The powerful combination of high-resolution geochronological data, innovative isotopic geochemistry and petro-structural analysis is continuously progressing our understanding of geological processes within the Earth's dynamic lithosphere. Moreover, the development of new techniques and improvement of analytical equipment inspire future progress and development.
This session aims to highlight multiscale and multi-disciplinary approaches to the use of radiogenic isotopes in unravelling duration and mechanisms of geological processes in different environments. Particularly we welcome contributions in which geochronology is coupled with petrology, major, trace elements and isotope geochemistry, phase equilibrium modelling, and structural geology.