Japan Geoscience Union Meeting 2015

Presentation information

Oral

Symbol S (Solid Earth Sciences) » S-RD Resources, Mineral Deposit & Resource Exploration

[S-RD41] Developments in resource geology: Origin and evolution of ore fluids

Mon. May 25, 2015 9:00 AM - 10:45 AM 106 (1F)

Convener:*Kenzo Sanematsu(Mineral Resource Research Group, Institute for Geo-Resources and Environment, National Institute of Advanced Industrial Science and Technology), Tatsuo Nozaki(Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology), Tsubasa Otake(Division of Sustainable Resources Engineering, Faculty of Engineering, Hokkaido University), Ryohei Takahashi(Faculty of International Resource Sciences, Akita University), Chair:Kenzo Sanematsu(Mineral Resource Research Group, Institute for Geo-Resources and Environment, National Institute of Advanced Industrial Science and Technology), Tatsuo Nozaki(Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology)

9:40 AM - 10:00 AM

[SRD41-03] Lithium isotope index as powerful research tool for earth resource

*Yoshiro NISHIO1 (1.JAMSTEC)

Keywords:lithium isotope, deep crustal fluid, geochemical thermometer, fluid inclusion

Lithium (Li) is one of important natural resources, because Li is used for secondary battery of electric and/or hybrid vehicles. The lightest alkali element, Li, is one of fluid-mobile elements. The leaching of Li from sediments into fluids is dramatically elevated together with increasing temperature, and the fact that subsequent re-uptake of the leached Li from the fluid by sediments (which occurs as the fluid cools) takes a considerable time. Li is relatively unaffected by surface water contamination because the Li contents of deep-rooted fluid samples are much greater than the surface water content. The two stable isotopes of Li are 6Li and 7Li, and their relative abundances are about 7.5% and 92.5%, respectively. Furthermore, the difference in the 7Li/6Li ratio between fluid and solid phases varies with the reaction temperature. As a result, the Li isotope ratio is a potentially useful geothermometer because the Li cation is monovalent and hence not redox sensitive, and it is not a nutrient, so it does not participate in biologically mediated reactions.
In this presentation, I'll talk about fundamental feature of Li isotope tool at first, and after then I show the potential of Li isotope tool for earth resource science.