Details of the Researcher

PHOTO

Tang Chi-Hsien
Section
International Research Institute of Disaster Science
Job title
Assistant Professor
e-Rad No.
50996676

Research History 3

  • 2024/04 - Present
    Tohoku University　Graduate School of Science Research Center for Prediction of Earthquakes and Volcanic Eruptions　Adjunct Assistant Professor

  • 2024/01 - Present
    Tohoku University　International Research Institute of Disaster Science　Assistant Professor

  • 2021/08 - 2023/12
    Academia Sinica　Institute of Earth Sciences　Postdoctoral Fellow

Education 3

  • National Taiwan University　Geosciences

    2017/09 - 2021/06

  • National Central University　Geophysics

    2014/09 - 2016/01

  • National Central University　Earth Sciences

    2010/09 - 2014/06

Research Areas 1

  • Natural sciences / Solid earth science / Crustal Deformation

Awards 9

  1. Kamide Lecture Award

    2025/07　Asia Oceania Geosciences Society

  2. Postdoctoral Researcher Academic Award

    2023　National Science and Technology Council (Taiwan)

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

    2022　Geological Society located in Taipei

  4. Postdoctoral Scholar Program

    2022　Academia Sinica

  5. Honorary membership

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

  6. Dean’s Award of College of Science

    2021　National Taiwan University

  7. Yi-Ben Tsai Graduate Student Scholarship

    2020　Chinese Taipei Geophysical Society

  8. Graduate Student Study Abroad Program

    2019　Ministry of Science and Technology (Taiwan)

  9. Dean’s Award of College of Earth Science

    2014　National Central University

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Papers 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　2025/07/08

    Publisher: American Geophysical Union (AGU)

    DOI： 10.1029/2025gl114742 　

    ISSN： 0094-8276

    eISSN： 1944-8007

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    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　2025/07/07

    Publisher: 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　2025/06/06

    Publisher: 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　2025/02/01

    Publisher: 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　2025/01/24

    Publisher: 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　2024/12/06

    Publisher: 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　2023/09/21

    Publisher: 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　2023/05/08

    Publisher: American Geophysical Union (AGU)

    DOI： 10.1029/2023gl103659 　

    ISSN： 0094-8276

    eISSN： 1944-8007

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    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　2022/03/22

    Publisher: 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　2020/11/15

    Publisher: 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　2020/08/26

    Publisher: 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　2019/02/27

    Publisher: 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　2018/10/02

    Publisher: 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　2017/04/14

    Publisher: 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

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Presentations 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 Invited

    Chi-Hsien Tang

    NIED seminar　2026/01/09

  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　2025/12/16

  3. Aseismic slip phenomenon in the southern Ryukyu forearc illuminated by geodetic observations Invited

    Chi-Hsien Tang

    IES Seminar　2025/09/25

  4. Characterizing earthquakes and aseismic slip in the western margin of the Philippine Sea plate Invited

    Chi-Hsien Tang

    AOGS Annual Meeting　2025/07/29

  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　2025/05/28

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

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

    JpGU Meeting　2025/05/25

  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　2025/05/30

  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　2025/05/28

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

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

    JpGU Meeting　2025/05/28

  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　2025/04/28

  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　2025/05/02

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

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

    AGU Fall Meeting　2024/12/13

  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　2024/12/11

  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　2024/12/12

  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　2024/12/12

  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

    GSJ Meeting　2024/10/30

  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　2024/05/28

  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　2024/05/28

  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　2024/05/31

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Research Projects 2

  1. Comparison of viscoelastic flow beneath Japan before and after the Tohoku-oki earthquake

    Offer Organization: Japan Society for the Promotion of Science

    System: Grants-in-Aid for Scientific Research

    Category: Grant-in-Aid for Early-Career Scientists

    Institution: Tohoku University

    2025/04/01 - 2028/03/31

  2. Waveglider-based GNSS-acoustic survey utilized oceanographic model

    Offer Organization: Japan Society for the Promotion of Science

    System: Grants-in-Aid for Scientific Research

    Category: Grant-in-Aid for Scientific Research (B)

    Institution: Tohoku University

    2024/04/01 - 2027/03/31

Teaching Experience 1

  1. Topics in Solid Earth Physics II　Tohoku University