The Palaeoproterozoic to early Neoproterozoic Annagh Gneiss Complex structurally underlies the Dalradian sequence in north Mayo, Ireland, and has been proposed as the depositional basement to Dalradian metasediments. The Annagh Gneiss Complex was deformed, metamorphosed and migmatized during the Grenville Orogeny and later reworked under amphibolite-facies conditions. This paper focuses on the timing of the post-Grenville events and particularly on the possible presence of post-Grenville, pre-Grampian deformation that could be attributed to the Knoydartian Orogeny. Seven U–Pb titanite analyses from Annagh Gneiss Complex gneisses have a weighted mean 207Pb/206Pb age of 963 ± 8 Ma, which dates cooling after the main Grenville metamorphism. Lo...
Irish Geological Research Meeting 2018, University College Cork, Ireland, 23-25 February 2018The Gra...
The Grenville Province is a remnant of a ca. 1.1 Ga orogen, exposed as a continuous belt in northeas...
Author Posting. © Geological Society of London, 2002. This article is posted here by permission of ...
Metasediments of the early Dalradian Grampian Group (Erris Group) and probable equivalents (Inishkea...
Accurately reconstructing the growth of continental margins during episodes of ocean closure has imp...
Abstract: Rb–Sr and 40Ar/39Ar step-heating and in situ 40Ar/39Ar laserprobe dating of fabric-forming...
The Early Ordovician Grampian Orogeny in the British Isles represents a classic example of collision...
Geological history and age determination of the Tyrone Igneous Complex and Tyrone Central Inlier are...
2015 GSA Annual Meeting, Baltimore, Maryland, USA, 1-4 November, 2015Here we extend the analysis of...
A study of the composition of detrital garnets from Ordovician siliciclastics from the Midland Valle...
Granulite-facies metamorphism affecting the Slishwood Division was extreme. Three samples yielded P–...
An intriguing and contradictory scenario has recently developed in the Caledonides of the British Is...
A multidisciplinary provenance study, including in situ U-Pb dating of detrital titanite, was undert...
This study addresses the timing and pressure-temperature (P-T) conditions of ophiolite obduction, on...
The Lough Nafooey arc, in the western Irish Caledonides, collided with Laurentia during the Early Or...
Irish Geological Research Meeting 2018, University College Cork, Ireland, 23-25 February 2018The Gra...
The Grenville Province is a remnant of a ca. 1.1 Ga orogen, exposed as a continuous belt in northeas...
Author Posting. © Geological Society of London, 2002. This article is posted here by permission of ...
Metasediments of the early Dalradian Grampian Group (Erris Group) and probable equivalents (Inishkea...
Accurately reconstructing the growth of continental margins during episodes of ocean closure has imp...
Abstract: Rb–Sr and 40Ar/39Ar step-heating and in situ 40Ar/39Ar laserprobe dating of fabric-forming...
The Early Ordovician Grampian Orogeny in the British Isles represents a classic example of collision...
Geological history and age determination of the Tyrone Igneous Complex and Tyrone Central Inlier are...
2015 GSA Annual Meeting, Baltimore, Maryland, USA, 1-4 November, 2015Here we extend the analysis of...
A study of the composition of detrital garnets from Ordovician siliciclastics from the Midland Valle...
Granulite-facies metamorphism affecting the Slishwood Division was extreme. Three samples yielded P–...
An intriguing and contradictory scenario has recently developed in the Caledonides of the British Is...
A multidisciplinary provenance study, including in situ U-Pb dating of detrital titanite, was undert...
This study addresses the timing and pressure-temperature (P-T) conditions of ophiolite obduction, on...
The Lough Nafooey arc, in the western Irish Caledonides, collided with Laurentia during the Early Or...
Irish Geological Research Meeting 2018, University College Cork, Ireland, 23-25 February 2018The Gra...
The Grenville Province is a remnant of a ca. 1.1 Ga orogen, exposed as a continuous belt in northeas...
Author Posting. © Geological Society of London, 2002. This article is posted here by permission of ...