The Woodsmith polyhalite orebody formed from evaporation of brines on the basin margin of the ancient Zechstein Sea, some 250 million years ago. The FTG survey will pick up subtle differences in density between evaporite minerals, namely sulphate and chloride minerals, which predominate in separate areas of the basin. This newly acquired information is being integrated with complementary pre-existing 2D seismic data and drill hole information to further map and model the coastline at the time of the polyhalite deposit formation. Improving our understanding of the overall basin morphology will allow us to better understand the smaller scale geometry of the orebody itself, enabling us to plan and mine more effectively and safely in the future.
Now that the survey is complete the data is being processed. Interpretation will involve sophisticated science and maths, integrating physics-constrained neural networks to generate synthetic density models. It will involve collaboration across multiple disciplines in the wider Anglo American group, with the local geologists at Woodsmith working closely with the global Discovery and Geosciences team, and utilising cutting-edge Machine Learning insight from the global Data Analytics team, to ensure we will get the most value from the information.