{"@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/1390282763076663808.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5575/geosoc.2018.0028"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"029311525"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/029311525"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I029311525"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/geosoc/124/9/124_2018.0028/_pdf"}},{"identifier":{"@type":"NAID","@value":"130007531014"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@language":"en","@value":"Progress of active fault studies in Japan in the past 25 years and future prospects"},{"@language":"ja","@value":"我が国における活断層研究の最近25年の成果と今後の展望"},{"@language":"ja-Kana","@value":"ワガクニ ニ オケル カツダンソウ ケンキュウ ノ サイキン 25ネン ノ セイカ ト コンゴ ノ テンボウ"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"<p>We reviewed studies of active faults in Japan during the past 25 years, particularly since the 1995 Hyogo-ken Nanbu earthquake that drastically changed the system and budget for such studies. Active fault studies have been central to the national seismic hazard reduction program, led by the Headquarters for Earthquake Research Promotion (HERP). Many studies have examined ~100 major active fault zones, employing paleoseismic trenching and high-resolution shallow seismic reflection profiling. Several types of large-scale maps of active faults have been published, including digital maps with three-dimensional base maps. These data are fundamental to the long-term evaluation of earthquake occurrences on major active fault zones. New research techniques have been introduced to active fault studies, such as detailed digital elevation models (DEMs), light detection and ranging (LiDAR), photogrammetry using unmanned aerial vehicles (UAV), shallow subsurface geophysics, and OxCal age modelling of paleoseismic events. Since the 1995 earthquake, there have been several surface-rupturing inland earthquakes with highly variable earthquake magnitude and coseismic faulting behavior. These earthquakes illustrate the need for new criteria for long-term evaluation of seismic hazard, including the incorporation of non-characteristic earthquakes into seismic hazard models, rather than assuming only characteristic earthquakes for a given fault zone.</p>"},{"@language":"ja","@value":"<p>本論文は，主に1990年以降に公表された論文や活断層図などを基に，日本の活断層研究の最近25年間の動向をまとめたものである．1995年の兵庫県南部地震以降，国の地震研究体制が大きく変化し，それに伴い活断層研究の体制が大きく変わった．それ以前とは比較にならない多額の予算が投入され，活断層の分布や活動履歴，地下構造に関する情報が急増し，活断層から発生する地震の長期予測に資するデータが蓄積された．一方，近年続発した内陸直下型被害地震は，活断層から発生する地震の規模や発生様式が多様かつ複雑であることを示しており，固有地震モデルに基づく地震の長期評価の妥当性の検証が必要である．活断層研究は，空中写真判読による地形解析と現地踏査を基礎にしながらも，近年急速に発達している宇宙測地学・物理探査・詳細地形データなどを取り入れて多面的に展開される必要がある．</p>"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751141551872","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60284428"},{"@type":"NRID","@value":"1000060284428"},{"@type":"ORCID","@value":"0000-0002-1729-8494"},{"@type":"AID","@value":"DA19006691"},{"@type":"NRID","@value":"9000413854618"},{"@type":"NRID","@value":"9000347361371"},{"@type":"NRID","@value":"9000413564384"},{"@type":"NRID","@value":"9000403163836"},{"@type":"NRID","@value":"9000023910521"},{"@type":"NRID","@value":"9000318589523"},{"@type":"NRID","@value":"9000413340204"},{"@type":"NRID","@value":"9000409992933"},{"@type":"NRID","@value":"9000375922327"},{"@type":"NRID","@value":"9000392869125"},{"@type":"NRID","@value":"9000347362363"},{"@type":"NRID","@value":"9000020971082"},{"@type":"NRID","@value":"9000403163857"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/7000008624"}],"foaf:name":[{"@language":"en","@value":"Tsutsumi Hiroyuki"},{"@language":"ja","@value":"堤 浩之"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"同志社大学理工学部環境システム学科"},{"@language":"en","@value":"Department of Environmental Systems Science, Faculty of Science and Engineering, Doshisha University"}]},{"@id":"https://cir.nii.ac.jp/crid/1030018198853579392","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000305637298"},{"@type":"NRID","@value":"9000391514311"},{"@type":"NRID","@value":"9000347191248"},{"@type":"NRID","@value":"9000010225980"},{"@type":"NRID","@value":"9000020963166"},{"@type":"NRID","@value":"9000280540928"},{"@type":"NRID","@value":"9000009976166"},{"@type":"NRID","@value":"9000347083860"},{"@type":"NRID","@value":"9000258264100"},{"@type":"NRID","@value":"9000312731134"},{"@type":"NRID","@value":"9000392674516"},{"@type":"NRID","@value":"9000391405365"},{"@type":"NRID","@value":"9000020989036"},{"@type":"NRID","@value":"9000020135345"},{"@type":"NRID","@value":"9000020979641"},{"@type":"NRID","@value":"9000399224128"},{"@type":"NRID","@value":"9000255912812"},{"@type":"NRID","@value":"9000014203826"},{"@type":"NRID","@value":"9000020955969"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0120038"}],"foaf:name":[{"@language":"en","@value":"Kondo Hisao"},{"@language":"ja","@value":"近藤 久雄"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"産業技術総合研究所活断層・火山研究部門"},{"@language":"en","@value":"Research Institute of Earthquake and Volcano Geology, Geological Survey of Japan, AIST"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801191626112","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"90356452"},{"@type":"NRID","@value":"1000090356452"},{"@type":"NRID","@value":"9000258418022"},{"@type":"NRID","@value":"9000392039705"},{"@type":"NRID","@value":"9000401503292"},{"@type":"NRID","@value":"9000002496633"},{"@type":"NRID","@value":"9000283727261"},{"@type":"NRID","@value":"9000392039493"},{"@type":"NRID","@value":"9000336380705"},{"@type":"NRID","@value":"9000009831402"},{"@type":"NRID","@value":"9000410949443"},{"@type":"NRID","@value":"9000009815345"},{"@type":"NRID","@value":"9000020957046"},{"@type":"NRID","@value":"9000403311025"},{"@type":"NRID","@value":"9000410949373"},{"@type":"NRID","@value":"9000290134845"},{"@type":"NRID","@value":"9000392039220"},{"@type":"NRID","@value":"9000360550625"},{"@type":"NRID","@value":"9000283726821"},{"@type":"NRID","@value":"9000392040357"},{"@type":"NRID","@value":"9000336381360"},{"@type":"NRID","@value":"9000021238952"},{"@type":"NRID","@value":"9000377383381"},{"@type":"NRID","@value":"9000392869016"},{"@type":"NRID","@value":"9000283727096"},{"@type":"NRID","@value":"9000304607135"},{"@type":"NRID","@value":"9000020936874"},{"@type":"NRID","@value":"9000392040776"},{"@type":"NRID","@value":"9000399241311"},{"@type":"NRID","@value":"9000258415666"},{"@type":"NRID","@value":"9000258415657"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/t-ishiyama"}],"foaf:name":[{"@language":"en","@value":"Ishiyama Tatsuya"},{"@language":"ja","@value":"石山 達也"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"東京大学地震研究所"},{"@language":"en","@value":"Earthquake Research Institute, University of Tokyo"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167630"},{"@type":"EISSN","@value":"13499963"},{"@type":"CODEN","@value":"CHTZA5"},{"@type":"NDL_BIB_ID","@value":"000000014674"},{"@type":"ISSN","@value":"00167630"},{"@type":"LISSN","@value":"00167630"},{"@type":"NCID","@value":"AN00141768"}],"prism:publicationName":[{"@language":"en","@value":"The Journal of the Geological Society of Japan"},{"@language":"ja","@value":"地質学雑誌"},{"@language":"en","@value":"Jour. Geol. Soc. Japan"},{"@language":"ja","@value":"地質雑"},{"@language":"ja","@value":"地雑"}],"dc:publisher":[{"@language":"en","@value":"The Geological Society of Japan"},{"@language":"ja","@value":"一般社団法人 日本地質学会"}],"prism:publicationDate":"2018-09-15","prism:volume":"124","prism:number":"9","prism:startingPage":"741","prism:endingPage":"757"},"reviewed":"false","url":[{"@id":"http://id.ndl.go.jp/bib/029311525"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I029311525"},{"@id":"https://www.jstage.jst.go.jp/article/geosoc/124/9/124_2018.0028/_pdf"}],"availableAt":"2018-09-15","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=active%20faults","dc:title":"active faults"},{"@id":"https://cir.nii.ac.jp/all?q=paleoseismology","dc:title":"paleoseismology"},{"@id":"https://cir.nii.ac.jp/all?q=seismic%20hazard%20evaluation","dc:title":"seismic hazard evaluation"},{"@id":"https://cir.nii.ac.jp/all?q=trenching","dc:title":"trenching"},{"@id":"https://cir.nii.ac.jp/all?q=seismic%20reflection%20surveys","dc:title":"seismic reflection surveys"},{"@id":"https://cir.nii.ac.jp/all?q=active%20fault%20maps","dc:title":"active fault maps"},{"@id":"https://cir.nii.ac.jp/all?q=non-characteristic%20earthquakes","dc:title":"non-characteristic earthquakes"},{"@id":"https://cir.nii.ac.jp/all?q=active%20faults","dc:title":"active faults"},{"@id":"https://cir.nii.ac.jp/all?q=paleoseismology","dc:title":"paleoseismology"},{"@id":"https://cir.nii.ac.jp/all?q=seismic%20hazard%20evaluation","dc:title":"seismic hazard evaluation"},{"@id":"https://cir.nii.ac.jp/all?q=trenching","dc:title":"trenching"},{"@id":"https://cir.nii.ac.jp/all?q=seismic%20reflection%20surveys","dc:title":"seismic reflection surveys"},{"@id":"https://cir.nii.ac.jp/all?q=active%20fault%20maps","dc:title":"active fault maps"},{"@id":"https://cir.nii.ac.jp/all?q=non-characteristic%20earthquakes","dc:title":"non-characteristic earthquakes"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781895263744","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H01829"},{"@type":"JGN","@value":"JP16H01829"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H01829/"}],"notation":[{"@language":"ja","@value":"高解像度地形データを活用した新たな電子活断層図の作成"},{"@language":"en","@value":"Newly designed digital active fault map using  high-resolution DEM-based geomorphological data"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781897274240","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H03114"},{"@type":"JGN","@value":"JP16H03114"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H03114/"}],"notation":[{"@language":"ja","@value":"一まわり小さな地震を考慮した活断層の地震発生予測モデルの構築"},{"@language":"en","@value":"Earthquake occurrence prediction model consideration one size small earthquake by active fault"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335841154176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geomorphic features of surface ruptures associated with the 2016 Kumamoto earthquake in and around the downtown of Kumamoto City, and implications on triggered slip along active faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282810795503744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Co-seismic surface ruptures produced by the 2014 Mw 6.2 Nagano earthquake, along the Itoigawa–Shizuoka tectonic line, central Japan"},{"@value":"Co‐seismic surface ruptures produced by the 2014 Mw 6.2 Nagano earthquake, along the Itoigawa–Shizuoka tectonic line, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564285709667968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stability of the regional stress field in central Japan during the late Quaternary inferred from the stress inversion of the active fault data"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760738354304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source rupture process of the 2011 Fukushima-ken Hamadori earthquake: how did the two subparallel faults rupture?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523503360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geometry and slip rates of active blind thrusts in a reactivated back-arc rift using shallow seismic imaging: Toyama basin, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233288139392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Widespread seismicity excitation throughout central Japan following the 2011 M=9.0 Tohoku earthquake and its interpretation by Coulomb stress transfer"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693141019904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evolution of crustal deformation in the northeast–central Japanese island arc: Insights from fault activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285705098939776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Active blind thrusts beneath the Tokyo metropolitan area: Seismic hazards and inversion 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strata"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570825953024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geomorphology, kinematic history, and earthquake behavior of the active Kuwana wedge thrust anticline, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043518050944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Transient Uplift After a 17th-Century Earthquake Along the Kuril Subduction Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520160356736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Holocene fault scarps near Tacoma, Washington, USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520943936000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Active folding of fluvial terraces across the Siwaliks Hills, Himalayas of central Nepal"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994790156032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A fault scarp in an urban area identified by LiDAR survey: A Case study on the Itoigawa–Shizuoka Tectonic Line, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944508789760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Growth of Wheeler Ridge anticline, California: geomorphic evidence for fault-bend folding behaviour during earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945888725504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Gently north-dipping Median Tectonic Line (MTL) revealed by recent seismic reflection studies, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419816904576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimation of ground deformation caused by the earthquake (M7.2) in Japan, 2008, from the geomorphic image analysis of high resolution LiDAR DEMs"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893296173312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geometry and kinematics of fault-bend folding"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893384486912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Surface rupturing earthquakes repeated in the 300 years along the ISTL active fault system, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895348410496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A 21-Event, 4,000-Year History of Surface Ruptures in the Anza Seismic Gap, San Jacinto Fault, and Implications for Long-term Earthquake Production on a Major Plate Boundary Fault"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845153958272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coseismic fold scarps and their kinematic behavior in the 1999 Chi‐Chi earthquake Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318381077632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slip history of the 1944 Bolu‐Gerede earthquake rupture along the North Anatolian fault system: Implications for recurrence behavior of multisegment earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319361016576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quaternary Climate Change and the Formation of River Terraces across Growing Anticlines on the North Flank of the Tien Shan, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320922659968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic reflection profiling across the seismogenic fault of the 1995 Kobe earthquake, southwestern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794342661504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coseismic fault‐related fold model, growth structure, and the historic multisegment blind thrust earthquake on the basement‐involved Yoro thrust, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794792148736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Why blind thrust faults do not propagate to the Earth's surface: Numerical modeling of coseismic deformation associated with thrust‐related anticlines"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795694290688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantitative Refinement of Calibrated<sup>14</sup>C Distributions"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230235392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Destructive Earthquake: Forecast and Disaster Prevention Measures. Significance of Imaging Seismogenic and Active Fault Systems for Earthquake Hazard Mitigation."},{"@value":"地震災害を考える　　予測と対策　　震源断層‐活断層システムのイメージングの意義と現状"},{"@language":"ja-Kana","@value":"シンゲン ダンソウ カツダンソウ システム ノ イメージング ノ イギ ト ゲンジョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303262336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rupture Process of the April 11, 2011 Fukushima Hamadori Earthquake (<I>M</I><SUB>j</SUB> 7.0)"},{"@language":"ja","@value":"2011年4月11日福島県浜通りの地震（<I>M</I><SUB>j</SUB>7.0）の震源過程"},{"@value":"Rupture Process of the April 11, 2011 Fukushima Hamadori Earthquake (Mj 7.0)"},{"@value":"Rupture process of the April 11, 2011 Fukushima Hamadori earthquake (Mj 7.0) —two fault planes inferred from strong motion and relocated aftershocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205349640576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"SEISMIC DISPLACEMENT 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