All Outputs (4)

New onshore insights into the role of structural inheritance during Mesozoic opening of the Inner Moray Firth Basin, Scotland (2021)
Journal Article
Tamas, A., Holdsworth, R. E., Underhill, J. R., Tamas, D. M., Dempsey, E. D., Hardman, K., …Selby, D. (2022). New onshore insights into the role of structural inheritance during Mesozoic opening of the Inner Moray Firth Basin, Scotland. Journal of the Geological Society, 179(2), Article 066. https://doi.org/10.1144/jgs2021-066

The Inner Moray Firth Basin (IMFB) forms the western arm of the North Sea trilete rift system that initiated mainly during the Late Jurassic–Early Cretaceous with the widespread development of major NE–SW-trending dip-slip growth faults. The IMFB is... Read More about New onshore insights into the role of structural inheritance during Mesozoic opening of the Inner Moray Firth Basin, Scotland.

Reinvestigating the relationships between the Badenoch Group, Dalradian Supergroup and the Grampian Shear Zone (2021)
Thesis
Evason, L. A. (2021). Reinvestigating the relationships between the Badenoch Group, Dalradian Supergroup and the Grampian Shear Zone. (Thesis). University of Hull. Retrieved from https://hull-repository.worktribe.com/output/4223712

In situ monazite and titanite U-Pb LA-ICP-MS geochronology and combined petrological and microstructural analysis has revealed both Neoproterozoic and Ordovician deformation within the Grampian Shear Zone (GSZ), central Scotland. The Grampian Shear Z... Read More about Reinvestigating the relationships between the Badenoch Group, Dalradian Supergroup and the Grampian Shear Zone.

A revised age, structural model and origin for the North Pennine Orefield in the Alston Block, northern England: intrusion (Whin Sill)-related base metal (Cu–Pb–Zn–F) mineralization (2021)
Journal Article
Dempsey, E. D., Holdsworth, R. E., Selby, D., Bird, A., Young, B., & Cornu, C. L. (2021). A revised age, structural model and origin for the North Pennine Orefield in the Alston Block, northern England: intrusion (Whin Sill)-related base metal (Cu–Pb–Zn–F) mineralization. Journal of the Geological Society, 178(4), Article jgs2020-226. https://doi.org/10.1144/jgs2020-226

Mineralization and associated fluid migration events in the c. 1500 km2 North Pennine Orefield (NPO) are known to be associated with tectonic activity, but the age of these tectonic events and origins of the base metal sulfide mineralization remain u... Read More about A revised age, structural model and origin for the North Pennine Orefield in the Alston Block, northern England: intrusion (Whin Sill)-related base metal (Cu–Pb–Zn–F) mineralization.

Caledonian and pre-Caledonian orogenic events in Shetland, Scotland: evidence from garnet Lu-Hf and Sm-Nd geochronology (2021)
Book Chapter
Walker, S., Bird, A. F., Thirllall, M. F., & Strachan, R. A. (2021). Caledonian and pre-Caledonian orogenic events in Shetland, Scotland: evidence from garnet Lu-Hf and Sm-Nd geochronology. In J. B. Murphy, R. A. Strachan, & C. Quesada (Eds.), Pannotia to Pangaea: Neoproterozoic and Paleozoic Orogenic Cycles in the Circum-Atlantic Region (305-331). London: Geological Society. https://doi.org/10.1144/SP503-2020-32

Garnet Lu-Hf and Sm-Nd ages from the Shetland Caledonides provide evidence of a pollorogenic history as follows: 1) c. 1050 Ma Grenvillian reworking of Neoarchaean basement; 2) c. 910 Ma Renlandian metamorphism of the Westing Group; 3) c. 622-606 Ma... Read More about Caledonian and pre-Caledonian orogenic events in Shetland, Scotland: evidence from garnet Lu-Hf and Sm-Nd geochronology.