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GroupLast nameFirst nameAffilationTitleStudent?Comment from AuthorShort PresentationLong PresentationSlack ChannelSlack Channel URL
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AllAll PresentationsPlease join slack & sptial chat for free discussion!All:https://www.dropbox.com/sh/leadvhzs1r2u47b/AADV8J65xqaMlhdIUf1C8AnQa?dl=0
https://join.slack.com/t/sloweqws2020virtual/shared_invite/zt-gu0hikae-CH23HqMoTlg1t1pGyhVIAg
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A01A01 All PresentationsA01班のショートプレゼン連結動画・全プレゼンへのリンクです。Short:https://www.dropbox.com/s/ud8mfyamp6bjcj5/S_A01_all.mp4?dl=0All:https://www.dropbox.com/sh/rvlbvehb1k0cuyv/AAAmw_ylfKSfG6-XQ_oCn6Uaa?dl=0
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A01AsoNaofumi東工大Observation of Volcanic Deep-Long-Period Earthquakes in North-Eastern Hiroshima発表は、広島県北東部で実施している地震観測に関するものですが、様々な議論・雑談・相談などウェルカムです。https://www.dropbox.com/s/46ghz12u25u0s39/S_A01_Aso_N.mov?dl=0https://www.dropbox.com/s/tqzkkvwlmqq45zp/L_A01_Aso_N.pdf?dl=0#p-a01-asohttps://app.slack.com/client/T01845XT9A9/C01AGLGP9R9
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A01BabaSatoru東京大学地震研究所Shallow very low frequency earthquakes accompanying low frequency tremors near the trench axis in the Costa Rica subduction zonestudent中米コスタリカにおける、超低周波地震の検出と、低周波微動のエネルギー推定を行いましたhttps://www.dropbox.com/s/puiv0nt6dvfnrmd/S_A01_Baba_Satoru.mp4?dl=0https://www.dropbox.com/s/fvc3bekzku15g19/L_A01_Baba_Satoru.mp4?dl=0#p-a01-babahttps://app.slack.com/client/T01845XT9A9/C01AAS2J066
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A01KatoAitaroERI, UTokyoDetection of deep low-frequency earthquakes in the Nankai subduction zone over 11 years using a matched filter techniquehttps://www.dropbox.com/s/4ehdfbcy8dp0lhn/L_A01_Kato_Aitaro.pdf?dl=0#p-a01-katohttps://app.slack.com/client/T01845XT9A9/C01A5QHNM63
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A01KawakuboSusumu東北大学理学研究科地球物理学専攻　地震・噴火予知研究観測センターShallow low-frequency tremor activity off Erimo, Hokkaido from 2006 to 2007 revealed from pop-up type ocean bottom seismometersstudent北海道襟裳沖でS-net設置以前の2006年から2007年に発生した低周波微動活動を捉えました。https://www.dropbox.com/s/zbgaz9kne6cfjil/S_A01_Kawakubo_Susumu.mp4?dl=0https://www.dropbox.com/s/uys30cyx9ii0ha3/L_A01_Kawakubo_Susumu.mp4?dl=0#p-a01-kawakubohttps://app.slack.com/client/T01845XT9A9/C01A1FH051U
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A01MaedaTakuya東京大学地震研究所Detection and evaluation of tremor migration beneath Kii Peninsula student東大地震研M1の前田です。紀伊半島において微動マイグレーションの抽出と評価を行いました。https://www.dropbox.com/s/pv1sd13ksnayvxc/S_A01_Maeda_Takuya.mov?dl=0https://www.dropbox.com/s/hhdm8laxe0x996h/L_A01_Maeda_Takuya.mov?dl=0#p-a01-maedahttps://app.slack.com/client/T01845XT9A9/C01A70JQD8W
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A01MiyazawaMasatoshi京都大学防災研究所Bayesian approach for detecting very low-frequency earthquakes dynamically triggered by surface waveshttps://www.dropbox.com/s/39qxhsa8efowrfv/S_A01_Miyazawa_M.mp4?dl=0https://www.dropbox.com/s/ym20ua7vsi46ay3/L_A01_Miyazawa_M.mp4?dl=0#p-a01-miyazawahttps://app.slack.com/client/T01845XT9A9/C019ZR8AZPY
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A01NakamuraMamoruUniversity of the RyukyusTime-space distribution of very-low frequency earthquakes in the northern Ryukyu Trench using ocean-bottom seismometers北部琉球海溝で発生した超低周波地震の活動を、広帯域海底地震計で調べました。https://www.dropbox.com/s/efa4tez759sb8sr/S_A01_Nakamura_Mamoru.mp4?dl=0https://www.dropbox.com/s/154bp60bfgl9dge/L_A01_Nakamura_Mamoru.pdf?dl=0#p-a01-nakamurahttps://app.slack.com/client/T01845XT9A9/C01B69S6J48
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A01NishikawaTomoaki京都大学防災研究所Detection of Earthquake Swarms along the Hikurangi Trench: Insights into the Relationship between Seismicity and Slow Slip Eventsニュージーランド・ヒクランギ海溝ではSSEに同期して群発地震が発生します。本研究では新しい群発地震カタログの作成を行いました。https://www.dropbox.com/s/uy0izxlfa1gp70q/S_A01_Nishikawa_Tomoaki.mov?dl=0https://www.dropbox.com/s/x3at6eq0xtuc8jo/L_A01_Nishikawa_Tomoaki.mov?dl=0#p-a01-nishikawahttps://app.slack.com/client/T01845XT9A9/C01ASB3LCRX
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A01ObaraKazushigeERI, UTokyoLong-term variation of deep low frequency tremor seismicity西南日本における深部低周波微動活動の20年間における経年的な変化について、その主な原因が長期的SSEによるものであることが分かりました。https://www.dropbox.com/s/6312y3acwufcyt9/S_A01_Obara_K.mp4?dl=0https://www.dropbox.com/s/druuo1xjjj5vne3/L_A01_Obara_K.mp4?dl=0#p-a01-obarahttps://app.slack.com/client/T01845XT9A9/C019TF5BYTH
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A01OhtaKazuaki防災科学技術研究所(NIED)Detailed tremor activity beneath the eastern Shikoku and Kii channel, southwest Japan, revealed by dense seismic observation四国東部〜紀伊水道下の微動とLFEの震源決定(絶対深さ推定)のお話．左記zoomは出入り自由なので適宜お声掛けください．slackも定期的に確認しています．https://www.dropbox.com/s/h7io54bajgrwbqu/L_A01_Ohta_Kazuaki.pdf?dl=0#p-a01-ohtahttps://app.slack.com/client/T01845XT9A9/C01AL9WUMQV
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A01TakahashiHidenobu東北大学Activities of low frequency tremors in Sanriku-Oki before the 2011 Tohoku-Oki earthquakestudent宮城沖，岩手沖における低周波微動の検出とその活動度の特徴に関して調べました．https://www.dropbox.com/s/gelkd81ua82skw7/S_A01_Takahashi_Hidenobu.mp4?dl=0https://www.dropbox.com/s/z32yks7jv6hm2rd/L_A01_Takahashi_Hidenobu.mp4?dl=0#p-a01-takahashi-hidenobuhttps://app.slack.com/client/T01845XT9A9/C01A1FJ5TML
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A01TakemuraShunsuke東京大学地震研究所Envelope-based inversion of source time functions for shallow low-frequency tremors southeast off the Kii Peninsula 3次元差分法で計算した地震波形エンベロープをGreen関数とした震源時間関数推定手法の開発をはじめました。https://www.dropbox.com/s/an2peacep39k89j/S_A01_Takemura_Shunsuke.mp4?dl=0https://www.dropbox.com/s/mc76f49ax7bqquz/L_A01_Takemura_Shunsuke.mp4?dl=0#p-a01-takemurahttps://app.slack.com/client/T01845XT9A9/C017SNKU6K1
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A01TakeoAkikoERI, UTokyoFull-automatic detection of deep very low frequency earthquake in the Nankai subduction zoneノイズや遠地地震の影響で難しい超低周波地震検出を完全自動化して「感度」と「陽性的中率」を推定しました。https://www.dropbox.com/s/fh7p6vb92sb01xl/S_A01_Takeo_Akiko.mp4?dl=0https://www.dropbox.com/s/rq02g1g8hmtqjx7/L_A01_Takeo_Akiko.mp4?dl=0#p-a01-takeohttps://app.slack.com/client/T01845XT9A9/C01B3HN5VDE
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A01TanakaYusakuERI2004年スマトラ地震や2011年東北沖地震の後に見られる超長期的な粘弾性緩和について衛星重力観測で見ると巨大地震後の粘弾性緩和が超長期的に進行しているようだ(GNSS等で見るよりも遥かに時定数が長い)という話です。アフタースリップ等を考える際の背景知識としてこのWSに出しております。https://www.dropbox.com/s/1e1l2kkwe1loz9o/S_A01_Tanaka_Yusaku.mp4?dl=0https://www.dropbox.com/s/hn6zw60oa3d555s/L_A01_Tanaka_Yusaku.mp4?dl=0#p-a01-tanaka-yusakuhttps://app.slack.com/client/T01845XT9A9/C01AED40YRJ
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A01UchidaNaokiGraduate School of Science, Tohoku UniversityDynamic structure of subduction zone mantle wedge revealed by shear-wave splitting of S-net seafloor data東北日本前弧の異方性をS-netデータを用いて推定し、プレートとマントルウエッジ間のカップリングに関して考察しました。https://www.dropbox.com/s/qjw0zjrt9fxfjlv/L_A01_Uchida_Naoki.mp4?dl=0#p-a01-uchidahttps://app.slack.com/client/T01845XT9A9/C01ALGVLR8S
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A01YamashitaYusuke京都大学防災研究所宮崎観測所Shallow low-frequency tremor at Hyuga-nada (2017-2018)新学術領域研究で実施した第1期観測の結果について報告します．2017-2018年の活動は2013年の活動と様々な特徴がよく似ていました．https://www.dropbox.com/s/ba7zx1118bvsnzn/S_A01_Yamashita_Yusuke.mp4?dl=0https://www.dropbox.com/s/ygp1ghm1wy7skds/L_A01_Yamashita_Yusuke.mp4?dl=0#p-a01-yamashita-yusukehttps://app.slack.com/client/T01845XT9A9/C019W46NQSK
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A02A02 All PresentationsA02班のショートプレゼン連結動画・全プレゼンへのリンクです。Short:https://www.dropbox.com/s/7l4oimjycvni854/S_A02_all.mp4?dl=0All:https://www.dropbox.com/sh/ivqkod4r36m2hjk/AADYgMKBtkxZv-h7wyy-lnrca?dl=0
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A02ChujoNaoya神戸大学大学院理学研究科惑星学専攻Slip distributions of short-term slow slip events in the northern Kii Peninsula based on NIED Hi-net tilt measurementsstudent紀伊半島北部におけるS-SSEのすべり分布を推定し、累積地震モーメント等について議論しました。https://www.dropbox.com/s/j6leh09ddljrn96/S_A02_Chujo_Naoya.mp4?dl=0https://www.dropbox.com/s/btlqz0lp4dw7hoz/L_A02_Chujo_Naoya.pdf?dl=0#p-a02-chujohttps://app.slack.com/client/T01845XT9A9/C01AV3D4FPT
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A02HiroseHitoshi神戸大学都市安全研究センターSlip distributions of short-term slow slip events in Shikoku, southwest Japan from 2001 to 2019 based on tilt change measurements左記のZoomは 9/16 9:30-18:00いつでも使えますので、私に関係なく、ご自由にお使いください。（なるべくいるようにしますが）https://www.dropbox.com/s/kp1xlray62vgoxn/S_A02_HIROSE_Hitoshi.mp4?dl=0https://www.dropbox.com/s/vhnk5w37ii45czd/L_A02_HIROSE_Hitoshi.pdf?dl=0#p-a02-hirose-hitoshihttps://app.slack.com/client/T01845XT9A9/C01AGLEU727
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A02KanoMasayuki東北大学Spatial and temporal relation between slow and large earthquakes: inference from crustal deformation data地殻変動データから示唆される巨大地震とスロー地震の関係（固着域下端でのゆっくりすべり、昔のＳＳＥは大きかった？）を紹介します（公募研究の途中経過）https://www.dropbox.com/s/h9nl66alqmr8hph/S_A02_Kano_M.mp4?dl=0https://www.dropbox.com/s/duvk92n6lrllm39/L_A02_Kano_M.pdf?dl=0#p-a02-kanohttps://app.slack.com/client/T01845XT9A9/C01ADMZP7KL
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A02NishimuraTakuya京都大学防災研究所Slow slip events in the Kanto and Tokai regions of central Japan detected using GNSS data during 1994-2019https://www.dropbox.com/s/wx1h29ytedr6fsn/S_A02_Nishimura_T.mp4?dl=0https://www.dropbox.com/s/7tjddk6n0l3zw2e/L_A02_Nishimura_T.pdf?dl=0#p-a02-nishimurahttps://app.slack.com/client/T01845XT9A9/C01AGLC3F5Z
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A02OkadaYutaro京都大学大学院理学研究科Development of the detection method for short-term slow slip events by using GNSS data and its application to the Nankai subduction zonestudenthttps://www.dropbox.com/s/fi636nqwyn1bb8g/S_A02_Okada_Yutaro.mp4?dl=0https://www.dropbox.com/s/34gv51s0gtqhlmh/L_A02_Okada_Yutaro.pdf?dl=0#p-a02-okadahttps://app.slack.com/client/T01845XT9A9/C01AV3E58SD
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A02TakagiRyota東北大学Detection of slow slip events on the Philippine Sea plate beneath the Kanto regionhttps://www.dropbox.com/s/ot3hkdof87vhl7g/S_A02_Takagi_Ryota.mp4?dl=0https://www.dropbox.com/s/phj7xgckpgu346t/L_A02_Takagi_Ryota.pdf?dl=0#p-a02-takagihttps://app.slack.com/client/T01845XT9A9/C01AM7W9KMG
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A02TanakaYoshiyukiDep. Earth and Planetary Science, UTokyoToward the detection of gravity signals accompanied by long-term slow slip eventshttps://www.dropbox.com/s/drjowb5gf7bftpg/S_A02_Tanaka_Yoshiyuki.mp4?dl=0https://www.dropbox.com/s/y1okgs7l2gmvnn7/L_A02_Tanaka_Yoshiyuki.mp4?dl=0#p-a02-tanaka-yoshiyukihttps://app.slack.com/client/T01845XT9A9/C019W441BM5
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A02TeshibaSawako神戸大学大学院理学研究科Slow slip events in the afterslip area of the 1996 Hyuganada earthquakes, based on GNSS datastudentGNSSデータから西南日本の非地震性すべりの時空間発展（2000年以前）を推定し、イベントの発生間隔・領域を議論しました。https://www.dropbox.com/s/caa4n0jrahudtl6/S_A02_Teshiba_Sawako.mp4?dl=0https://www.dropbox.com/s/wlfryo0rdazp8yb/L_A02_Teshiba_Sawako.pdf?dl=0#p-a02-teshibahttps://app.slack.com/client/T01845XT9A9/C01ADU5C2AF
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A02UkawaTomoki神戸大学大学院 理学研究科 惑星学専攻房総スロースリップイベントに伴う群発地震活動に基づく応力変化の推定studentDieterich et al. (2000)の手法を用いて、地震活動率から、SSE周辺域(群発地震域)の応力変化の推定を試みました。https://www.dropbox.com/s/9cupqpdn4866m5a/S_A02_Ukawa_Tomoki.mp4?dl=0https://www.dropbox.com/s/2eezsxti6at6kns/L_A02_Ukawa_Tomoki.mp4?dl=0#p-a02-ukawahttps://app.slack.com/client/T01845XT9A9/C01ADBRGT6Z
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B01B01 All PresentationsB01班のショートプレゼン連結動画・全プレゼンへのリンクです。Short:https://www.dropbox.com/s/i79jg8e1k9ncspl/S_B01_all.mp4?dl=0All:https://www.dropbox.com/sh/qteen5kq5ri6lof/AABQJJZwduvsFuW1ma5Jq7Z6a?dl=0
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B01AraiRyutaJAMSTECヒクランギ沈み込み帯の断層構造・地震波異方性・海山https://www.dropbox.com/s/66y32185uxlzlk1/L_B01_Arai_R.pptx?dl=0#p-b01-araihttps://app.slack.com/client/T01845XT9A9/C01B21ML70R
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B01KitaSaekoBRIEpisodic slow slip, intraslab events and repeatersbeneath Kii peninsula, southwestern Japan紀伊半島でのスラブ内地震，ETS，プレート境界型地震の関係性についての議論を深めました．議論に相似地震のことが加わりました．https://www.dropbox.com/s/3t4u1wmxm1vuinl/S_B01_Kita_Saeko.mp4?dl=0https://www.dropbox.com/s/k7j7lmnlm3q1gcl/L_B01_Kita_Saeko.pdf?dl=0#p-b01-kitahttps://app.slack.com/client/T01845XT9A9/C01APCFCU10
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B01KurashimoEiji東京大学地震研究所Seismic reflection profiling across deep low-frequency tremor zone in western Shikoku, southwestern Japanhttps://www.dropbox.com/s/ea74u91a3sa4vub/S_B01_Kurashimo_Eiji.mp4?dl=0https://www.dropbox.com/s/28gg5yi68tvuf0n/L_B01_Kurashimo_Eiji.mp4?dl=0#p-b01-kurashimohttps://app.slack.com/client/T01845XT9A9/C01AGEEBWN6
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B01MochizukiKimihiroERI, U. TokyoStructural features of the subducting plate and its relation to fluid transfer and fault slip typeshttps://www.dropbox.com/s/qe9i6wi4jrkexif/S_B01_Mochizuki_K.mp4?dl=0https://www.dropbox.com/s/333haii34i5e8i2/L_B01_Mochizuki_K.pptx?dl=0#p-b01-mochizukihttps://app.slack.com/client/T01845XT9A9/C01AGLH3QTV
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B01NakajimaJunichi東工大Spatiotemporal characteristics of low-frequency earthquakes in the continental plate内陸地殻の低周波地震の検出とその時空間変化に関する研究ですhttps://www.dropbox.com/s/63v21y2wkeqiu42/L_B01_Nakajima_Junichi.pdf?dl=0#p-b01-nakajimahttps://app.slack.com/client/T01845XT9A9/C01AGLB94DU
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B01TonegawaTakashiJAMSTECWeak faults at megathrust plate boundary respond to tidal stress掘削船「ちきゅう」の船舶ノイズを使って、南海トラフの分岐断層の潮汐応答を調べました。https://www.dropbox.com/s/2mmhqqrk49cap2u/S_B01_Tonegawa_T_rev1.m4v?dl=0https://www.dropbox.com/s/fon0ep694fbnajq/L_B01_Tonegawa_T_rev1.m4v?dl=0#p-b01-tonegawahttps://app.slack.com/client/T01845XT9A9/C01ACNW86RJ
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B01UyeshimaMakotoEarthquake Research Institute, the University of TokyoOn the Network-MT survey in the western part of Shikoku Island facing the area of the Bungo Channel long-term slow slip event https://www.dropbox.com/s/f5mt9hv8muu9a9o/L_B01_Uyeshima_Makoto.pdf?dl=0#p-b01-uyeshimahttps://app.slack.com/client/T01845XT9A9/C01AZ5Z5YAV
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B02B02 All PresentationsB02班のショートプレゼン連結動画・全プレゼンへのリンクです。Short:https://www.dropbox.com/s/zn40xrv5su6wzl7/S_B02_all.mp4?dl=0All:https://www.dropbox.com/sh/dgwnoeph4q9hz8k/AAC_cWWcwCSJVQw1VsZr4w4Ea?dl=0
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B02HashimotoYoshitakaKochi UniversiryThe effects of decollement geometry on stress, sediments' properties and VLFEs distributionin Nankai Troughslackへのコメントもいただけるとありがたいです。https://www.dropbox.com/s/ehqmh17qspe3tae/S_B02_Hashimoto_Y.mov?dl=0https://www.dropbox.com/s/30qacl0mw9nn35g/L_B02_Hashimoto_Y.mov?dl=0#p-b02-hashimotohttps://app.slack.com/client/T01845XT9A9/C01AED24D6G
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B02HiroseTakehiroKochi/JAMSTECHigh fluid pressure patch beneath the décollement as a potential source of slow earthquakes at the Nankai Trough off Cape Muroto質問はコメントはメール(hiroset@jamstec.go.jp)もしくはSlackにお願いします。https://www.dropbox.com/s/ga299k5z2pt4gos/S_B02_Hirose_Takehiro.mp4?dl=0https://www.dropbox.com/s/opagkdpnfilihrz/L_B02_Hirose_Takehiro.pdf?dl=0#p-b02-hirose-takehirohttps://app.slack.com/client/T01845XT9A9/C01B69NJ3A4
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B02NishiyamaNaokiUniversity of TsukubaSpatial change in inclusion band spacing as an indicator of temporal change in slow earthquake recurrence intervals質問、コメントはSlack、またはzoomからお願いします。https://www.dropbox.com/s/aq84psmrn8xc6fb/S_B02_Nishiyama_Naoki.mp4?dl=0https://www.dropbox.com/s/jxln6qhcximtuye/L_B02_Nishiyama_Naoki.mp4?dl=0#p-b02-nishiyamahttps://app.slack.com/client/T01845XT9A9/C01AED358F6
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B02OkazakiKeishiKCC/JAMSTECRheology of the fluid-rich fault zone under the PT conditions at the source region of deep slow earthquakes「高温高圧下における流体の富む断層のレオロジー」。質問・コメントについてはSlackもしくはメール（okazakik@jamstec.go.jp）にてお願いします。https://www.dropbox.com/s/hchnyu8yexkua3p/S_B02_Okazaki_Keishi.mp4?dl=0https://www.dropbox.com/s/03lbn5dn70909kn/L_B02_Okazaki_Keishi.pdf?dl=0#p-b02-okazakihttps://app.slack.com/client/T01845XT9A9/C01ANKZBQ76
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B02OtsuboMakotoGeological Survey of Japan Localized fluid discharge by tensile cracking during the post-seismic period in subduction zones南海トラフの陸上アナログの延岡でのextension veinを使って，プレート境界付近での間隙流体圧は地震後も高い状態（λ*=0.8程度）を保持しているという成果です．https://www.dropbox.com/s/igeu3vl3dawoj8p/S_B02_Otsubo_Makoto.mov?dl=0https://www.dropbox.com/s/clk84trq213namt/L_B02_Otsubo_Makoto.pdf?dl=0#p-b02-otsubohttps://app.slack.com/client/T01845XT9A9/C01A6HB8PBL
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B02TakahashiMikiGSJ, AISTSLIP ACCELERATION PRIOR TO DYNAMIC WEAKENING質問･コメントはメール（miki.takahashi@aist.go.jp）もしくはSlackにてお願いします。https://www.dropbox.com/s/rh9yvdcdmdiiwsa/S_B02_Miki_Takahashi.pdf?dl=0https://www.dropbox.com/s/nlj7n4lmxeym0xn/L_B02_Miki_Takahashi.pdf?dl=0#p-b02-takahashi-mikihttps://app.slack.com/client/T01845XT9A9/C01B21LC54Z
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B02TanikawaWataru海洋研究開発機構Slip velocity dependence of permeability and friction, explained by thermal pressurization due to frictional heating質問･コメントはメール（tanikawa@jamstec.go.jp）もしくはSlackにてお願いします。https://www.dropbox.com/s/0u5igsxanbvhozz/S_B02_Tanikawa_Wataru.mp4?dl=0https://www.dropbox.com/s/31dfcre6ek2d74f/L_B02_Tanikawa_Wataru.mp4?dl=0#p-b02-tanikawahttps://app.slack.com/client/T01845XT9A9/C01ANL24S4C
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B02TsutsumiAkito京都大学大学院理学研究科Effect of pore-fluid pressure on the frictional velocity dependence of plate-boundary fault materials質問・コメントについてはSlackもしくはメール（tsutsumi@kueps.kyoto-u.ac.jp)までお願いします。https://www.dropbox.com/s/tedbjgw7vbzuqqr/S_B02_Tsutsumi_Akito.mp4?dl=0https://www.dropbox.com/s/s2yb725m0ytlpk4/L_B02_Tsutsumi_Akito.mp4?dl=0#p-b02-tsutsumihttps://app.slack.com/client/T01845XT9A9/C019Z0B5WUF
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B02UjiieKohtaroUniversity of TsukubaGeological conditions of ETS zonehttps://www.dropbox.com/s/fh2lzpxr833bcy1/S_B02_Ujiie_Kohtaro.mp4?dl=0https://www.dropbox.com/s/lowypr0dve68175/L_B02_Ujiie_Kohtaro.mp4?dl=0#p-b02-ujiiehttps://app.slack.com/client/T01845XT9A9/C01ADBR7761
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B02YamaguchiAsuka東京大学大気海洋研究所熊野沖前縁衝上断層帯の発達過程https://www.dropbox.com/s/5hxyx15r5lsina2/S_B02_Yamaguchi_Asuka.mp4?dl=0https://www.dropbox.com/s/q6ncprw1yc1ow11/L_B02_Yamaguchi_Asuka.mp4?dl=0#p-b02-yamaguchi-asukahttps://app.slack.com/client/T01845XT9A9/C01AGLDJ26S
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C01C01 All PresentationsC01班のショートプレゼン連結動画・全プレゼンへのリンクです。Short:https://www.dropbox.com/s/bq0eno0kwlfzuty/S_C01_all.mp4?dl=0All:https://www.dropbox.com/sh/0c21b75s0pljeva/AAA6bRDW-Nv1ph8Z4xKyOFwTa?dl=0
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C01AgataRyoichiroJAMSTECRevisiting the slip distribution of the long-term slow slip events in the Bungo Channel: up and downdip limit of the distribution https://www.dropbox.com/s/rp7ot5iaoqsptjy/L_C01_Agata_Ryoichiro.pdf?dl=0#p-c01-agatahttps://app.slack.com/client/T01845XT9A9/C01APMFR4FM
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C01AndoRyosuke東京大学理学系研究科地球惑星科学専攻脆性パッチサイズと粘性に温度依存性を考慮したモデルでスロー地震の普遍的な深さ依存性を再現https://www.dropbox.com/s/t9lqrjlewhjyvvd/S_C01_Ando_ryo.pptx?dl=0←9/17追加#p-c01-andohttps://app.slack.com/client/T01845XT9A9/C01AV4088BC
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C01ChangTa-Wei東京大学理学系研究科地球惑星科学専攻Joint Relocation of Centroid and Hypocenter via Cross-Correlation Approachstudent相互相関関数による震源とセントロイドの再決定手法を開発しましたhttps://www.dropbox.com/s/atiy39d5e9qskw3/S_C01_Chang_Tawei.mov?dl=0https://www.dropbox.com/s/yelwvbfmtua8enx/L_C01_Chang_Tawei.mov?dl=0#p-c01-changhttps://app.slack.com/client/T01845XT9A9/C01ADBQFLDT
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C01HoriTakaneJAMSTECA concept of regular & slow earthquake modelhttps://www.dropbox.com/s/4vfs7skbjs6c7wj/L_C01_Hori_Takane.pdf?dl=0#p-c01-horihttps://app.slack.com/client/T01845XT9A9/C01AGLE2D4N
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C01IdeSatoshiDept. EPS, Univ. TokyoWhat can we observe with DAS? 2020 Jan. JAMSTEC Muroto submarine cable experimentモデル班の趣旨とずれますが、JAMSTECのDASのデータをいろいろいじってみました。slackは見ていますhttps://www.dropbox.com/s/7xt49z0nskb92qw/S_C01_Ide_Satoshi.mp4?dl=0https://www.dropbox.com/s/gg558ra8tr50lgb/L_C01_Ide_Satoshi.mp4?dl=0#p-c01-idehttps://app.slack.com/client/T01845XT9A9/C01A9NB5HD4
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C01MitsuiYutaShizuoka UniversityOmori‑like decay of postseismic velocities from early stages of the post-Tohoku EQ: Was it truly caused by ‘afterslip’ ?Slack、もしくは、メール(mit@shizuoka.ac.jp)でお願いします。https://www.dropbox.com/s/n73b6fesoaxivpe/S_C01_Mitsui_Y.mp4?dl=0https://www.dropbox.com/s/19qqcx2007baddd/L_C01_Mitsui_Y.mp4?dl=0#p-c01-mitsuihttps://app.slack.com/client/T01845XT9A9/C019ZR7UG6A
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C01NakanoMasaruJAMSTECTemporal changes of event size distribution of shallow tectonic tremorspatial chatに左記時間帯参加予定。
slackは随時		https://www.dropbox.com/s/9n1d8u9yyj4y51u/S_C01_Nakano_Masaru.mp4?dl=0https://www.dropbox.com/s/w1x4l5w4hci6837/L_C01_Nakano_Masaru.mp4?dl=0#p-c01-nakanohttps://app.slack.com/client/T01845XT9A9/C01AED2RRGU
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C01OikawaGenki東京工業大学理学院地球惑星科学系巨大地震による応力変化が火山深部低周波地震の活動に与える影響studenthttps://www.dropbox.com/s/efvupguk44bp0h1/S_C01_Oikawa_Genki.mp4?dl=0https://www.dropbox.com/s/56kw0rlmdgv08a0/L_C01_Oikawa_Genki.mp4?dl=0#p-c01-oikawahttps://app.slack.com/client/T01845XT9A9/C01ASB38RA5
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C01ShibataRitsuya東京工業大学Quantitative comparison between the radiation-corrected EGF and the conventional EGFstudentSlackは随時返信させていただきます。https://www.dropbox.com/s/p3pdx5kct35h2ci/S_C01_Shibata_Ritsuya.mp4?dl=0https://www.dropbox.com/s/gz21rip5d6xwvfk/L_C01_Shibata_Ritsuya.pdf?dl=0#p-c01-shibatahttps://app.slack.com/client/T01845XT9A9/C01A1MXMN31
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C01TohAkiko東京大学Influence of a subducted oceanic ridge on the distribution of shallow VLFEs in the Nankai Trough as revealed by moment tensor inversion and cluster analysishttps://www.dropbox.com/s/xdb6yldc2kdhigc/S_C01_Toh_A.pdf?dl=0https://www.dropbox.com/s/4hg0shq9d0l6s17/L_C01_Toh_A_rev2.pdf?dl=0#p-c01-tohhttps://app.slack.com/client/T01845XT9A9/C01APJJBS3V
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C01YabeSuguruGSJ, AISTSeismic energy radiation by shallow tectonic tremors & its along-strike heterogeneities at the Nankai trough and the Japan trench質問などはSlackにお願いします．https://www.dropbox.com/s/k73xxm1q8xadn8o/S_C01_Yabe_Suguru.m4v?dl=0https://www.dropbox.com/s/vtqhsnkgncx4ga0/L_C01_Yabe_Suguru.m4v?dl=0#p-c01-yabehttps://app.slack.com/client/T01845XT9A9/C01A6PFCH7D
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C01YamashitaFutoshiNIEDForeshock activities controlled by slip rate on a 4-meter-long laboratory faulthttps://www.dropbox.com/s/c1l4iiel96qka6t/S_C01_Yamashita_Futoshi.mp4?dl=0https://www.dropbox.com/s/bdozx43rx3aa9n2/L_C01_Yamashita_Futoshi.mp4?dl=0#p-c01-yamashita-futoshihttps://app.slack.com/client/T01845XT9A9/C01ADBP6A77
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C02C02 All PresentationsC02班のショートプレゼン連結動画・全プレゼンへのリンクです。Short:https://www.dropbox.com/s/8bfu5dxmd70j2uf/S_C02_all.mp4?dl=0All:https://www.dropbox.com/sh/eaf5ned14nlhmx9/AABcQ6Wu7NrfOoBwAioIl2ZHa?dl=0
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C02FukudaKota東京大学地震研究所Model for tectonic tremor, enduring events, moment rate spectrum, moment - duration scaling.studenthttps://www.dropbox.com/s/2re89kr9w7wyj0a/S_C02_Fukuda_Kota.mp4?dl=0https://www.dropbox.com/s/vbfbw7qlsslzhrx/L_C02_Fukuda_Kota.mp4?dl=0#p-c02-fukudahttps://app.slack.com/client/T01845XT9A9/C01ADBPEK37
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C02HatanoTakahiro大阪大学すべり速度と水圧の動的相互作用によるSSEのモデルhttps://www.dropbox.com/s/d32g83lrm0a0lhk/S_C02_Hatano_Takahiro.mp4?dl=0https://www.dropbox.com/s/dworxpevkgohhgk/L_C02_Hatano_Takahiro.pdf?dl=0#p-c02-hatanohttps://app.slack.com/client/T01845XT9A9/C019Z09UXKR
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C02KatsuragiHiroakiOsaka UniversityPeriodic weakening vs abrupt slip in a compressed granular bed -The effect of hierarchical structure-https://www.dropbox.com/s/371v2ztr6f8gf2j/S_C02_Katsuragi_Hiroaki.m4v?dl=0https://www.dropbox.com/s/or2ecwzbopqqj5k/L_C02_Katsuragi_Hiroaki.m4v?dl=0#p-c02-katsuragihttps://app.slack.com/client/T01845XT9A9/C01ADU5LP4K
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C02KunduSumantaDepartment of Earth and Space Science, Osaka University, Osaka, JapanCorrelations in earthquake time series as revealed by the visibility graphMeeting ID: 712 403 8554
Passcode: Kundu		https://www.dropbox.com/s/h9t47a5hs4eonz5/S_C02_Kundu_Sumanta.mov?dl=0https://www.dropbox.com/s/y33ziksu1no94x6/L_C02_Kundu_Sumanta.mov?dl=0#p-c02-kunduhttps://app.slack.com/client/T01845XT9A9/C01A1MY9C31
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C02OprisAncaOsaka UniversityImaging the spatio-temporal correlations in tremor activityMeeting ID: 939 036 6333 Passcode: 862385https://www.dropbox.com/s/mzlurgeyuzn2zog/S_C02_Opris_Anca.pdf?dl=0https://www.dropbox.com/s/bxyxap2yd5u0m7x/L_C02_Opris_Anca.mov?dl=0#p-c02-oprishttps://app.slack.com/client/T01845XT9A9/C01ADBSV2J1
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C02SuminoYutakaTokyo University of ScienceSearch for Slow Earthquakeas the Benjamin-Feir instabilityI try to connect zoom in this period, but I would be happy if you could notify me thorugh slackhttps://www.dropbox.com/s/x1ikf66fucw326f/S_C02_Sumino_Yutaka.mp4?dl=0https://www.dropbox.com/s/wmscw834neuypu9/L_C02_Sumino_Yutaka.mp4?dl=0#p-c02-suminohttps://app.slack.com/client/T01845XT9A9/C01AAKDRVBP
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C02SuzukiTakehito青学大理工Systematic understanding of slip-front-propagation velocity with the slip-velocity-dependent friction lawhttps://www.dropbox.com/s/bq9egu7qx5ker02/S_C02_Suzuki_Takehito.mp4?dl=0https://www.dropbox.com/s/26ynb4p81u0fv9a/L_C02_Suzuki_Takehito.mp4?dl=0#p-c02-suzukihttps://app.slack.com/client/T01845XT9A9/C01ACNVV9RA
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C02YamaguchiTetsuoDepartment of Biomaterial Sciences, The University of TokyoOscillatory slip nucleation in laboratory earthquake experimentshttps://www.dropbox.com/s/b2sjg17v49538rc/S_C02_Yamaguchi_Tetsuo.mp4?dl=0https://www.dropbox.com/s/pm1ne95xvnlm4zq/L_C02_Yamaguchi_Tetsuo.mp4?dl=0#p-c02-yamaguchi-tetsuohttps://app.slack.com/client/T01845XT9A9/C019Z0BR20P