Session Details

R8: Metamorphic rocks and tectonics

Thu. Sep 12, 2024 3:30 PM - 6:00 PM JST
Thu. Sep 12, 2024 6:30 AM - 9:00 AM UTC
ES024 Higashiyama Campus
Chairperson:Yui Kouketsu(Nagoya University), Shunsuke Endo

[R8-01]Toward the establishment of "EBSD method for the detection of quartz with phase transition to coesite": Incorporation of the Gongen area, Sanbagawa metamorphic belt, Shikoku, SW-Japan「発表賞エントリー」

*Momoko Minowa1, Takayoshi Nagaya1, Taisuke Ito2, Simon Wallis2 (1. Tokyo Gakugei University, 2. The University of Tokyo)

[R8-02]Pressure-Temperature-Time Conditions of The Basement Rocks in The Banggai-Sula Microcontinent, Indonesia「発表賞エントリー」

*Fransiska Ayuni Catur Wahyuandari1, Nobuhiko Nakano1, Tatsuro Adachi1, Nugroho Imam Setiawan2 (1. Kyushu Univ., 2. Gadjah Mada Univ.)

[R8-03]Amphibolites from the Mineoka belt revisited

*Yuji ICHIYAMA1, Shun Takamizawa1, Hisatoshi Ito2, Akihiro Tamura3, Tomoaki Morishita3 (1. Chiba University, 2. Central Research Institute of ElectricPower Industry, 3. Kanazawa University)

[R8-04]Compositional heterogeneity of garnet in garnet-biotite felsic granulite, Czech Republic

*Daisuke NAKAMURA1, Yuuka FUJIMURA1, Yuuki KODERA1 (1. Okayama University)

[R8-06]Observations of geological structures and microstructures associated with strain release at a continental plate boundary fault「発表賞エントリー」

*Haruki Yoshiasa1, Jun-ichi Ando1,2, Kaushik Das1,2, Dyuti Prakash Sarkar3 (1. Hiroshima University, 2. HiPeR, 3. JAMSTEC)

[R8-07]Comparison and verification study of new sample forms for use in Raman carbonaceous material geothermometer「発表賞エントリー」

*Shunsuke Ogino1, Yui Kouketsu1, Satoshi Takahashi1 (1. Nagoya Univ. Env.)

[R8-09]Microstructural and petrological characteristics of the Ryoke mylonite occurred along the Median Tectonic Line in the Shinshiro area, Aichi Prefecture

*Miharu Niwa1,2, Katsuyoshi Michibayashi1,3, Kenichiro Tani4, Takuma Nishimura5 (1. Nagoya Univ. Env., 2. TMNH, 3. JAMSTEC, 4. NMNS, 5. HMNH)

[R8-10]Re-proposal of the metamorphic zone division in the Horokanai area of the Kamuikotan Belt based on the mineral paragenesis and phengite K-Ar Age.

*Takao HIRAJIMA1, Kousuke Naemura2, Kenta Yoshida3 (1. Kyoto University, 2. Iwate University, 3. JAMSTEC)