Craig Magee

TL;DR: In this paper, the authors synthesize field-and seismic reflection-based observations and highlight that extensive lateral magma transport may occur within mafic sill complexes, promoting the development of volcanoes that do not overlie the melt source.

TL;DR: In this paper, the authors presented a study dedicated to the memory of Dr Ken Thomson, who pioneered early work looking at intrusions within the Faroe-Shetland Basin.

TL;DR: In this paper, the authors examined both brittle and non-brittle intrusion mechanisms and expand upon them with field observations from a series of widespread and variable magmatic systems, and incorporated variable host material behaviours in numerical and analogue modelling, tuned using direct field observations, to further further understand the controls on shallow-level intrusion.

TL;DR: In this article, the authors use high-quality 2D seismic reflection data from the Ceduna Subbasin, offshore southern Australia, to quantitatively analyse 56, pristinely-preserved, Eocene-age volcanogenic mounds, and a genetically-related network of subvolcanic sills and laccoliths.

TL;DR: In this article, the authors used 3D seismic reflection data from the Irish Rockall Basin, offshore western Ireland, to constrain the structural style and emplacement history of a sill complex that contains 82 seismically resolved intrusions.