Graphitization of Neoproterozoic sedimentary marbles in The Aird, Scottish Highlands
Heptinstall, E. a., Parnell, J., Schito, A., Boyce, A. j., Armstrong, J. g., Muirhead, D.
Scottish Journal of Geology, vol. 60, no. 2, sjg2023-013
Contributions to Journals: Articles
Speciation of trace elements in the Bowland Shale
Parnell, J., Nwoko, K., Feldmann, J., Armstrong, J.
Geological Society, London, Special Publications, vol. 534, no. 1, pp. 241-256
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An introduction to the Bowland Shale Formation, UK: processes and resources
Emmings, J. F., Parnell, J., Stephenson, M. H., Lodhia, B. H.
Geological Society Special Publication, vol. 534, no. 1, pp. 1-18
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Trace element release from Bowland Shale into spring water in Lancashire
Armstrong, J. G. T., Parnell, J., Boyce, A. J., Perez, M.
Geological Society Special Publication, vol. 534, pp. 229-239
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The record of coal exploration in the Ordovician-Silurian in the Southern Uplands of Scotland and the north of Ireland
Parnell, J., Armstrong, J. G. T., Lings, A.
Earth and Environmental Science Transactions of the Royal Society of Edinburgh
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Cycling of rare earth elements at the Precambrian-Cambrian boundary
Armstrong, J. G. T., Parnell, J.
Global and Planetary Change, vol. 236, 104434
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Molecular and mineral biomarker record of terrestrialization in the Rhynie Chert
Akinsanpe, T., Bowden, S., Parnell, J.
Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 640, 112101
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Trace element minerals from carbonatite-related fluids, The Aird, Scotland
Heptinstall, E. A., Parnell, J., Boyce, A. J., Still, J. W.
Scottish Journal of Geology, vol. 59, no. 1-2, sjg2021-015
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The stable isotope (C, O, S) record of Paleoproterozoic marbles, Scotland
Parnell, J., Boyce, A. J., Armstrong, J. G., Schito, A., Muirhead, D.
Scottish Journal of Geology, vol. 59, no. 1-2, sjg2023-009
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The Role of Organic Carbon in the Southern Uplands-Down-Longford Terrane Accretionary Prism, Scotland and Ireland
Parnell, J., Armstrong, J., Blamey, N., Boyce, A. J., Schito, A., Muirhead, D.
Petroleum Geoscience, vol. 29, no. 3
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