{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360869855133802240.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.gsf.2025.102016"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S1674987125000167?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S1674987125000167?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Forecasting strong subsequent earthquakes in Japan using an improved version of NESTORE machine learning algorithm"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380869855133802371","@type":"Researcher","foaf:name":[{"@value":"S. Gentili"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869855133802263","@type":"Researcher","foaf:name":[{"@value":"G.D. Chiappetta"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869855133802120","@type":"Researcher","foaf:name":[{"@value":"G. Petrillo"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869855133802268","@type":"Researcher","foaf:name":[{"@value":"P. Brondi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869855133802271","@type":"Researcher","foaf:name":[{"@value":"J. Zhuang"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"16749871"}],"prism:publicationName":[{"@value":"Geoscience Frontiers"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2025-05","prism:volume":"16","prism:number":"3","prism:startingPage":"102016"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license","http://creativecommons.org/licenses/by-nc-nd/4.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S1674987125000167?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S1674987125000167?httpAccept=text/plain"}],"createdAt":"2025-02-17","modifiedAt":"2025-11-07","project":[{"@id":"https://cir.nii.ac.jp/crid/1040299826881404800","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23K28048"},{"@type":"JGN","@value":"JP23K28048"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23K28048/"}],"notation":[{"@language":"ja","@value":"欠測問題を含む拡張ホークスモデルの統計的推論手法の開発"},{"@language":"en","@value":"Development of Statistical Inference of Generalized Hawkes process Including the Missing Problem"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050302237609563776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Aftershocks following the 2011 Tohoku-Oki earthquake driven by both stress transfer and afterslip"}]},{"@id":"https://cir.nii.ac.jp/crid/1050857899425936512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High probability of successive occurrence of Nankai megathrust earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005518351715072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting the magnitude of the largest expected earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142940256896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geologically current motion of 56 plates relative to the no-net-rotation reference frame"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143792303616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Single-Link Cluster Analysis As A Method to Evaluate Spatial and Temporal Properties of Earthquake Catalogues"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144733682688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An introduction to ROC analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146521954688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A review of the rupture characteristics of the 2011 Tohoku-oki Mw 9.1 earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013171784135040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Pseudoprospective Evaluation of the Foreshock Traffic-Light System in Ridgecrest and Implications for Aftershock Hazard Assessment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017284955412992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Testing of the Seismic Gap Hypothesis in a Model With Realistic Earthquake Statistics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429442030208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Verifying the Magnitude Dependence in Earthquake Occurrence"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429443508992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Bayesian earthquake forecasting approach based on the epidemic type aftershock sequence model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025434005364736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"<i>b</i>‐More‐Incomplete and <i>b</i>‐More‐Positive: Insights on a Robust Estimator of Magnitude Distribution"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025434010468352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting the 2016–2017 Central Apennines Earthquake Sequence With a Neural Point Process"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025435025026432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Bayesian Estimation of the ETAS Model for Earthquake Occurrences"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025435813767296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Prediction of the occurrence of Related Strong Earthquakes in Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025437724463232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Assessing the Predictive Power of GPS-Based Ground Deformation Data for Aftershock Forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025437724535168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting Strong Subsequent Earthquakes in Greece with the Machine Learning Algorithm NESTORE"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025439309256576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Testing of the foreshock hypothesis within an epidemic like description of seismicity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025439373172736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A neural encoder for earthquake rate forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025439377387648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Incorporating Foreshocks in an Epidemic-like Description of Seismic Occurrence in Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500184192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evolution of the Sea of Japan back-arc and some unsolved issues"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710008366208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Distribution of the largest event in the critical epidemic-type aftershock-sequence model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619928457472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimation of Space–Time Branching Process Models in Seismology Using an EM–Type Algorithm"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620699175680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Software Package to Analyze Seismicity: ZMAP"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620789538432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Earthquake Aftershocks: Update"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621568598912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic moment distribution revisited: I. Statistical results"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306906103813120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic clusters and fluids diffusion: a lesson from the 2018 Molise (Southern Italy) earthquake sequence"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306906104256640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fluids-Triggered Swarm Sequence Supported by a Nonstationary Epidemic-Like Description of Seismicity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306912427989248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting strong aftershocks in earthquake clusters from northeastern Italy and western Slovenia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306912429364608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting strong aftershocks in the Italian territory: a National and Regional application for NESTOREv1."}]},{"@id":"https://cir.nii.ac.jp/crid/1360306913488392576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiated energy evolution during seismic sequences"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306913488393600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Pattern recognition approach to the subsequent event of damaging earthquakes in Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306913488394624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting strong subsequent earthquakes in California clusters by machine learning"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306914726539520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"GP-ETAS: semiparametric Bayesian inference for the spatio-temporal epidemic type aftershock sequence model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166809021696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structural control on the Tohoku earthquake rupture process investigated by 3D FEM, tsunami and geodetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567184984493184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Properties of the probability distribution associated with the largest event in an earthquake cluster and their implications to foreshocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092887403392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geologically current plate motions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092887737984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Philippine Sea and East Asian plate tectonics since 52 Ma constrained by new subducted slab reconstruction methods"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094476809216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Distribution of the largest aftershocks in branching models of triggered seismicity: Theory of the universal Båth law"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118734486016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"3D anisotropic structure of the Japan subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360579819990771840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Developments of the Nationwide Earthquake Early Warning System in Japan After the 2011 Mw9.0 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232382020608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The debate on the earthquake magnitude correlations: a meta-analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580234626978688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On Splitting Training and Validation Set: A Comparative Study of Cross-Validation, Bootstrap and Systematic Sampling for Estimating the Generalization Performance of Supervised Learning"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584344415421952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Impact of the Fukushima Accident on 3H and 14C Environmental Levels: A Review of Ten Years of Investigation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584346290518528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Using Deep Learning for Flexible and Scalable Earthquake Forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588385275928448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The partitioning of radiated energy and the largest aftershock of seismic sequences occurred in the northeastern Italy and western Slovenia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588385277607936","@type":"Article","resourceType":"preprint","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting strong subsequent events in the Italian territory: a National and Regional application for NESTOREv1.0"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641785240704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting large aftershocks within one day after the main shock"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663120807168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three Regimes of the Distribution of the Largest Event in the Critical ETAS Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569842455040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stochastic Declustering of Space-Time Earthquake Occurrences"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857596777971968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Overlap of Aftershock Coda Waves and Short‐Term Postseismic Forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861709551898368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861711798115328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Genesis of Aftershocks in Spring Slider Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861712168464256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fault Heterogeneity and the Connection between Aftershocks and Afterslip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855142165120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Distribution Related to All Samples and Extreme Events in the ETAS Cluster"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869858471505792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting of the first hour aftershocks by means of the perceived magnitude"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869859439773952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Semiparametric Bayesian forecasting of SpatioTemporal earthquake occurrences"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943443536384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Minimum Magnitude of Completeness in Earthquake Catalogs: Examples from Alaska, the Western United States, and Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945509912960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Better Decisions through Science"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946248869760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A space-time clustering model for historical earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418841004416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Is the sequence of earthquakes in Southern California, with aftershocks removed, Poissonian?"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419392518272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Aftershock Statistics of Major Subduction Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420032115712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Single-Link Cluster Analysis, Synthetic Earthquake Catalogues, and Aftershock Identification"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420539253760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Aftershocks hazard in Italy Part I: Estimation of time-magnitude distribution model parameters and computation of probabilities of occurrence"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894500861184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Comparison of characteristic and Gutenberg-Richter models for time-dependent M ≥ 7.9 earthquake probability in the Nankai-Tokai subduction zone, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368370160128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Space–time ETAS models and an improved extension"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844399914624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Earthquake Early Warning Starts Nationwide in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845170625024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Statistical Models for Earthquake Occurrences and Residual Analysis for Point Processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319305963264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep learning of aftershock patterns following large earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793836264832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Analysis of the Completeness Magnitude and Seismic Network Coverage of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794560747776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Second‐order moment of central California seismicity, 1969–1982"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268746760448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lateral inhomogeneities of the upper mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269943288704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Space-Time Point-Process Models for Earthquake Occurrences"}]},{"@id":"https://cir.nii.ac.jp/crid/1370869855133802117","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Catalog of large earthquakes in the region of Japan from 1885 through 1980"}]},{"@id":"https://cir.nii.ac.jp/crid/1370869855133802121","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Noise classification for the unified earthquake catalog using ensemble learning: the enhanced image of seismic activity along the Japan Trench by the S-net seafloor network"}]},{"@id":"https://cir.nii.ac.jp/crid/1370869855133802241","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A density-based algorithm for discovering clusters in large spatial databases with noise"}]},{"@id":"https://cir.nii.ac.jp/crid/1370869855133802247","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Risk of human-triggered earthquakes laid out in biggest-ever database"}]},{"@id":"https://cir.nii.ac.jp/crid/1370869855133802274","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"NESTOREv1.0: A MATLAB package for strong forthcoming earthquake forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1370869855133802374","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristics of northern and central California seismicity"}]},{"@id":"https://cir.nii.ac.jp/crid/1370869855133802377","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Time of increased probability for the great earthquakes of the world"}]},{"@id":"https://cir.nii.ac.jp/crid/1370869855133802381","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Robust statistics for outlier detection"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942185033344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shear-wave splitting in a region with newly-activated seismicity after the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842091742208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Change in seismicity beneath the Tokyo metropolitan area due to the 2011 off the Pacific coast of Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791867587968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Data completeness of the Kumamoto earthquake sequence in the JMA catalog and its influence on the estimation of the ETAS parameters"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792045148416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Earthquake forecast models for inland Japan based on the G-R law and the modified G-R law"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266972568320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of automatic hypocenter determination in the JMA unified catalog"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.gsf.2025.102016"},{"@type":"KAKEN","@value":"PRODUCT-25636372"}]}