Professor John Parnell

Kaolin polytype evidence for a hot-fluid pulse along Caledonian thrusts during rifting of the European margin

• [ONLINE] DOI: https://doi.org/10.1180/0026461046830195

Methane-related authigenic carbonates from the Black Sea: geochemical characterisation and relation to seeping fluids

• [ONLINE] DOI: https://doi.org/10.1016/j.margeo.2004.08.001

Mineral Radioactivity in Sands as a mechanism for fixation of organic carbon on the Earthly Earth

• [ONLINE] DOI: https://doi.org/10.1023/B:ORIG.0000043132.23966.a1

Record of fluid flow history through fractured conglomerates, Lower Old Red Sandstone of central Scotland

The origin and tectonic significance of Lewisian- and Torridonian-hosted clastic dykes near Gairloch, NW Scotland

The preservation of fluid inclusions in diverse surface precipitates: the potential for sampling palaeo-water from surface deposits on Mars

• [ONLINE] DOI: https://doi.org/10.1017/S1473550404001867

The role of Raman spectroscopy as an astrobiological tool in the exploration of Mars

• [ONLINE] DOI: https://doi.org/10.1002/jrs.1189

Titanium mobilization by hydrocarbon fluids related to sill intrusion in a sedimentary sequence, Scotland

• [ONLINE] DOI: https://doi.org/10.1016/j.oregeorev.2003.08.010

The structural and diagenetic evolution of injected sandstones: examples from the Kimmeridgian of NE Scotland

• [ONLINE] DOI: https://doi.org/10.1144/0016-764902-091

A low-cost approach to the exploration of mars through a robotic technology demonstrator mission

• [ONLINE] View publication in Scopus