Exposed marine Devonian rocks of Great Britain are in South-West England where successions together span most of the Devonian Period. The Geological Conservation Review (GCR) sites of the volume are located in Cornwall and Devon, the latter providing the historic stratotype of the Devonian System. Site stratigraphies are linked to basins of three sub-provinces. Those represent different, albeit largely penecontemporaneous, tectonosedimentary regimes of the differing settings of the Rhenohercynian Zone. The sites and their selection criteria based on their international and national importance in understanding Devonian geological history are listed. A History of Research section provides a detailed review of work on the Devonian rocks of the...
Abstra & The Portscatho Formation, within the allochthonous unit of the Middle and Upper Devoni...
During the Devonian of the Rhenich geosyncline (sediments exposed in the Rheinisches Schiefergebirge...
The Upper Greensand Formation, mostly capped by the Chalk, crops out on the edges of a broad, dissec...
The majority of ‘Marine Devonian’ GCR sites are located on the Early to Latest Devonian rocks of cen...
The North Devon Basin, situated in a more proximal passive margin regime than the rift basins to the...
Abstract: A formal stratigraphy based on new macrofaunal evidence is proposed for a little-known are...
Until the 19th century, the rocks exposed throughout the provinces of Devonshire and Cornwall in sou...
This is the first volume of the Geological Conservation Review (GCR) of Great Britain to be publishe...
Deep marine deposits of the Gramscatho Basin of south Cornwall reflect two tectonic regimes; Early t...
The Devonian record presents an opportunity to test and validate an existing marine bioregionalizati...
This report details the stratigraphy and palaeogeography of Devonian and Carboniferous rocks of the ...
Upper Cretaceous rocks, primarily Chalk, cover a vast area of England forming the Downs and Wolds as...
Abstract: Different methods of clay mineral correlation within sedimentary sequences provide varying...
This report presents an up dated biostratigraphical framework for correlation of the Middle Devonian...
This study is the first regional synthesis and sequence stratigraphic interpretation of the Namurian...
Abstra & The Portscatho Formation, within the allochthonous unit of the Middle and Upper Devoni...
During the Devonian of the Rhenich geosyncline (sediments exposed in the Rheinisches Schiefergebirge...
The Upper Greensand Formation, mostly capped by the Chalk, crops out on the edges of a broad, dissec...
The majority of ‘Marine Devonian’ GCR sites are located on the Early to Latest Devonian rocks of cen...
The North Devon Basin, situated in a more proximal passive margin regime than the rift basins to the...
Abstract: A formal stratigraphy based on new macrofaunal evidence is proposed for a little-known are...
Until the 19th century, the rocks exposed throughout the provinces of Devonshire and Cornwall in sou...
This is the first volume of the Geological Conservation Review (GCR) of Great Britain to be publishe...
Deep marine deposits of the Gramscatho Basin of south Cornwall reflect two tectonic regimes; Early t...
The Devonian record presents an opportunity to test and validate an existing marine bioregionalizati...
This report details the stratigraphy and palaeogeography of Devonian and Carboniferous rocks of the ...
Upper Cretaceous rocks, primarily Chalk, cover a vast area of England forming the Downs and Wolds as...
Abstract: Different methods of clay mineral correlation within sedimentary sequences provide varying...
This report presents an up dated biostratigraphical framework for correlation of the Middle Devonian...
This study is the first regional synthesis and sequence stratigraphic interpretation of the Namurian...
Abstra & The Portscatho Formation, within the allochthonous unit of the Middle and Upper Devoni...
During the Devonian of the Rhenich geosyncline (sediments exposed in the Rheinisches Schiefergebirge...
The Upper Greensand Formation, mostly capped by the Chalk, crops out on the edges of a broad, dissec...