Ireland and neighbouring Britain share much of their tectonic history and are both far from
active plate boundaries at present. Their seismicity shows surprising lateral variations, with …

Faults are important structures in the formation of many mineral deposits, often acting as
conduits for ore-forming fluids and sometimes providing, or generating, the bounding …

Faults and fractures are a critical store and pathway for groundwater in Ireland's limestone
bedrock aquifers either directly as conductive structures or indirectly as the locus for the …

The evolution of rift basins is often influenced by the reactivation of pre-existing structures, a
response that is partly controlled by the angular relationship between fault strike and the …

The Variscan orogen in southern Ireland and Britain is characterized by an intensely
deformed, EW–trending fold-and-thrust belt. Farther north in Ireland, the Carboniferous …

Abstract The Celtic Sea basins lie on the continental shelf between Ireland and northwest
France and consist of a series of ENE–WSW trending elongate basins that extend from St …

In contrast to much of the European Atlantic margin, the influence of salt on basin evolution
has received little attention to date in the basins west of Ireland, despite salt being proven in …

板内小位移走滑断裂在全球广泛发育, 对沉积盆地油气运聚成藏和差异富集具有重要控制作用.
在对我国中西部三大含油气盆地内部小位移走滑断裂几何学特征对比分析基础上 …

The Lundy Island (Bristol Channel, UK) granite is a felsic expression of the southernmost
igneous centre of the North Atlantic Igneous Province that emplaced millions of cubic …

Airborne magnetics have found few applications in investigating basalt-trapped areas
because anomaly interferences from deep and shallow sources prevent clear identification …