V11F:
Insight into Earth's Mantle and Deep Subduction Processes through Accessory Minerals and Microinclusions I

Session ID#: 2885

Monday, 15 December 2014: 8:00 AM-10:00 AM
Salons 4-6 (Marriott Marquis)
Chairs:  Larissa Dobrzhinetskaya, Univ California Riverside, Riverside, CA, United States and Yoshihide Ogasawara, Waseda University, Tokyo, Japan
Primary Convener:  Larissa Dobrzhinetskaya, Univ California Riverside, Riverside, CA, United States
Co-conveners:  Harry W Green II, Univ California, Riverside, CA, United States and Yoshihide Ogasawara, Waseda University, Tokyo, Japan
OSPA Liaison:  Yoshihide Ogasawara, Waseda University, Tokyo, Japan
Co-Sponsor(s):
  • DI - Study of the Earth's Deep Interior
  • EGU-GMPV - European Geophysical Union-Geochemistry Mineralogy Petrology and Volcanology
  • MR - Mineral and Rock Physics
  • T - Tectonophysics
Index Terms:

3621 Mantle processes [MINERALOGY AND PETROLOGY]
3652 Pressure-temperature-time paths [MINERALOGY AND PETROLOGY]
3653 Fluid flow [MINERALOGY AND PETROLOGY]
3654 Ultra-high pressure metamorphism [MINERALOGY AND PETROLOGY]
Virtual Option?: No

Abstracts Submitted to this Session:

Welcoming Remarks
Unusual tiny inclusions and accessory minerals: evidence of ultra-deep origin and low-pressure modification of the Luobusa podiform chromitites (Invited) (2669)
Shinji Yamamoto, University of Tokyo, Bunkyo-ku, Japan, Tsuyoshi Komiya, University of Tokyo, Department of Earth Science and Astronomy, Tokyo, Japan and Shigenori Maruyama, Tokyo Institute of Technology, Department of Earth and Planetary Sciences, Tokyo, Japan
Mantle Recycling of Crustal Materials through Study of Ultrahigh-Pressure Minerals in Collisional Orogens, Ophiolites, and Xenoliths (10272)
Juhn G Liou1, Tatsuki Tsujimori2, Jingsui Yang3, Ru-Yuan Zhang1 and W G Ernst1, (1)Stanford University, Dept. of Geological and Environmental Sciences,, Stanford, CA, United States, (2)Okayama University, Institute for Study of the Earth's Interior, Misasa, Japan, (3)CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology of CAGS, Beijing, China
Hydrogen Incorporation in Bridgmanite and Water in Earth's Lower Mantle (6185)
Joseph R Smyth, University of Colorado Boulder, Department of Geological Sciences, Boulder, CO, United States
The Importance of Redox Reactions in Fluid Transport Systems in the Earth's Deep Mantle: Evidence from Nano-Inclusions (Invited) (11737)
Dorrit E Jacob, Macquarie University, Sydney, NSW, Australia, Richard Wirth, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany and Larissa Dobrzhinetskaya, Univ California Riverside, Riverside, CA, United States
Microdiamonds from the European Variscan Orogenic Belt (Invited) (10444)
Jana Kotkova1,2, Petra Jakubova2, Martin J Whitehouse3 and Yana Fedortchouk4, (1)Czech Geological Survey, Prague, 118, Czech Republic, (2)Masaryk University, Department of Geological Sciences, Brno, Czech Republic, (3)Swedish Museum of Natural History, Department of Geosciences, Stockholm, Sweden, (4)Dalhousie University, Department of Earth Sciences, Halifax, NS, Canada
Maruyamaite, a new K-dominant tourmaline coexisting with diamond –an important accessory mineral in UHP rocks (29198)
Rentaro Shimizu and Yoshihide Ogasawara, Waseda University, Tokyo, Japan
5 min