For access to project outputs see
https://www2.bgs.ac.uk/HiTechAlkCarb/(opens in new window).
The team developed the following new geomodels:
1. an online catalogue of alkaline rocks and carbonatites (
http://alkcarb.myrocks.info/(opens in new window))
2. a mineral-systems model which can be used to describe and predict mineralisation in alkaline and carbonatite systems at province to district scale,
3. a conceptual model of the nature of mineralisation within alkaline and carbonatite complexes and their idealised 3D structure,
4. an idealised deposit-scale 3D model for large alkaline silicate complexes, delivered as a 3D pdf. This model contains geology, and process mineralogy that leads towards environmental and social impacts, in a concise and comprehensive approach to exploration characteristics.
5. a 3D model for carbonatite-dominated systems featuring the HiTech AlkCarb natural lab at the Kaiserstuhl extinct volcano (Germany), including its niobium and REE-rich rocks, delivered as a video.
To provide data, comparisons, geological and geophysical research to feed into these geomodels, fieldwork was carried out in all of our natural labs (Germany, Italy, Greenland, Malawi, Mongolia, Namibia, South Africa and Scotland). Partners and invited Expert Councillors have taken part in workshops and field visits to gather information from recent academic and industry projects, and discuss hypotheses.
Much of research has been published, or is on route to publication in international peer reviewed journals. Highlights include a major review of fenite alteration haloes around carbonatites, pyrochlore as a monitor for magmatic and hydrothermal processes, formation of the niobium tantalum deposit at Motzfeldt (Greenland), role of phosphorus in controlling the REE budget in carbonatites, formation of a fluorite deposit associated with volcanic rocks in Italy, a review of mantle to mine of Italian carbonatites, and a review of scandium.
Our new geomodels aimed to incorporate environmental and social factors and a report has been prepared concentrating on the radioactive elements often associated with REE - the main public concern regarding mining of REE deposits. Our own experiences of concerns regarding drilling in Germany have been written up as a policy paper and shared with colleagues on other EU funded projects and with the Commission.
Our geophysics research aimed to provide information about geological structures at depth for the geomodels and improve interpretation of the geology using geophysics results. Our field work at Kaiserstuhl is complete and written up. Highlights include the discovery of a new target area and other probable extensions of Kaiserstuhl hidden under sedimentary cover. Drone surveys were particularly successful at the scale needed for REE exploration. Geophysics expertise was also applied at the Songwe Hill REE carbonatite project (Malawi).
95 boreholes (total 9.8 km) were logged with spectral gamma, conductivity, magnetic susceptibility, and gyro deviation to test the correlation between geophysical signals, geology and REE. This was particularly effective in identifying important gangue minerals. An NSAMT geophysical survey shows potential carbonatite extension.