The Lough Foyle Basin is a half-graben that straddles the border between Northern Ireland and the Republic of Ireland and contains sediments that range in age from Lower Carboniferous to Holocene. The basin’s post-rift succession is represented by sediments of the Penarth Group and Lias Group. The lithostratigraphy and biostratigraphy of that interval are revised using new borehole material and existing outcrop. Palaeontological data provide a chronostratigraphic framework and aid palaeoenvironmental interpretations. Foraminifera, ostracods, palynomorphs indicate a nearshore, marginal marine depositional setting throughout much of the Rhaetian with a more marine, shelf and nearshore depositional setting for the Lias Group. The Penarth Group...
This offshore area comprises two broadly NNE–trending Mesozoic and Tertiary basins present to the n...
A thick and relatively complete succession of Carboniferous rocks of Tournaisian to Westphalian age...
The North Celtic Sea Basin (NCSB) is one of a number of basins related to regional Mesozoic extensio...
The thickest section of Early Jurassic strata known from onshore Ireland (total Jurassic thickness 5...
Northern Ireland Waterloo Mudstone Formation has received relatively little attention due to the sca...
Microfossil abundance data and oxygen & carbon stable isotope data presented in this pape
The Celtic Sea area, offshore southern Ireland, is underlain by several discrete rift basins, part o...
Abstract: The Celtic Sea, offshore southern Ireland, is underlain by several discrete rift basins, w...
The Jurassic and Cretaceous sedimentary infill of the Irish and Celtic Sea Basins is intimately asso...
During the Carboniferous, Northern Ireland straddled a zone of dextral strike-slip, comparable to t...
Alluvial sediments of Continental Old Red Sandstone aspect have been examined in northeast Ireland. ...
The Carboniferous rocks of the Dublin Basin extend from the east coast of north Co. Dublin westward...
There have been many studies into the post-Palaeozoic exhumation history of the Irish Sea basin syst...
A continuous succession of marine and marginal-marine sediments of Rhaetian (Late Triassic) and Hett...
The latest Triassic to earliest Jurassic transition has been widely studied due the occurrence of a ...
This offshore area comprises two broadly NNE–trending Mesozoic and Tertiary basins present to the n...
A thick and relatively complete succession of Carboniferous rocks of Tournaisian to Westphalian age...
The North Celtic Sea Basin (NCSB) is one of a number of basins related to regional Mesozoic extensio...
The thickest section of Early Jurassic strata known from onshore Ireland (total Jurassic thickness 5...
Northern Ireland Waterloo Mudstone Formation has received relatively little attention due to the sca...
Microfossil abundance data and oxygen & carbon stable isotope data presented in this pape
The Celtic Sea area, offshore southern Ireland, is underlain by several discrete rift basins, part o...
Abstract: The Celtic Sea, offshore southern Ireland, is underlain by several discrete rift basins, w...
The Jurassic and Cretaceous sedimentary infill of the Irish and Celtic Sea Basins is intimately asso...
During the Carboniferous, Northern Ireland straddled a zone of dextral strike-slip, comparable to t...
Alluvial sediments of Continental Old Red Sandstone aspect have been examined in northeast Ireland. ...
The Carboniferous rocks of the Dublin Basin extend from the east coast of north Co. Dublin westward...
There have been many studies into the post-Palaeozoic exhumation history of the Irish Sea basin syst...
A continuous succession of marine and marginal-marine sediments of Rhaetian (Late Triassic) and Hett...
The latest Triassic to earliest Jurassic transition has been widely studied due the occurrence of a ...
This offshore area comprises two broadly NNE–trending Mesozoic and Tertiary basins present to the n...
A thick and relatively complete succession of Carboniferous rocks of Tournaisian to Westphalian age...
The North Celtic Sea Basin (NCSB) is one of a number of basins related to regional Mesozoic extensio...