Geosyncline-Margin Sedimentary Rocks in Silurian of West Connacht, Ireland
- 1 January 1969
- book chapter
- Published by American Association of Petroleum Geologists AAPG/Datapages
Abstract
The Upper Llandoverian rocks of West Connacht that are present between the Highland Boundary fault and the Dalradian inlier of Connemara were depositKeywords
This publication has 0 references indexed in Scilit: