles.
1. North–South trending pre-cleavage folds in the Skiddaw Slate Group of the English Lake District;Webb;Nature,1972
2. Microfossils from the Skiddaw Group
3. Sections through the Skiddaw–Borrowdale unconformity in eastern Lakeland;Wadge;Proc. Yorks. geol. Soc.,1971
4. Age of cleavage in the Skiddaw Slates in relation to the Skiddaw aureole
5. THREE CRITICAL LOCALITIES ON THE JUNCTION OF THE BORROWDALE VOLCANIC ROCKS WITH THE SKIDDAW SLATES IN THE LAKE DISTRICT
Cited by
38 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献