Nature and timing of Late Mississippian to Mid-Pennsylvanian glacio-eustatic sea-level changes of the Pennine Basin, UK: Discussion Reply

Waters, C.N.; Condon, D.J.. 2013 Nature and timing of Late Mississippian to Mid-Pennsylvanian glacio-eustatic sea-level changes of the Pennine Basin, UK: Discussion Reply. Journal of the Geological Society, 170 (5). 850. https://doi.org/10.1144/jgs2013-055

Full text not available from this repository. (Request a copy)

Official URL: http://dx.doi.org/10.1144/jgs2013-055

Abstract/Summary

Although we appreciate that the points made by Bailey are relevant to any discussion of interpreting stratigraphic patterns as being astronomically paced, we take this opportunity to discuss the details of the Carboniferous of the Pennine Basin beyond simple rock thickness–time concepts or models and reiterate points relevant to the conclusions of Waters & Condon (2012), namely the nature of the expression of sea-level variation within the Carboniferous Pennine Basin and its regional and global geological context.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1144/jgs2013-055
ISSN:	0016-7649
Date made live:	12 Nov 2013 14:18 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/503800

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1144/jgs2013-055

ISSN:

0016-7649

Date made live:

12 Nov 2013 14:18 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/503800