研究者詳細

顔写真

タン　チ－シエン
Tang Chi-Hsien
Tang Chi-Hsien
所属
災害科学国際研究所　災害評価・低減研究部門　海域地震学研究分野
職名
助教
学位

  • Ｐｈ．Ｄ．（National Taiwan University）

  • Ｍ．Ｓ．（National Central University）

e-Rad 研究者番号
50996676

経歴 3

  • 2024年4月 ～ 継続中
    東北大学　大学院理学研究科 附属地震・噴火予知研究観測センター　兼任助教

  • 2024年1月 ～ 継続中
    東北大学　災害科学国際研究所　助教

  • 2021年8月 ～ 2023年12月
    中央研究院　地球科学研究所　ポストドクトラル研究員

学歴 3

  • 国立台湾大学　地質科学研究所

    2017年9月 ～ 2021年6月

  • 国立中央大学　地球物理研究所

    2014年9月 ～ 2016年1月

  • 国立中央大学　地球科学学系

    2010年9月 ～ 2014年6月

研究分野 1

  • 自然科学一般 / 固体地球科学 / 地殻変動

受賞 9

  1. Kamide Lecture Award

    2025年7月　Asia Oceania Geosciences Society

  2. Postdoctoral Researcher Academic Award

    2023年　National Science and Technology Council (Taiwan)

  3. Vei Chow Juan Best Ph.D. Thesis Award

    2022年　Geological Society located in Taipei

  4. Postdoctoral Scholar Program

    2022年　Academia Sinica

  5. Honorary membership

    2021年　The Phi Tau Phi Scholastic Honor Society of the Republic of China

  6. Dean’s Award of College of Science

    2021年　National Taiwan University

  7. Yi-Ben Tsai Graduate Student Scholarship

    2020年　Chinese Taipei Geophysical Society

  8. Graduate Student Study Abroad Program

    2019年　Ministry of Science and Technology (Taiwan)

  9. Dean’s Award of College of Earth Science

    2014年　National Central University

︎全件表示 ︎最初の5件までを表示

論文 14

  1. Geodetic Evidence of Shallow Slow‐Slip Phenomena Beneath the Southern Ryukyu Forearc

    Chi‐Hsien Tang, Ya‐Ju Hsu, Yutaro Okada, Yusaku Ohta, Takeshi Sagiya, Pei‐Ru Jian, Yoshiaki Tamura, Takaaki Jike

    Geophysical Research Letters　52　(13)　e2025GL114742　2025年7月8日

    出版者・発行元： American Geophysical Union (AGU)

    DOI： 10.1029/2025gl114742 　

    ISSN：0094-8276

    eISSN：1944-8007

    詳細を見る 詳細を閉じる

    Abstract While slow slip events (SSEs) are recognized as a ubiquitous phenomenon in subduction zones, accurately tracking the spatiotemporal distribution of shallow SSEs remains challenging. Here, we investigate the potential occurrence of shallow SSEs in the southern Ryukyu forearc at the western boundary of the Philippine Sea plate using 25 years of Global Navigation Satellite System data. We identify trenchward transient motions near the Miyako Islands, with cumulative displacements of ∼10 mm between 2009 and 2011, indicating shallow SSEs that released a geodetic moment equivalent to Mw 6.8. These SSEs likely occurred updip of a Mw 6.1 interplate earthquake, whose associated positive Coulomb stress changes may have encouraged slow slip. Our results indicate that the shallow southern Ryukyu plate interface can accumulate elastic strain and release energy either aseismically or seismically. We therefore emphasize the importance of near‐trench seafloor geodesy to fully characterize fault slip behaviors beneath the southern Ryukyu forearc.

  2. Earthquake disaster resilience in Taiwan observed from the April 2024 ML 7.1 Hualien earthquake

    Ryuta Enokida, Yo Fukushima, Chi-Hsien Tang, Tsung-Yi Pan, Chun-Lin Kuo, Kohju Ikago, Takako Izumi, Shinichi Kuriyama

    Frontiers in Built Environment　11　1593942　2025年7月7日

    出版者・発行元： Frontiers Media SA

    DOI： 10.3389/fbuil.2025.1593942 　

    ISSN：2297-3362

    eISSN：2297-3362

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    This study investigated Taiwan’s earthquake disaster resilience and remaining challenges after the Hualien earthquake, which occurred at 07:58 a.m. local time (UTC+8) on 3 April 2024. Through a survey, we found possible factors for the relatively suppressed damage caused by this earthquake. The 2024 Hualien earthquake (ML: 7.1) was not as severe as the 2018 earthquake (ML: 6.2) in terms of the maximum velocity of ground motion, which greatly affected the structural damage, owing to the different mechanisms of the earthquakes. Earthquake-resistant measures in Taiwan have high standards, such as building codes and seismic monitoring networks. At the 2024 earthquake, early warning systems and data-sharing networks for seismic records were useful for prompting immediate evacuation. Based on rapidly shared information and predesigned frameworks, disaster response operations quickly made evacuations, rescues, and other decisions. In addition to these government actions, support from non-government organizations (NGOs) has greatly contributed to evacuation, shelter management, and evacuee care in severely affected areas. The timing of this earthquake positively acted to limit the impact on Taroko National Park, as it was not the peak time for visitors, although the park still had the majority of casualties caused by landslides. These lessons can be possibly reflected in earthquake disaster resilience in other countries.

  3. Multi-fault segment complexity and multi-rupture episodes during the 2024 Mw 7.5 Noto Peninsula earthquake

    Rintaro Enomoto, Yoshihiro Kaneko, Chi-Hsien Tang, Yo Fukushima, Hiroyuki Goto, Shin’ichi Miyazaki

    Earth, Planets and Space　77　(1)　83　2025年6月6日

    出版者・発行元： Springer Science and Business Media LLC

    DOI： 10.1186/s40623-025-02213-w 　

    eISSN：1880-5981

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    Abstract Major intraplate earthquakes pose a substantial threat to nearby inhabited regions, but their rupture characteristics are often unclear due to limited observations. The 2024 Mw 7.5 Noto Peninsula earthquake in Japan, recorded by numerous near-fault strong-motion seismometers, high-rate GNSS, and satellite data, presents a unique opportunity to investigate fault rupture evolution and the resulting strong ground motions in detail. Using kinematic rupture modeling, we developed a source model that reproduces SAR-based and GNSS data, as well as near-fault velocity and displacement waveforms with periods longer than 4 s. Our approach integrates 3D velocity and inelastic attenuation models for Japan, incorporating regional topography and bathymetry. To reduce the number of unknown parameters, we used an a priori fault slip model derived from SAR and GNSS data and fixed the fault geometry and final slip distribution, adjusting only the rupture timing and rise time of individual fault segments. The preferred source model reveals multiple slip episodes and intricate rupture evolution, including a backward-propagating rupture toward the mainshock hypocenter likely triggered by abrupt changes in local fault geometry. The mainshock hypocenter and subsequent rupture initiations occur in areas of increased shear stresses along the periphery of the preceding swarm activity. These subsequent ruptures propagated bilaterally along southwestern and northeastern fault segments with rupture speeds ranging from 1.4 to 2.1 km/s, slower than those of other intraplate thrust earthquakes of similar magnitude. The southwestward rupture broke large slip asperities (up to $$\sim 10$$ m) on non-planar fault segments offshore Monzen, where the coseismic uplift was $$\sim 4$$ m. Our results suggest that the 2024 Noto Peninsula earthquake is a remarkable example of a complex intraplate earthquake involving multi-segment rupture with multiple slip episodes, providing important insights into the physics of rupture propagation and the resulting ground motions. Graphical Abstract

  4. Hydrologically-induced crustal stress changes and their association with seismicity rates in Taiwan

    Ya-Ju Hsu, Roland Bürgmann, Zhongshan Jiang, Chi-Hsien Tang, Christopher W. Johnson, Da-Yi Chen, Hsin-Hua Huang, Miao Tang, Xinghai Yang

    Earth and Planetary Science Letters　651　119181　2025年2月1日

    出版者・発行元： Elsevier BV

    DOI： 10.1016/j.epsl.2024.119181 　

    ISSN：0012-821X

  5. Geodetic constraints on the September 2022 Guanshan and Chihshang earthquakes, eastern Taiwan

    Hsin Tung, Horng-Yue Chen, Ya-Ju Hsu, Chi-Hsien Tang, Jian-Cheng Lee, Yu Wang, Hung Kyu Lee

    Tectonophysics　895　230600　2025年1月24日

    出版者・発行元： Elsevier BV

    DOI： 10.1016/j.tecto.2024.230600 　

    ISSN：0040-1951

  6. Landscape changes caused by the 2024 Noto Peninsula earthquake in Japan

    Yo Fukushima, Daisuke Ishimura, Naoya Takahashi, Yoshiya Iwasa, Luca C. Malatesta, Takayuki Takahashi, Chi-Hsien Tang, Keisuke Yoshida, Shinji Toda

    Science Advances　10　(49)　eadp9193　2024年12月6日

    出版者・発行元： American Association for the Advancement of Science (AAAS)

    DOI： 10.1126/sciadv.adp9193 　

    eISSN：2375-2548

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    Landscapes are shaped by tectonic, climatic, and surface processes over geological timescales, but we rarely witness the events of marked landscape change. The moment magnitude 7.5 Noto Peninsula earthquake in central Japan was caused by a large thrust faulting, up to nearly 10 meters of slip, that expanded more than 150 kilometers along the fault zone. The deformation field reconstructed from satellite data and field surveys reveals up to 4.4 meters of uplift and associated coastal advance along the entire northern coast of the peninsula, meter-scale systematic movement of the mountain slopes consistent with slip on flexural faults, and activation of secondary inland faults, suggesting synchronized ruptures. The findings show excellent consistency between the coseismic deformation and geomorphic features and provide a vivid example of the role of a major earthquake in landscape formation.

  7. Nearby fault interaction within the double-vergence suture in eastern Taiwan during the 2022 Chihshang earthquake sequence

    Chi-Hsien Tang, Yunung Nina Lin, Hsin Tung, Yu Wang, Shiann-Jong Lee, Ya-Ju Hsu, J. Bruce H. Shyu, Yu-Ting Kuo, Horng-Yue Chen

    Communications Earth & Environment　4　(1)　333　2023年9月21日

    出版者・発行元： Springer Science and Business Media LLC

    DOI： 10.1038/s43247-023-00994-0 　

    eISSN：2662-4435

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    Abstract Nearby faults interact through stress changes induced by fault slip and viscoelastic flow. The process is, however, often elusive and can be geometry-dependent and time-variant. Here, we combine geodetic and field observations to characterize the interaction of two head-to-head, conjugate faults in eastern Taiwan during the 2022 Chihshang earthquake sequence. We map the coseismic slip on the Central Range fault and dynamically-triggered shallow slip on the Longitudinal Valley fault, which has been creeping interseismically. Overlapping of seismic and aseismic slip suggests that the Longitudinal Valley fault is capable of hosting a variety of distinct slip behaviors. Moreover, substantial slip on the Central Range fault suppresses Coulomb stress on the Longitudinal Valley fault, and vice versa, resulting in seismic bursts in an out-of-phase pattern on the two faults as seen in the hundred-year historical records. Such fault interaction implies the need for time-dependent seismic hazard reassessment for the complex fault system.

  8. Oblique Blind Faulting Underneath the Luzon Volcanic Arc During the 2022 Mw 7.0 Abra Earthquake, the Philippines

    Chi‐Hsien Tang, Ya‐Ju Hsu, Teresito Bacolcol, Yunung Nina Lin, Horng‐Yue Chen, Yu‐Ting Kuo, Hsuan‐Han Su, Hsin‐Ming Lee, Alfie Pelicano, Genesis Sapla, Shui‐Beih Yu

    Geophysical Research Letters　50　(9)　e2023GL103659　2023年5月8日

    出版者・発行元： American Geophysical Union (AGU)

    DOI： 10.1029/2023gl103659 　

    ISSN：0094-8276

    eISSN：1944-8007

    詳細を見る 詳細を閉じる

    Abstract Unknown seismogenic structures lurking beneath convergent margins introduce substantial uncertainty in seismic hazard assessments. In northwestern Luzon, the Mw 7.0 Abra earthquake on 27 July 2022 highlights the seismic activity along an unmapped blind fault underneath the Cordillera Central. By integrating coseismic displacements constrained by radar satellite imagery and Global Navigation Satellite System, we image oblique coseismic slip at 11–22 km depth with peak slip of ∼1 m beneath the Philippine Fault Zone in northern Luzon. The southward propagation of coseismic slip and aftershocks terminated at a distance of 50 km from the northern end of the 1990 Luzon earthquake rupture, leaving a seismicity gap in between. Coulomb stress changes of reaching 2 bars are imparted at the shallow portions of the Vigan‐Aggao and Abra River faults, where the updated 100‐year seismic potential is increased to Mw 7.0–7.7, given the thick seismogenic layer of ∼30 km in northern Luzon.

  9. Strain Partitioning in the Southern Ryukyu Margin Revealed by Seafloor Geodetic and Seismological Observations

    Horng‐Yue Chen, Ya‐Ju Hsu, Ryoya Ikuta, Hsin Tung, Chi‐Hsien Tang, Chin‐Shang Ku, Hsuan‐Han Su, Pei‐Ru Jian, Masataka Ando, Toshiaki Tsujii

    Geophysical Research Letters　49　(6)　e2022GL098218　2022年3月22日

    出版者・発行元： American Geophysical Union (AGU)

    DOI： 10.1029/2022gl098218 　

    ISSN：0094-8276

    eISSN：1944-8007

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    Abstract The southern Ryukyu subduction zone is one of the potential sources for tsunamigenic earthquakes. Despite a great seismic risk, the deformation pattern remains poorly known, primarily due to the absence of seafloor constraints. With GNSS‐acoustic measurements over years, we characterize the convergence rate across this margin growing from 92 mm/yr offshore eastern Taiwan to 123 mm/yr near the Gagua Ridge. The new data suggest the subduction interface is capable of hosting Mw 7.5–8.4 earthquakes. The orientations of seafloor movement and P‐axes in the Nanao Basin are both subnormal to the trench, notably deviate from the direction of plate convergence. By considering the combined effect of plate convergence and backarc rifting, different trends between the forearc convergence, P‐axes, and seafloor movement may indicate some degree of slip‐partitioning. The trench‐parallel component is likely accommodated in part by earthquakes near Taiwan, lower plate deformation, and strike‐slip faults within the accretionary wedge.

  10. Assessing seasonal and interannual water storage variations in Taiwan using geodetic and hydrological data

    Ya-Ju Hsu, Yuning Fu, Roland Bürgmann, Shao-Yiu Hsu, Chin-Cheng Lin, Chi-Hsien Tang, Yih-Min Wu

    Earth and Planetary Science Letters　550　116532　2020年11月15日

    出版者・発行元： Elsevier BV

    DOI： 10.1016/j.epsl.2020.116532 　

    ISSN：0012-821X

  11. Heterogeneous Power‐Law Flow With Transient Creep in Southern California Following the 2010 El Mayor‐Cucapah Earthquake

    Chi‐Hsien Tang, Sylvain Barbot, Ya‐Ju Hsu, Yih‐Min Wu

    Journal of Geophysical Research: Solid Earth　125　(9)　e2020JB019740　2020年8月26日

    出版者・発行元： American Geophysical Union (AGU)

    DOI： 10.1029/2020jb019740 　

    ISSN：2169-9313

    eISSN：2169-9356

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    Abstract The rheology of the crust and mantle and the interaction of viscoelastic flow with seismic/aseismic slip on faults control the state of stress in the lithosphere over multiple seismic cycles. The rheological behavior of rocks is well constrained in a laboratory setting, but the in situ properties of the lithosphere and its lateral variations remain poorly known. Here, we access the lower‐crustal rheology in Southern California by exploiting 8 years of geodetic postseismic deformation following the 2010 El Mayor‐Cucapah earthquake. The data illuminate viscoelastic flow in the lower crust with lateral variations of effective viscosity correlated with the geological province. We show that a Burgers assembly with dashpots following a nonlinear constitutive law can approximate the temporal evolution of stress and strain rate, indicating the activation of nonlinear transient creep before steady‐state dislocation creep. The transient and background viscosities in the lower crust of the Salton Trough are on the order of ~1018 and ~1019 Pa s, respectively, about an order of magnitude lower than those in the surrounding regions. We highlight the importance of transient creep, nonlinear flow laws, and lateral variations of rheological properties to capture the entire history of postseismic relaxation following the El Mayor‐Cucapah earthquake.

  12. Lower-crustal rheology and thermal gradient in the Taiwan orogenic belt illuminated by the 1999 Chi-Chi earthquake

    Chi-Hsien Tang, Ya-Ju Hsu, Sylvain Barbot, James D. P. Moore, Wu-Lung Chang

    Science Advances　5　(2)　eaav3287　2019年2月27日

    出版者・発行元： American Association for the Advancement of Science (AAAS)

    DOI： 10.1126/sciadv.aav3287 　

    eISSN：2375-2548

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    Rapid shortening reveals transient creep and the temperature conditions of dislocation creep in the Taiwan lower crust.

  13. Detecting rock uplift across southern Taiwan mountain belt by integrated GPS and leveling data

    Ya-Ju Hsu, Yen-Ru Lai, Rey-Jer You, Horng-Yue Chen, Louis S. Teng, Yi-Chuen Tsai, Chi-Hsien Tang, Hsuan-Han Su

    Tectonophysics　744　275-284　2018年10月2日

    出版者・発行元： Elsevier BV

    DOI： 10.1016/j.tecto.2018.07.012 　

    ISSN：0040-1951

  14. Imaging the distribution of transient viscosity after the 2016 M w 7.1 Kumamoto earthquake

    James D. P. Moore, Hang Yu, Chi-Hsien Tang, Teng Wang, Sylvain Barbot, Dongju Peng, Sagar Masuti, Justin Dauwels, Ya-Ju Hsu, Valère Lambert, Priyamvada Nanjundiah, Shengji Wei, Eric Lindsey, Lujia Feng, Bunichiro Shibazaki

    Science　356　(6334)　163-167　2017年4月14日

    出版者・発行元： American Association for the Advancement of Science (AAAS)

    DOI： 10.1126/science.aal3422 　

    ISSN：0036-8075

    eISSN：1095-9203

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    Crustal rock strength from outer space The response of crustal rock to stresses is challenging to estimate yet vital for determining risks from events such as earthquakes. Moore et al. take advantage of the recent M w 7.1 Kumamoto earthquake in Japan to determine the rheology of crustal rocks in the region. The observed inversion of the crustal strain rates demonstrates that certain areas have stiff rock and others (e.g., under the Aso volcanic complex) have much weaker rock. The results match up with expectations, which means that the method can successfully measure rock properties over a wide range of strength and large spatial and temporal scales. Science , this issue p. 163

︎全件表示 ︎最初の5件までを表示

講演・口頭発表等 19

  1. Lateral extent of coseismic slip and limited near-trench rupture during the 2025 Mw 8.7-8.8 Kamchatka earthquake from geodetic and tsunami data 招待有り

    Chi-Hsien Tang

    NIED seminar　2026年1月9日

  2. Unraveling the Complex Rupture Processes of the 2024 Noto Peninsula Earthquake through 3D Wavefield Simulations and MCMC Inversion

    Rintaro Enomoto, Yoshihiro Kaneko, Chi-Hsien Tang, Yo Fukushima, Hiroyuki Goto, Shin'ichi Miyazaki

    AGU Fall Meeting　2025年12月16日

  3. Aseismic slip phenomenon in the southern Ryukyu forearc illuminated by geodetic observations 招待有り

    Chi-Hsien Tang

    IES Seminar　2025年9月25日

  4. Characterizing earthquakes and aseismic slip in the western margin of the Philippine Sea plate 招待有り

    Chi-Hsien Tang

    AOGS Annual Meeting　2025年7月29日

  5. Initiation of GNSS-Acoustic seafloor geodetic observation along the Japan trench off Boso

    Fumiaki Tomita, Motoyuki Kido, Kazuo Nakahigashi, Yusaku Ohta, Kanata Endo, Chi-Hsien Tang, Ryota Hino

    JpGU Meeting　2025年5月28日

  6. Geodetic and seismic insights into seismogenic features and fault segmentation along the southern Ryukyu Trench 招待有り

    Ya-Ju Hsu, Pei-Ru Jian, Chi-Hsien Tang

    JpGU Meeting　2025年5月25日

  7. Multi-Fault Segment Complexity and Multi-Rupture Episodes during the 2024 Mw 7.5 Noto Peninsula Earthquake

    Rintaro Enomoto, Yoshihiro Kaneko, Chi-Hsien Tang, Yo Fukushima, Hiroyuki Goto, Shin'ichi Miyazaki

    JpGU Meeting　2025年5月30日

  8. Geodetic constraints on the September 2022 Guanshan and Chihshang earthquakes, eastern Taiwan

    Hsin Tung, Horng-Yue Chen, Ya-Ju Hsu, Chi-Hsien Tang, Jian-Cheng Lee, Yu Wang

    JpGU Meeting　2025年5月28日

  9. A long-term slow slip event beneath the southern Ryukyu forearc revealed by 25 years of GNSS observations 招待有り

    Chi-Hsien Tang, Ya-Ju Hsu, Yutaro Okada, Yusaku Ohta, Takeshi Sagiya, Pei-Ru Jian, Yoshiaki Tamura, Takaaki Jike

    JpGU Meeting　2025年5月28日

  10. Stress transfer cycle from slow to fast earthquakes across the southernmost Ryukyu subduction thrust during deep slow slip

    Sean Kuanhsiang Chen, Chi-Hsien Tang, Wei Peng, Kate Huihusan Chen, Yun-Tsai Lai, J. Bruce H. Shyu, Yih-Min Wu

    EGU General Assembly　2025年4月28日

  11. Unraveling crustal deformation and seismogenic signatures in eastern Taiwan

    Ya-Ju Hsu, Hsin Tung, Horng-Yue Chen, Yu Wang, Yunung Lin, Chi-Hsien Tang

    EGU General Assembly　2025年5月2日

  12. Landscape Changes Associated with the 2024 Noto Peninsula Earthquake, Japan, Revealed Through Integration of Geodetic and Geomorphological Approaches 招待有り

    Yo Fukushima, Daisuke Ishimura, Naoya Takahashi, Yoshiya Iwasa, Luca Claude Malatesta, Takayuki Takahashi, Chi-Hsien Tang, Keisuke Yoshida, Shinji Toda

    AGU Fall Meeting　2024年12月13日

  13. Unraveling the Rupture Source of the 2024 M7.2 Hualien Earthquake Using Geodetic Data

    Hsin Tung, Ya-Ju Hsu, Horng-Yue Chen, Yu-Nung Nina Lin, Yu Wang, Chi-Hsien Tang

    AGU Fall Meeting　2024年12月11日

  14. Kinematic Rupture Modeling Unveils Multi-Fault Segments and Multi-Rupture Episodes during the 2024 Mw 7.5 Noto Peninsula Earthquake

    Rintaro Enomoto, Yoshihiro Kaneko, Chi-Hsien Tang, Yo Fukushima, Hiroyuki Goto, Shin'ichi Miyazaki

    AGU Fall Meeting　2024年12月12日

  15. A mysterious shallow slow slip event beneath the southern Ryukyu forearc

    Chi-Hsien Tang, Ya-Ju Hsu, Yutaro Okada, Yusaku Ohta, Takeshi Sagiya, Yoshiaki Tamura, Takaaki Jike

    AGU Fall Meeting　2024年12月12日

  16. A mysterious shallow slow slip event beneath the southern Ryukyu forearc

    Chi-Hsien Tang, Ya-Ju Hsu, Yutaro Okada, Yusaku Ohta, Takeshi Sagiya, Yoshiaki Tamura, Takaaki Jike

    日本測地学会第142回講演会　2024年10月30日

  17. Kinematic and dynamic rupture modeling of the 2024 Mw7.5 Noto earthquake

    Yoshihiro Kaneko, Rintaro Enomoto, Yoshito Nozuka, Chi-Hsien Tang, Yo Fukushima, Hiroyuki Goto, Shin'ichi Miyazaki

    JpGU Meeting　2024年5月28日

  18. Landscape changes caused by the 2024 Noto peninsula earthquake and its relation to the long-term landscape evolution

    Naoya Takahashi, Yo Fukushima, Daisuke Ishimura, Yoshiya Iwasa, Luca Claude Malatesta, Takayuki Takahashi, Chi-Hsien Tang, Keisuke Yoshida, Shinji Toda

    JpGU Meeting　2024年5月28日

  19. Extreme coseismic uplift and faulting complexity during the January 1, 2024, Mw 7.5 Noto Peninsula earthquake

    Chi-Hsien Tang, Yo Fukushima, Shinji Toda, Keisuke Yoshida, Naoya Takahashi, Takayuki Takahashi

    JpGU Meeting　2024年5月31日

︎全件表示 ︎最初の5件までを表示

共同研究・競争的資金等の研究課題 2

  1. 東北沖地震前後の日本列島下部における粘弾性流動の比較

    唐 啓賢

    提供機関：Japan Society for the Promotion of Science

    制度名：Grants-in-Aid for Scientific Research

    研究種目：Grant-in-Aid for Early-Career Scientists

    研究機関：Tohoku University

    2025年4月1日 ～ 2028年3月31日

  2. 海洋物理モデルと連携したWave GliderによるGNSS-音響観測の高度化

    木戸 元之, 飯沼 卓史, 有吉 慶介, 富田 史章, 太田 雄策, 唐 啓賢

    提供機関：Japan Society for the Promotion of Science

    制度名：Grants-in-Aid for Scientific Research

    研究種目：Grant-in-Aid for Scientific Research (B)

    研究機関：Tohoku University

    2024年4月1日 ～ 2027年3月31日

担当経験のある科目(授業) 1

  1. 固体地球物理学特殊講義Ⅱ　東北大学