New developments in the Re-Os isotope system
New developments in the Re-Os isotope system
Session ID#: 121165
Session Description:
Rhenium and osmium (Re-Os) are mostly enriched in sulfides, mantle derived rocks, organic-rich sedimentary rocks, crude oil, and environmental products. This makes the Re-Os system a powerful tool to date geological processes in multiple disciplines. Recent theoretical and analytical advances in mass spectrometry have also opened up the exciting possibility of using stable Re and Os isotopes to trace environmental and magmatic processes.
This session invites contributions from all aspects of Re and Os isotope geochemistry (both stable and radiogenic), including but not limited to: theoretical calculations, modelling, analytical method development, geochronology, continental growth, mantle geochemistry, mineral and petroleum exploration, and modern- and paleo-environments.
Index Terms:
1040 Radiogenic isotope geochemistry [GEOCHEMISTRY]
3699 General or miscellaneous [MINERALOGY AND PETROLOGY]
4912 Biogeochemical cycles, processes, and modeling [PALEOCEANOGRAPHY]
8499 General or miscellaneous [VOLCANOLOGY]
Primary Convener: Zeyang Liu, GIG Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China
Conveners: Yang Li, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China and Alexander J Dickson, Royal Holloway University of London, Earth Sciences, Egham, United Kingdom
Primary Liaison: Zeyang Liu, GIG Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China
See more of: Volcanology, Geochemistry and Petrology