日本地球惑星科学連合2019年大会

講演情報

[E] 口頭発表

セッション記号 S (固体地球科学) » S-SS 地震学

[S-SS06] Nankai Trough Seismogenic Zone Experiment: Logging and sampling the seismogenic megathrust

2019年5月28日(火) 13:45 〜 15:15 コンベンションホールB (2F)

コンビーナ:金川 久一(千葉大学大学院理学研究科)、Demian M Saffer(Pennsylvania State University)、木下 正高(東京大学地震研究所)、座長:金川 久一(千葉大学大学院理学研究科)、Saffer Demian(Department of Geosciences, Pennsylvania State University)、木下 正高(東京大学地震研究所)

14:00 〜 14:15

[SSS06-02] Deep Drilling at the Nankai Trough: IODP NanTroSEIZE Expedition 358 Summary and First Results

★Invited Papers

*Harold Tobin1Takehiro Hirose7Matt Ikari5Kyuichi Kanagawa10Gaku Kimura3Masataka Kinoshita8Hiroko Kitajima6Demian M Saffer4Asuka Yamaguchi9Lena Maeda2Nobu Eguchi2Sean Toczko2 (1.Department of Earth and Space Sciences, University of Washington、2.JAMSTEC-CDEX、3.Tokyo Un. of Marine Science-Technology、4.Penn State University、5.MARUM Un. of Bremen、6.Texas A&M University、7.JAMSTEC-KCC、8.Un. of Tokyo Earthquake Research Institute、9.Un. of Tokyo AORI、10.Chiba University)

キーワード:Nankai Trough, IODP , megathrust

IODP Expedition 358 was carried out beginning October 10, 2018 and scheduled to continue until March 31, 2019. The primary objective was to sample and make geophysical measurements in and around the megasplay fault/plate boundary fault at Site C0002, by extending the riser borehole (Hole C0002P) established during previous Integrated Ocean Drilling Program NanTroSEIZE expeditions. After Expedition 348 in 2014, Hole C0002P was left suspended, with steel casing in pace holding the borehole open to 2922 meters below the sea floor (mbsf). The primary seismic reflector target interpreted as the main plate boundary fault zone was estimated to lie at a little more than 5000 mbsf, necessitating a plan to re-enter that hole and then add about 2000 meters of new depth drilling to reach and cross it.

Drilling commenced with a sidetracking operation to establish Hole C0002Q, which was advanced to 3263 mbsf, but operational difficulties precluded going any deeper. Two more attempts were made to advance the riser hole over many weeks, but ultimately did not result in further progress toward the objective. At the time of this writing, coring operations are ongoing at the site at a depth of about 2900 mbsf, in deformed and steeply-dipping mid-Miocene age inner accretionary wedge rocks. There are plans to end riser operations at Site C0002 at the end of February 2019 despite not reaching the primary target, and instead commence drilling at a new site to target the frontal thrust portion of the plate boundary near previous IODP Site C0006. First results from the expedition will be reviewed in this presentation, and a preliminary assessment of the scientific outcomes will be made.