Metasediments of the early Dalradian Grampian Group (Erris Group) and probable equivalents (Inishkea Division) structurally overlie Palaeoproterozoic to Neoproterozoic Annagh Gneiss Complex orthogneisses in NW Mayo, Ireland. Sm-Nd isotopic data suggest a Palaeoproterozoic source for the metasediments. K-feldspar and granitoid clasts from the Doonamo Formation, Erris Group, record U-Pb zircon ages of c. 1740 Ma and c. 980 Ma, respectively. These ages are within error of the c. 1730-1750 Ma Mullet gneisses and c. 990 Ma Grenvillian migmatitic leucosomes in the underlying Annagh Gneiss Complex. U-Pb detrital zircon data reveal that the Erris Group was deposited after c. 955 Ma, with predominant input from c. 1640, c. 1500 and c. 990 Ma interpr...
Whole-rock Sm-Nd model ages of 1601 Ma (lower Laggan Formation) and 1674 Ma (upper Blackrock Formati...
An intriguing and contradictory scenario has recently developed in the Caledonides of the British Is...
The Early Ordovician Grampian Orogeny in the British Isles represents a classic example of collision...
Metasediments of the early Dalradian Grampian Group (Erris Group) and probable equivalents (Inishkea...
The Palaeoproterozoic to early Neoproterozoic Annagh Gneiss Complex structurally underlies the Dalra...
The Lower Old Red Sandstone in southern Ireland is hosted in the Early Devonian Dingle Basin, which ...
The Lower Old Red Sandstone in southern Ireland is hosted in the Early Devonian Dingle Basin, which ...
The Tyrone Central Inlier is a metamorphic terrane of uncertain affinity situated outboard of the m...
Detrital zircon analysis of sandstones interbedded with c. 464 Ma ignimbrites in the lower Mweelrea ...
<p>The Tyrone Central Inlier is a metamorphic terrane of uncertain affinity situated outboard of the...
A multidisciplinary provenance study, including in situ U-Pb dating of detrital titanite, was undert...
Abstract: Rb–Sr and 40Ar/39Ar step-heating and in situ 40Ar/39Ar laserprobe dating of fabric-forming...
Accurately reconstructing the growth of continental margins during episodes of ocean closure has imp...
Abstract: U–Pb ages determined by laser-ablation multi-collector inductively coupled plasma mass spe...
The Caledonides of Britain and Ireland include terranes attributed to both Laurentian and Gondwanan ...
Whole-rock Sm-Nd model ages of 1601 Ma (lower Laggan Formation) and 1674 Ma (upper Blackrock Formati...
An intriguing and contradictory scenario has recently developed in the Caledonides of the British Is...
The Early Ordovician Grampian Orogeny in the British Isles represents a classic example of collision...
Metasediments of the early Dalradian Grampian Group (Erris Group) and probable equivalents (Inishkea...
The Palaeoproterozoic to early Neoproterozoic Annagh Gneiss Complex structurally underlies the Dalra...
The Lower Old Red Sandstone in southern Ireland is hosted in the Early Devonian Dingle Basin, which ...
The Lower Old Red Sandstone in southern Ireland is hosted in the Early Devonian Dingle Basin, which ...
The Tyrone Central Inlier is a metamorphic terrane of uncertain affinity situated outboard of the m...
Detrital zircon analysis of sandstones interbedded with c. 464 Ma ignimbrites in the lower Mweelrea ...
<p>The Tyrone Central Inlier is a metamorphic terrane of uncertain affinity situated outboard of the...
A multidisciplinary provenance study, including in situ U-Pb dating of detrital titanite, was undert...
Abstract: Rb–Sr and 40Ar/39Ar step-heating and in situ 40Ar/39Ar laserprobe dating of fabric-forming...
Accurately reconstructing the growth of continental margins during episodes of ocean closure has imp...
Abstract: U–Pb ages determined by laser-ablation multi-collector inductively coupled plasma mass spe...
The Caledonides of Britain and Ireland include terranes attributed to both Laurentian and Gondwanan ...
Whole-rock Sm-Nd model ages of 1601 Ma (lower Laggan Formation) and 1674 Ma (upper Blackrock Formati...
An intriguing and contradictory scenario has recently developed in the Caledonides of the British Is...
The Early Ordovician Grampian Orogeny in the British Isles represents a classic example of collision...