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3D Seismic reflection evidence for lower crustal intrusions beneath the Faroe–Shetland Basin, NE Atlantic Margin (2023)
Journal Article
Layfield, L. K., Schofield, N., Watson, D., Holford, S. P., Jolley, D. W., Kilhams, B. A., Muirhead, D. K., Roberts, A. M., Alvey, A. D., Ellwood, A., & Widdowson, M. (2023). 3D Seismic reflection evidence for lower crustal intrusions beneath the Faroe–Shetland Basin, NE Atlantic Margin. Journal of the Geological Society, 180(5), Article jgs2022-172. https://doi.org/10.1144/jgs2022-172

Lower crustal intrusion is considered to be a common process along volcanic or magma-rich passive margins, including the NE Atlantic Margin, where it is thought to have occurred during phases of Paleogene magmatism, both prior to and during continent... Read More about 3D Seismic reflection evidence for lower crustal intrusions beneath the Faroe–Shetland Basin, NE Atlantic Margin.

Relicts of Neo-Tethyan mantle wedge in the Indo-Burma Range, India: Record of carbonate metasomatism and Neo-Tethyan mantle evolution (2023)
Journal Article
Kingson, O., Liu, Y., Bhutani, R., & Widdowson, M. (in press). Relicts of Neo-Tethyan mantle wedge in the Indo-Burma Range, India: Record of carbonate metasomatism and Neo-Tethyan mantle evolution. Results in Earth Sciences, Article 100001. https://doi.org/10.1016/j.rines.2023.100001

Several different geochemical signatures, i.e., mid-oceanic ridge (MOR) and supra subduction zone (SSZ), are frequently reported from ophiolite belts. Such bi-modal geochemical signatures are generally interpreted in terms of formation in two contras... Read More about Relicts of Neo-Tethyan mantle wedge in the Indo-Burma Range, India: Record of carbonate metasomatism and Neo-Tethyan mantle evolution.