Location: Wern Ddu Clay Pit (Coed y Werin), Caerphilly, Wales, UK
The site is owned and managed by the Caerphilly Woodlands Trust, and the Wern Ddu Clay Pit is designated as a Geological Site of Special Scientific Interest.
Senior Geochemist/Basin Modeller
Location: Lyme Regis, Dorset, UK
Cliffs below Devonshire Head (SY:328-910 to SY:332-914) between Seven Rock Point and Monmouth Beach
Access: Monmouth Beach is accessed via Cobb Road, just to the west of the Boat Building Academy (SY:335-915)
Title: Clay Mineralogy, Organic Matter and Climate of the Blue Lias Formation, Lyme Regis - By…
Senior Geochemist/Basin Modeller
Location: Hartland Quay, Devon, UK
Hartland Quay Car park (SS:223-247) to Warren Beach (SS:225-249) Access: Warren Beach is accessed via Hartland Quay slipway north of The Wrecker's Retreat Inn (SS:223-248)
Title: Folding without cracking - By Andrew Green
The cliffs north of Hartland Quay present a spectacular array of antiformal and synformal folds, including…
Senior Geochemist/Basin Modeller
By Paul Farrimond
The C29 hopane, 30-norhopane, is not only a member of the series of regular hopanes but also of a less common series that lack the methyl group at C-22 in the side chain, the 30-norhopanes.
Director & Technical Advisor
By Tiago Cunha & Marianne Nuzzo
MARUM - Centre for Marine Environmental Sciences, University of Bremen, Germany
Javier GarcÃa-Pintado & Marta Pérez-Gussinyé
We introduced the usage of a box-size numerical model of miscible multiphase flow, with explicit advection and diffusion in both the liquid and gas phases, to model the migration and…
Senior Petroleum Geochemist / Basin Modeller
By Andrew Green
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In petroleum geochemistry, a source rock is classified as an interval of rock that contains sufficient organic matter of the right type that has the potential to generate, or has already generated, commercial quantities of hydrocarbons.
Senior Geochemist/Basin Modeller
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Office Manager
Storage of CO2 in geological formations depends on a combination of physical and chemical mechanisms such as physical trapping below caprocks or trapping by dissolution in groundwater. The most effective storage mechanism is the permanent mineralisation of CO2 by conversion into carbonate minerals (Benson et al. , 2005).
Seep biogeochemistry & organic geochemistry
A major aim of reactive flow models in CCS activities is to understand and predict the evolution of the CO2 plume injected in the reservoir for planning and monitoring purposes (e. g. Jenkins et al. , 2015).
Seep biogeochemistry & organic geochemistry
This unusual hopane-like compound is recognised together with the hopanes in the m/z 191 mass chromatogram and was for many years used as a biomarker of hypersalinity due to its common high abundance in sediments deposited under such conditions.  However, a key paper by Sinninghe-Damsté et al.
Director & Technical Advisor