Abstract
AbstractEvidence is adduced to relate the published minimum absolute date of — 475 m.y., for the metamorphism of the Connemara Schists, to its correct position in the Lower Palaeozoic stratigraphy of Western Ireland. The metamorphism pre-dates the Didymograptus extensus zone of the Arenig in Connemara and South Mayo and an Upper Cambrian or Tremadocian age is considered likely.
Publisher
Cambridge University Press (CUP)
Reference15 articles.
1. A gepchronological study of the metamorphic complexes of the Scottish Highlands;Giletti;Proc. geol. Soc.,1961
2. The Age of the Connemara Schists and of their Metamorphism
3. The discovery of Cambrian trilobites in the Highland Border rocks near Callender, Perthshire;Pringle;Advanc. Sci.,1940
4. IV.—Geology of West Galway and S.W. Mayo, Ireland
5. The Wenlock Strata of South Mayo
Cited by
53 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