1887
PDF

Abstract

The Fastnet Basin is a small, elongate, northeast-southwest-trending basin situated at the south-western end of the North Celtic Sea Basin. Together with the North and South Celtic Sea basins and the Cockburn Basin, it forms part of a series of basins whose formation, during the Triassic, was related to the opening of the North Atlantic, the Norwegian-Greenland Sea and the Tethys Ocean. Initial rifting would have followed inherited Caledonide and Variscide fault trends.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201410233
1994-06-10
2024-04-24
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410233
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error