[S-MP32] Deformed rocks, Metamorphic rocks and Tectonics

Wed. May 29, 2019 10:45 AM - 12:15 PM A08 (TOKYO BAY MAKUHARI HALL)

convener:Yumiko Harigane(Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST)), Yoshihiro Nakamura(Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology), Chairperson:Tomoki Taguchi(京都大学　大学院理学研究科), Kenta Yoshida(JAMSTEC)

We invite all researchers who aim to understand the dynamics of the earth's crust and mantle at the plate boundaries, to discuss the latest results from various viewpoints. The scope will include contributions through petrology and structural geology as well as various techniques including rheology and transformation of heat and mass.

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10:45 AM - 11:00 AM

[SMP32-07] Garnet zoning suggesting the correlation between the Higo and Abukuma metamorphic rocks

*Tadao Nishiyama¹, Yuto Wakida¹ (1.Department of Earth and Environmental Sciences, School of Science, Graduate School of Science and Technology, Kumamoto University)

11:00 AM - 11:15 AM

[SMP32-08] FeAlO₃ phase at ultrahigh-temperature metamorphic conditions: Evidences from the sillimanite—Fe₂O₃ and sillimanite—Fe₃O₄ systems at 9 kbar and 1050 ℃

*Toshisuke Kawasaki¹, Tatsuro Adachi², Hiroaki Ohfuji¹, Yasuhito Osanai² (1.Ehime University, 2.Kyushu University)

11:15 AM - 11:30 AM

[SMP32-09] Halogens in nanogranitoids entrapped during granulite facies to ultrahigh-temperature metamorphism in the lower crust

*Fumiko Higashino¹, Tetsuo Kawakami² (1. Graduate School of Environmental Studies, Tohoku University, 2.Graduate School of Science, Kyoto University)

11:30 AM - 11:45 AM

[SMP32-10] Significance of high-Ti biotite and anatectic conditions of paragneiss in the Oki-Dogo Island, Japan

Hiroshi Yoshida¹, *Shunsuke Endo¹, Mai Fujiwara¹, Atsushi Kamei¹ (1.Department of Earth Science, Interdisciplinary Faculty of Science and Engineering, Shimane University)

11:45 AM - 12:00 PM

[SMP32-11] Eclogite-to-granulite transition in the Ufipa Complex (Tanzania): the time-lag between collision and the granulitization

*Morita Isamu¹, Tatsuki Tsujimori¹, Nelson Boniface², Shogo Aoki³, Kazumasa Aoki³ (1.Tohoku University, 2.University of Dar es Salaam, 3.Okayama University of Science)

12:00 PM - 12:15 PM

[SMP32-12] Switching of metamorphic growth kinetics due to volume fraction of metamorphic fluid

*Kazuhiro Miyazaki¹ (1.Orogenic Processes Research Group, Institute of Geology and Geoinformation, Geological Survey of Japan/National Institute of Advanced Industrial Science and Technology)

Session information

[S-MP32] Deformed rocks, Metamorphic rocks and Tectonics

[SMP32-07] Garnet zoning suggesting the correlation between the Higo and Abukuma metamorphic rocks

[SMP32-08] FeAlO₃ phase at ultrahigh-temperature metamorphic conditions: Evidences from the sillimanite—Fe₂O₃ and sillimanite—Fe₃O₄ systems at 9 kbar and 1050 ℃

[SMP32-09] Halogens in nanogranitoids entrapped during granulite facies to ultrahigh-temperature metamorphism in the lower crust

[SMP32-10] Significance of high-Ti biotite and anatectic conditions of paragneiss in the Oki-Dogo Island, Japan

[SMP32-11] Eclogite-to-granulite transition in the Ufipa Complex (Tanzania): the time-lag between collision and the granulitization

[SMP32-12] Switching of metamorphic growth kinetics due to volume fraction of metamorphic fluid

Authentication

Session information

[S-MP32] Deformed rocks, Metamorphic rocks and Tectonics

[SMP32-07] Garnet zoning suggesting the correlation between the Higo and Abukuma metamorphic rocks

[SMP32-08] FeAlO3 phase at ultrahigh-temperature metamorphic conditions: Evidences from the sillimanite—Fe2O3 and sillimanite—Fe3O4 systems at 9 kbar and 1050 ℃

[SMP32-09] Halogens in nanogranitoids entrapped during granulite facies to ultrahigh-temperature metamorphism in the lower crust

[SMP32-10] Significance of high-Ti biotite and anatectic conditions of paragneiss in the Oki-Dogo Island, Japan

[SMP32-11] Eclogite-to-granulite transition in the Ufipa Complex (Tanzania): the time-lag between collision and the granulitization

[SMP32-12] Switching of metamorphic growth kinetics due to volume fraction of metamorphic fluid

Authentication

[SMP32-08] FeAlO₃ phase at ultrahigh-temperature metamorphic conditions: Evidences from the sillimanite—Fe₂O₃ and sillimanite—Fe₃O₄ systems at 9 kbar and 1050 ℃