The Saturn project is aimed at developing geo-software for industry and academic applications. Two academic applications have already been developed. These are currently being tested for U-Pb and Trace Element
AIRG is currently improving new methods to obtain in situ isotope information of apatite. The mineral apatite is a key mineral for thermochronology studies via U/Th–He, fission-track and U-Pb dating.
In addition to in-situ trace element compositions, AIR-G is now providing state of the art in situ U-Pb and Sr-Sr of carbonatic rocks for research and oil exploration. We are
Anatexis of the continental crust with the efficient extraction of granitoid melts is a fundamental process that governs the internal architecture of a number of orogenic belts around the world.
Here we develop and apply methods in LA-ICP-MS for a wide range of geological/mineralogical applications Here we develop a few methods in stable isotopes via LA-ICP-MS for geological applications. We
A craton is a large, stable block of the Earth’s crust that forms the foundation of continents and has survived the cycles of continental drift, rifting, and tectonic activity over
Archean and Proterozoic Basins We are currently using isotopes to investigate a number of Archaean and Proterozoic basins in South America. Amongst the most important isotope methods used are: U-Pb