Abstract

Palaeocurrents from the northernmost Aberystwyth Grits Formation are consistently from the north, which is at variance with the generally accepted southerly source area for the rest of the formation. The anomalous directions appear to indicate a structural high and possible sediment source to the north.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.