Japan Geoscience Union Meeting 2015

Presentation information

Oral

Symbol M (Multidisciplinary and Interdisciplinary) » M-TT Technology & Techniques

[M-TT44] Frontiers in Geochemistry: Prospect for geochemistry in 30 years

Tue. May 26, 2015 4:15 PM - 6:00 PM 102B (1F)

Convener:*Takafumi Hirata(Graduate School of Science, Kyoto University), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Urumu Tsunogai(Graduate School of Environmental Studies, Nagoya University), Hajime Obata(Marine inorganic chemistry division, Atmosphere and Ocean Research Institute, University of Tokyo), Shogo Tachibana(Department of Natural History Scieces, Hokkaido University), Katsuhiko Suzuki(Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology), Gen Shimoda(Geological Survey of Japan, AIST), Hiroyuki Kagi(Geochemical Laboratory, Graduate School of Science, University of Tokyo), Yusuke Yokoyama(Atmosphere and Ocean Research Institute, University of Tokyo), Tetsuya Yokoyama(Department of Earth and Planetary Sciences, Graduate School of Science and Engineering, Tokyo Institute of Technology), Chair:Takafumi Hirata(Graduate School of Science, Kyoto University), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo)

5:00 PM - 5:15 PM

[MTT44-06] Studies of the Earth's Interior and Geochemistry

*Hikaru IWAMORI1 (1.Japan Agency for Marine-Earth Science and Technology)

In this presentation, I would like to discuss the following points, in terms of the relationship between studies of the Earth's interior and geochemistry, referring to several examples from the combined studies. First, geochemistry concerns both geoscience and chemistry. How we balance the two does matter for both geochemists and the others. Second, how we relate mechanisms and processes of an elemental scale to global scale-phenomena requires some concrete methods which lie often outside geochemistry. An approach bridging the two scales may play an important role. Third, since the Earth (and the planetary) system is highly complex, there is no doubt that combining information available from all geoscience fields (including geochemistry) is crucial. As an example, `Geofluid Map` in the crust and mantle is discussed.