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GM2.7 | What’s new with cosmogenic nuclides?
EDI PICO
What’s new with cosmogenic nuclides?
Convener: Gerald Raab | Co-conveners: Romano Clementucci, Zsófia Ruszkiczay-Rüdiger, Sebastien Lenard
The introduction of cosmogenic nuclides in (quantitative) geomorphology and geochronology spurred developments that transformed them into essential tools in these fields. Cosmogenic nuclides provide information on the exposure ages of features at the surface (e.g., river terraces, fault and landslide scarps, glacial moraines), burial ages of deep deposits, as well as quantitative information on the rates and evolution of surface processes (e.g., surface denudation, weathering, soil mixing), and are even used as a tool for paleoaltimetry, paleo-environment reconstruction and to yield information about planetary objects and meteorites. Continued technique development and creative applications expand the ways we use cosmogenic nuclides.

We invite projects at any stage, from early development to well-established methods applied to novel situations. These include new laboratory setups, measurement methods, laboratory techniques for extraction, modeling, theoretical advancements, and all cosmogenic nuclide applications.