U–Pb apatite geochronology is increasingly recognized as a valuable tool for constraining
the age of mid-crustal ductile shear zones. The crustal-scale Outer Hebrides Fault Zone …

The Neoarchaean foreland basement of the Faroe-Shetland terrane (FST) displays
abundant evidence for isotopic resetting of U-Pb systems in apatite between c. 1800 and …

Ion-microprobe U–Th–Pb geochronological data are presented for four samples from
Paleoproterozoic belts in the Lewisian of the northern Outer Hebrides, north-west Scotland …

The South Harris Complex of the Scottish Outer Hebrides forms a distinctive component of
the Lewisian Complex and contains three supposedly co-magmatic meta-igneous bodies, a …

Pseudotachylites within the Neoarchaean to Palaeoproterozoic basement of the Lewisian
Gneiss Complex have been analysed using the high spatial resolution 40Ar/39Ar UV …

In mafic systems where primary mineral assemblages have witnessed moderate-to high-
temperature hydrous overprinting and deformation, little is known about the retentivity of the …

In ancient basement regions such as the Lewisian Complex, NW Scotland, the ages of brittle
deformation events are commonly poorly constrained owing to a lack of datable fills. An …

The Outer Hebrides Fault Zone is a major ESE-dipping detachment exposed within
basement gneisses of the Archaean–Palaeoproterozoic Lewisian Complex, northwest …

The Jarrow assemblage is a Lagerstätte of Pennsylvanian tetrapods and fish preserved in
the Leinster Coalfield, Ireland. Fossils from this site have an interesting taphonomy that is …

U–Pb zircon ages obtained from the late-to post-tectonic 'Newer Granite'suite in Shetland,
northernmost Scottish Caledonides, indicate a significantly more protracted intrusion history …