Abstract
Ancient basement faults within plate interiors may be reactivated by external forces, generating intraplate seismicity. However, the driving mechanisms remain unclear. The 2017 Changdao earthquake swarm in the Bohai Bay Basin, eastern China, provides an opportunity to investigate such processes. A high-resolution earthquake catalog, constructed using matched filter detection and waveform-based relocation, reveals that the swarm occurred at 7-13 km depth along an X-shaped fault network, with migration following sqrt(t) diffusion (D = 0.08 – 1.2 m² s-1). High b-values and external forcing rate, and substantial isotropic components (13-38%) in the moment tensors indicate fluid involvement. Combined with low VP/VS ratios and proximity to CO2-rich hydrocarbon fields, we propose a fault-valve model where highly compressible fluids episodically breach fault intersections, triggering transient crack opening and swarm migration. This study reveals how deep fluids reactivate ancient basement faults in intraplate regions, and provides new insights for seismic hazard assessment in hydrocarbon-bearing basins.
Similar content being viewed by others
Data availability
Three-component (3-C) waveform data from 12 seismic stations are available from the China Earthquake Network Center (CENC) Data Sharing Service (login required): https://data.earthquake.cn/datashare/login.jsp. The datasets supporting this study are deposited on Figshare (DOI: 10.6084/m9.figshare.30944375), including the detected earthquake catalog (Supplementary Data 1), the relocated earthquake catalog (Supplementary Data 2), and the focal-mechanism catalog (Supplementary Data 3). The Figshare files are under embargo until 24 January 2026, after which they will be publicly accessible44.
Code availability
ETAS modeling was implemented using GeoTaos60 (https://bemlar.ism.ac.jp/lxl/). The MFT code41 is also available from the corresponding author.
References
Ben-Zion, Y. & Sammis, C. G. Characterization of fault zones. Pure Appl. Geophys. 160, 677–715 (2003).
Wibberley, C. A., Gonzalez-Dunia, J. & Billon, O. Faults as barriers or channels to production-related flow: insights from case studies. Pet. Geosci. 23, 134–147 (2017).
Xu, J. et al. Features of seismogenic structures of great earthquakes in the Bohai Bay basin area, north China. Seismol. Geol. 34, 618–636 (2012).
Sibson, R. H. Conditions for fault-valve behaviour. Geol. Soc. Lond. Spec. Publ. 54, 15–28 (1990).
Ruh, J. B. & Vergés, J. Effects of reactivated extensional basement faults on structural evolution of fold-and-thrust belts: Insights from numerical modelling applied to the Kopet Dagh Mountains. Tectonophysics 746, 493–511 (2018).
Sibson, R. H. An episode of fault-valve behaviour during compressional inversion?— The 2004 MJ6.8 Mid-Niigata Prefecture, Japan, earthquake sequence. Earth Planet. Sci. Lett. 257, 188–199 (2007).
Kato, A. et al. Reactivation of ancient rift systems triggers devastating intraplate earthquakes. Geophys. Res. Lett. 36, L05301 (2009).
Kato, A. Implications of fault-valve behavior from immediate aftershocks following the 2023 Mj6.5 earthquake beneath the Noto Peninsula, central Japan. Geophys. Res. Lett. 51, e2023GL106444 (2024).
Peng, Z. et al. The evolution process between the earthquake swarm beneath the Noto Peninsula, central Japan and the 2024 M 7.6 Noto Hanto earthquake sequence. Earthq. Res. Adv. 100332. https://doi.org/10.1016/j.eqrea.2024.100332 (2025)
Sibson, R. H. Structural permeability of fluid-driven fault-fracture meshes. J. Struct. Geol. 18, 1031–1042 (1996).
Townend, J. & Zoback, M. D. How faulting keeps the crust strong. Geology 28, 399–402 (2000).
Camanni, G. & Ye, Q. The significance of fault reactivation on the Wilson cycle undergone by the northern South China Sea area in the last 60 Myr. Earth-Sci. Rev. 225, 103893 (2022).
Ma, Z. et al. Slow rupture in a fluid-rich fault zone initiated the 2024 Mw 7.5 Noto earthquake. Science 385, 866–871 (2024).
Sibson, R. H. Crustal stress, faulting and fluid flow. Geol. Soc. Lond. Spec. Publ. 78, 69–84 (1994).
Miller, S. A. The role of fluids in tectonic and earthquake processes. Adv. Geophys. 54, 1–46 (2013).
Yoshida, K. et al. Updip fluid flow in the crust of the northeastern Noto Peninsula, Japan, triggered the 2023 Mw 6.2 Suzu earthquake during swarm activity. Geophys. Res. Lett. 50, e2023GL106023 (2023).
Yoshida, K. et al. Role of a hidden fault in the early process of the 2024 Mw7.5 Noto Peninsula earthquake. Geophys. Res. Lett. 51, e2024GL110993 (2024).
Mogi, K. Some discussions on aftershocks, foreshocks and earthquake swarms—the fracture of a semi finite body caused by an inner stress origin and its relation to the earthquake phenomena. Bull. Earthq. Res. Inst. 41, 615–658 (1963).
Vidale, J. E. & Shearer, P. M. A survey of 71 earthquake bursts across southern California: exploring the role of pore fluid pressure fluctuations and aseismic slip as drivers. J. Geophys. Res. Solid Earth 111, B05312 (2006).
Su, J., Lei, X., Li, J. & Huang, C. Detailed view of the seismogenic structures and processes of the 2022 Bayan Har intraplate earthquake swarm on the East Margin of the Qinghai–Tibet Plateau. Seismol. Res. Lett. 94, 2167–2180 (2023).
Liu, M. et al. Intersection between tectonic faults and magmatic systems promotes swarms with large-magnitude earthquakes around the Tengchong volcanic field, southeastern Tibetan Plateau. Geology 52, 302–307 (2024).
Shelly, D. R., Moran, S. C. & Thelen, W. A. Evidence for fluid-triggered slip in the 2009 Mount Rainier, Washington earthquake swarm. Geophys. Res. Lett. 40, 1506–1512 (2013).
Shelly, D. R. et al. A fluid-driven earthquake swarm on the margin of the Yellowstone caldera. J. Geophys. Res. Solid Earth 118, 4872–4886 (2013).
Shelly, D. R. et al. Fluid-faulting interactions: fracture-mesh and fault-valve behavior in the February 2014 Mammoth Mountain, California, earthquake swarm. Geophys. Res. Lett. 42, 5803–5812 (2015).
Ross, Z. E., Cochran, E. S., Trugman, D. T. & Smith, J. D. 3D fault architecture controls the dynamism of earthquake swarms. Science 368, 1357–1361 (2020).
Lei, X. et al. Fault reactivation and earthquakes with magnitudes of up to Mw 4.7 induced by shale-gas hydraulic fracturing in Sichuan Basin, China. Sci. Rep. 7, 7971 (2017).
Lei, X., Su, J. & Wang, Z. Growing seismicity in the Sichuan Basin and its association with industrial activities. Sci. China Earth Sci. 63, 1633–1660 (2020).
Fischer, T. et al. Intra-continental earthquake swarms in West-Bohemia and Vogtland: a review. Tectonophysics 611, 1–27 (2014).
De Barros, L., Cappa, F., Deschamps, A. & Dublanchet, P. Imbricated aseismic slip and fluid diffusion drive a seismic swarm in the Corinth Gulf, Greece. Geophys. Res. Lett. 47, e2020GL087142 (2020).
De Barros, L., Wynants-Morel, N., Cappa, F. & Danré, P. Migration of fluid-induced seismicity reveals the seismogenic state of faults. J. Geophys. Res. Solid Earth 126, e2021JB022767 (2021).
Shelly, D. R., Ellsworth, W. L. & Hill, D. P. Fluid-faulting evolution in high definition: connecting fault structure and frequency-magnitude variations during the 2014 Long Valley Caldera, California, earthquake swarm. J. Geophys. Res. Solid Earth 121, 1776–1795 (2016).
Lei, X. & Wang, G. Is clustered seismicity an indicator of regional stress? Insights from earthquake sequences in Yongning-Luguhu faulted basin, Southwest China. Earthq. Res. Adv. 2, 100138 (2022).
Woo, J. U. & Ellsworth, W. L. Reactivation of Precambrian faults by deep wastewater injection in Midland Basin, Texas, and performance evaluation of seismic response areas. Bull. Seismol. Soc. Am. 113, 2543–2556 (2023).
Nishimura, T., Hiramatsu, Y. & Ohta, Y. Episodic transient deformation revealed by the analysis of multiple GNSS networks in the Noto Peninsula, central Japan. Sci. Rep. 13, 8381 (2023).
Long, L., Kocaoglu, A., Hawman, R. & Gore, P. The Norris Lake earthquake swarm of June through September, 1993; preliminary findings. Seismol. Res. Lett. 65, 167–171 (1994).
Chen, J. & Wolf, L. W. A notable earthquake swarm in Alabama: Natural or anthropogenic?. Seismol. Res. Lett. 89, 1583–1594 (2018).
Adeboboye, O. E. et al. Localized west-dipping seismic structure defines the Elgin-Lugoff Swarm Sequence in South Carolina. Seismol. Res. Lett. 95, 123–145 (2024).
Li, X. et al. Inversion of P-wave three-dimensional velocity structure and analysis of seismogenic structure of earthquake swarm in 2017 in Miaodao islands, Shandong province. Seismol. Geol. 42, 1188–1204 (2020).
Qu, J. et al. Crustal P-wave velocity structure and earthquake distribution in the Jiaodong Peninsula, China. Tectonophysics 814, 228973 (2021).
Gibbons, S. J. & Ringdal, F. The detection of low magnitude seismic events using array-based waveform correlation. Geophys. J. Int. 165, 149–166 (2006).
Peng, Z. & Zhao, P. Migration of early aftershocks following the 2004 Parkfield earthquake. Nat. Geosci. 2, 877–881 (2009).
Waldhauser, F. & Ellsworth, W. L. A double-difference earthquake location algorithm: method and application to the northern Hayward Fault, California. Bull. Seismol. Soc. Am. 90, 1353–1368 (2000).
Yang, H. F., Zhu, L. P. & Chu, R. S. Fault-plane determination of the 18 April 2008 Mount Carmel, Illinois, earthquake by detecting and relocating aftershocks. Bull. Seismol. Soc. Am. 99, 3413–3420 (2009).
Wang, P., Wang, B., Peng, Z. & Lei, X. The datasets of the 2017 Changdao swarm in eastern China. figshare. https://doi.org/10.6084/m9.figshare.30944375 (2026).
Wiemer, S. & Katsumata, K. Spatial variability of seismicity parameters in aftershock zones. J. Geophys. Res. Solid Earth 104, 13135–13151 (1999).
Zhu, L. P. & Helmberger, D. V. Advancement in source estimation techniques using broadband regional seismograms. Bull. Seismol. Soc. Am. 86, 1634–1641 (1996).
Yu, C. Q., Tao, K., Cui, X. F., Hu, X. P. & Ning, J. Y. P-wave first-motion focal mechanism solution and their quality evaluation. Chin. J. Geophys. 52, 1402–1411 (2009).
Vavryčuk, V. & Hrubcová, P. Seismological evidence of fault weakening due to erosion by fluids from observations of intraplate earthquake swarms. J. Geophys. Res. Solid Earth 122, 3701–3718 (2017).
Vavryčuk, V. Iterative joint inversion for stress and fault orientations from focal mechanisms. Geophys. J. Int. 199, 69–77 (2014).
Liu, F. B., Qu, J. H., Li, G. Y. & Tian, Z. Y. Time-space evolution characteristics of the focal mechanism consistency parameter of the Changdao earthquake swarm in Shandong Province. China Earthq. Eng. J. 40, 1034–1041 (2018).
Chen, X., Shearer, P. M. & Abercrombie, R. E. Spatial migration of earthquakes within seismic clusters in Southern California: Evidence for fluid diffusion. J. Geophys. Res. 117, B04301 (2012).
Shapiro, S. A., Huenges, E. & Borm, G. Estimating the crust permeability from fluid-injection-induced seismic emission at the KTB site. Geophys. J. Int. 131, F15–F18 (1997).
Lohman, R. B. & McGuire, J. J. Earthquake swarms driven by aseismic creep in the Salton Trough, California. J. Geophys. Res. Solid Earth 112, B04405 (2007).
Peng, Z. & Lei, X. Physical mechanisms of earthquake nucleation and foreshock: cascade triggering, aseismic slip, or fluid flows?. Earthq. Res. Adv. 5, 100349 (2025).
Hainzl, S. Seismicity patterns of earthquake swarms due to fluid intrusion and stress triggering. Geophys. J. Int. 159, 1090–1096 (2004).
Shapiro, S. A., Rentsch, S. & Rothert, E. Characterization of hydraulic properties of rocks using probability of fluid-induced microearthquakes. Geophysics 70, 27–33 (2005).
Schoenball, M. & Ellsworth, W. L. A systematic assessment of the spatiotemporal evolution of fault activation through induced seismicity in Oklahoma and southern Kansas. J. Geophys. Res. Solid Earth 122, 10189–10206 (2017).
Sheng, M. et al. Earthquakes triggered by fluid diffusion and boosted by fault reactivation in Weiyuan, China due to hydraulic fracturing. J. Geophys. Res. Solid Earth 127, e2021JB022963 (2022).
Yukutake, Y. et al. Fluid-induced swarm earthquake sequence revealed by precisely determined hypocenters and focal mechanisms in the 2009 activity at Hakone volcano, Japan. J. Geophys. Res. Solid Earth 116, B04308 (2011).
Ogata, Y. Detection of precursory relative quiescence before great earthquakes through a statistical model. J. Geophys. Res. Solid Earth 97, 19845–19871 (1992).
Hainzl, S. & Ogata, Y. Detecting fluid signals in seismicity data through statistical earthquake modeling. J. Geophys. Res. 110, B05S07 (2005).
Lei, X. et al. A detailed view of the injection-induced seismicity in a natural gas reservoir in Zigong, southwestern Sichuan basin, China. J. Geophys. Res. Solid Earth 118, 4296–4311 (2013).
Zhang, H., Eaton, D. W., Li, G., Liu, Y. & Harrington, R. M. Discriminating induced seismicity from natural earthquakes using moment tensors and source spectra. J. Geophys. Res. Solid Earth 121, 972–993 (2016).
Lin, G., Peng, Z. & Neves, M. Comparisons of in situ VP/VS ratios and seismic characteristics between northern and southern California. Geophys. J. Int. 229, 2162–2174 (2022).
Sui, S., Shen, W., Mahan, K. & Schulte-Pelkum, V. Constraining the crustal composition of the continental US using seismic observables. GSA Bull. 135, 2038–2056 (2023).
Ji, G., Lei, J. & Zhao, D. 3-D crustal velocity structure and seismogenic environment of earthquake swarms in the Jiaodong area using multiple-phase travel-time tomography. Chin. J. Geophys. 68, 123–138 (2025).
Lin, G. & Shearer, P. M. Evidence for water-filled cracks in earthquake source regions. Geophys. Res. Lett. 36, L17315 (2009).
Lin, G. Spatiotemporal variations of in situ VP/VS ratio within the Salton Sea Geothermal Field, southern California. Geothermics 84, 101740 (2020).
Nakajima, J. Crustal structure beneath earthquake swarm in the Noto Peninsula, Japan. Earth Planets Space 74, 160 (2022).
Nakajima, J. The Wakayama earthquake swarm in Japan. Earth Planets Space 75, 48 (2023).
Okada, T. et al. Shear wave splitting and seismic velocity structure in the focal area of the earthquake swarm and their relation with earthquake swarm activity in the Noto Peninsula, Central Japan. Earth Planets Space 76, 24 (2024).
Geoffroy, L. et al. Hydrothermal fluid flow triggered by an earthquake in Iceland. Commun. Earth Environ. 3, 54 (2022).
Masihi, A. & Fischer, T. In-situ VP/VS ratio variations in seismic swarms as indicator of magmatic processes: Fagradalsfjall volcanic activity, SW Iceland. Geophys. J. Int. 241, 1725–1739 (2025).
Huang, Y. et al. Fault material heterogeneity controls deep interplate earthquakes. Sci. Adv. 11, eadr9353 (2025).
Toksöz, M. N., Cheng, C. H. & Timur, A. Velocities of seismic waves in porous rocks. Geophysics 41, 621–645 (1976).
Takei, Y. Effect of pore geometry on VP/VS: from equilibrium geometry to crack. J. Geophys. Res. Solid Earth 107, ECV 6–1–ECV (2002).
Doi, I. et al. Relationship between hypocentral distributions and VP/VS ratio structures inferred from dense seismic array data: a case study of the 1984 western Nagano Prefecture earthquake, central Japan. Geophys. J. Int. 195, 1323–1336 (2013).
Ou, G.X. et al. Research progress on mantle fluids and deep oil and gas in the Miaodao Archipelago. In China Geophysics 2010: Proceedings of the 26th Annual Meeting of the Chinese Geophysical Society and the 13th Academic Conference of the Seismological Society of China 187–188 (Chinese Geophysical Society & Seismological Society of China, 2010).
Chen, C. et al. Mantle transition zone, stagnant slab and intraplate volcanism in Northeast Asia. Geophys. J. Int. 209, 68–85 (2017).
Lei, J., Tian, X., Mishra, O. P. & Huang, Z. Deep structure and dynamics under East Asia. J. Asian Earth Sci. 258, 105921 (2023).
Xu, X. W., Wu, W. M. & Zhang, X. K. The latest tectonic changes and earthquakes in the crustal region of the capital region. (Science Press, Beijing, 2002).
Yu, X. F. et al. Deep structural framework and genetic analysis of gold concentration areas in the northwestern Jiaodong Peninsula, China: a new understanding based on high-resolution reflective seismic survey. Acta Geol. Sin. 92, 1823–1840 (2018).
Sibson, R. H. Implications of fault-valve behaviour for rupture nucleation and recurrence. Tectonophysics 211, 283–293 (1992).
Gudmundsson, A., Marinoni, L. B. & Marti, J. Injection and arrest of dykes: implications for volcanic hazards. J. Volcanol. Geotherm. Res. 88, 1–13 (1999).
Chen, Y., Li, Z. H., Tang, K. & Shi, Y. Mechanism of metamorphic fluid expulsion from ductile contact aureole: insights from numerical modeling of a growing mid-crustal magma chamber. Earth Planet. Sci. Lett. 626, 118545 (2024).
Li, Y., Li, H. & Huang, Y. Seismicity in the Weiyuan-Rongxian area, Sichuan Basin, SW China. J. Asian Earth Sci. 272, 106241 (2024).
Cappa, F. Modelling fluid transfer and slip in a fault zone when integrating heterogeneous hydromechanical characteristics in its internal structure. Geophys. J. Int. 178, 1357–1362 (2009).
Wang, P. & Wang, B. S. Stress drop estimation of Chang Island earthquake swarm by generalized superposition inversion method. Chin. J. Geophys. 63, 1970–1985 (2020).
Cardenas, M. B. & Jiang, X.-W. Groundwater flow, transport, and residence times through topography-driven basins with exponentially decreasing permeability and porosity. Water Resour. Res. 46, W11538 (2010).
Saar, M. O. & Manga, M. Depth dependence of permeability in the Oregon Cascades inferred from hydrogeologic, thermal, seismic, and magmatic modeling constraints. J. Geophys. Res. Solid Earth 109, B04204 (2004).
Stober, I. Depth- and pressure-dependent permeability in the upper continental crust: data from the Urach 3 geothermal borehole, southwest Germany. Hydrogeol. J. 19, 685–699 (2011).
Amezawa, Y. et al. Long-living earthquake swarm and intermittent seismicity in the northeastern tip of the Noto Peninsula, Japan. Geophys. Res. Lett. 50, e2022GL102670 (2023).
Lei, X. Fluid-driven fault nucleation, rupture processes, and permeability evolution in Oshima granite-preliminary results and acoustic emission datasets. Geohazard Mech. 2, 164–180 (2024).
van der Elst, N. J. & Brodsky, E. E. Connecting near-field and far-field earthquake triggering to dynamic strain. J. Geophys. Res. Solid Earth. 115, B07311 (2010).
Bell, A. F. et al. Dynamic earthquake triggering response tracks evolving unrest at Sierra Negra volcano, Galápagos Islands. Sci. Adv. 7, eabh0894 (2021).
Hill, D. P. & Prejean, S. G. Dynamic Triggering. in Treatise on Geophysics 273–304 (Elsevier, 2015).
Kilb, D., Gomberg, J. & Bodin, P. Triggering of earthquake aftershocks by dynamic stresses. Nature 408, 570–574 (2000).
Pankow, K. L. & Kilb, D. Going beyond rate changes as the sole indicator for dynamic triggering of earthquakes. Sci. Rep. 10, 4120 (2020).
Hardebeck, J. L., DeSalvio, N. D., Fan, W. & Barbour, A. J. False positives in the identification of dynamic earthquake triggering. J. Geophys. Res. Solid Earth 130, e2025JB031566 (2025).
Danré, P., De Barros, L., Cappa, F. & Passarelli, L. Parallel dynamics of slow slips and fluid-induced seismic swarms. Nat. Commun. 15, 8943 (2024).
Poupinet, G., Ellsworth, W. L. & Frechet, J. Monitoring velocity variations in the crust using earthquake doublets: an application to the Calaveras Fault, California. J. Geophys. Res. Solid Earth 89, 5719–5731 (1984).
Shearer, P. M. Improving local earthquake locations using the L1 norm and waveform cross correlation: application to the Whittier Narrows, California, aftershock sequence. J. Geophys. Res. Solid Earth 102, 8269–8283 (1997).
Pan, S. Z. et al. Crustal velocity structure beneath Jiaodong Peninsula and its tectonic implications. Chin. J. Geophys. 58, 3251–3263 (2015).
Matthews, M. V. & Reasenberg, P. A. Statistical methods for investigating quiescence and other temporal seismicity patterns. Pure Appl. Geophys. 126, 357–372 (1988).
Peng, Z., Wang, W., Chen, Q. F. & Jiang, T. Remotely triggered seismicity in north China following the 2008 Mw 7.9 Wenchuan earthquake. Earth Planets Space 62, 893–898 (2010).
Peng, Z., Long, L. T. & Zhao, P. The relevance of high-frequency analysis artifacts to remote triggering. Seismol. Res. Lett. 82, 654–660 (2011).
Liu, G. et al. Detecting remotely triggered microseismicity around Changbaishan Volcano following nuclear explosions in North Korea and large distant earthquakes around the world. Geophys. Res. Lett. 44, 4829–4838 (2017).
Wessel, P. et al. The generic mapping tools version 6. Geochem. Geophys. Geosyst. 20, 5556–5564 (2019).
Wang, Z. C. et al. Shallow-depth sonic reflection profiling studies on the active Penglai-Weihai fault zone offshore of the northern Shandong peninsula. Chin. J. Geophys. 49, 1092–1101 (2006).
Acknowledgements
We thank the CEE editors Dr. Luca Dal Zilio and Dr. Joe Aslin, reviewers Dr. Debi Kilb and another anonymous reviewer for their help in improving the manuscript, Dr. Hongfeng Yang for sharing his modified double difference location program, Drs Jianchang Zheng, Jinxi Hou, Bo Zhang for their suggestions on the focal source mechanisms, the matched-filter, and earthquake locations, respectively. This study was supported by the National Natural Science Foundation of China (Grant No. 42430103), Chinese Academy of Sciences (CAS) Project for Young Scientists in Basic Research (Grant No. YSBR-020), the Natural Science Foundation of Shandong Province, China (Grant No. ZR2024MD093), the Natural Science Foundation of Dongying city (Grant No. 2024ZR032), the Scientific Research Startup Foundation of Shandong Institute of Petroleum and Chemical Technology, and the Science Development Foundation of Dongying city, China (Grant No. DJB2022015). Z. P. is partially supported by the U.S. National Science Foundation (Grant No. RISE-2425889). Seismic waveforms and catalog are provided by the China Earthquake Networks Center. Figures are constructed with the Generic Mapping Tools108.
Author information
Authors and Affiliations
Contributions
P.W. and B.W. conceived and initiated the study. P.W. processed the data and drafted the manuscript. Z.P. provided the matched-filter detection code. B.W., Z.P., and X.L. contributed to interpretation of the results and revised the manuscript. P.W. prepared the figures and movie, with input and modifications suggested by Z.P., B.W., and X.L. The supplementary Movie was edited and refined by Z.P. All authors reviewed and approved the final manuscript.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing interests.
Peer review
Peer review information
Communications Earth and Environment thanks Debi Kilb and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Primary Handling Editors: Luca Dal Zilio and Joseph Aslin. [A peer review file is available].
Additional information
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Rights and permissions
Open Access This article is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License, which permits any non-commercial use, sharing, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if you modified the licensed material. You do not have permission under this licence to share adapted material derived from this article or parts of it. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by-nc-nd/4.0/.
About this article
Cite this article
Wang, P., Wang, B., Peng, Z. et al. Reactivation of basement faults by deep fluids during the 2017 Changdao earthquake swarm, Eastern China. Commun Earth Environ (2026). https://doi.org/10.1038/s43247-026-03228-1
Received:
Accepted:
Published:
DOI: https://doi.org/10.1038/s43247-026-03228-1


