首页 | 本学科首页   官方微博 | 高级检索  
     检索      


The Precambrian–Cambrian nonconformity at the Ercall Quarries,The Wrekin,Shropshire, UK
Authors:Jamie K Pringle  Ian G Stimpson
Institution:School of Physical Sciences & Geography, William Smith Building, Keele University, Keele, Staffs, ST5 5BG, UK. j.k.pringle@keele.ac.uk, i.g.stimpson@keele.ac.uk
Abstract:The Precambrian–Cambrian boundary is iconic, marking the first appearance of shelly fauna in the fossil record, and opening the Phanerozoic Eon. In England and Wales, the transition from predominantly Precambrian igneous rocks to Cambrian sedimentary strata is generally unconformable. An exceptional exposure of this transition can be observed in the Ercall Quarries in Shropshire, a classic locality in all senses of the word.
Keywords:
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号