{"@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/1360004229807854720.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2017gl074060"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL074060"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL074060"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL074060"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL074060"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Tidal Response in Shallow Tectonic Tremors"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Various types of slow earthquakes (e.g., tectonic tremors and slow slip events) have been reported in tectonic zones, especially in the subduction zone. The tidal response of a tremor is considered to be strongly related to the weak friction state of the plate interface, and many studies have reported observational evidence of such correlation between tides and deep tremor activity. Here we used the modified frequency scanning method at a single station to detect micro tectonic tremors that have not been previously reported in southern Kyushu. In the early stage of the tremor activity, tremors are mostly modulated by slow slip events. In contrast, we found a seismic response to ocean tides during the later stage in the shallower part of the subduction zone. This might indicate that the tremors are triggered by tidal changes caused by fault weakening due to slow slip events as same as deeper condition.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004229807854851","@type":"Researcher","foaf:name":[{"@value":"S. Katakami"}],"jpcoar:affiliationName":[{"@value":"Division of Earth and Planetary Sciences Kyoto University  Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229807854852","@type":"Researcher","foaf:name":[{"@value":"Y. Yamashita"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute Kyoto University  Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229807854720","@type":"Researcher","foaf:name":[{"@value":"H. Yakiwara"}],"jpcoar:affiliationName":[{"@value":"Nansei‐Toko Observatory for Earthquakes and Volcanoes, Graduate School of Science and Engineering Kagoshima University  Kagoshima Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229807854848","@type":"Researcher","foaf:name":[{"@value":"H. Shimizu"}],"jpcoar:affiliationName":[{"@value":"Institute of Seismology and Volcanology (SEVO), Faculty of Sciences Kyushu University  Shimabara Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229807854849","@type":"Researcher","foaf:name":[{"@value":"Y. Ito"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute Kyoto University  Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229807854721","@type":"Researcher","foaf:name":[{"@value":"K. Ohta"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute Kyoto University  Kyoto Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2017-10-13","prism:volume":"44","prism:number":"19","prism:startingPage":"9699","prism:endingPage":"9706"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL074060"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL074060"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL074060"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL074060"}],"createdAt":"2017-09-26","modifiedAt":"2023-09-03","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781862646400","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K17745"},{"@type":"JGN","@value":"JP15K17745"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K17745/"}],"notation":[{"@language":"ja","@value":"南海トラフにおける浅部低周波微動活動の履歴と特徴の解明"},{"@language":"en","@value":"Elucidation of activity for shallow low-frequency tremor in Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781962844928","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"17K01328"},{"@type":"JGN","@value":"JP17K01328"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-17K01328/"}],"notation":[{"@language":"ja","@value":"浅部スロー地震域は津波波源域？1662年日向灘地震津波の地球物理学・地質学的検証"},{"@language":"en","@value":"Is the Focal Region of the Shallow Slow Earthquake a Tsunami Source Area? A Geophysical and Geological Study of the 1662 Hyuga-nada Earthquake Tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782277971584","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26000002"},{"@type":"JGN","@value":"JP26000002"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26000002/"}],"notation":[{"@language":"ja","@value":"深海調査で迫るプレート境界浅部すべりの謎～その過去・現在"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256879561344","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H06473"},{"@type":"JGN","@value":"JP16H06473"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-16H06473/"}],"notation":[{"@language":"ja","@value":"海陸機動的観測に基づくスロー地震発生様式の解明"},{"@language":"en","@value":"Study on the Mechanisms Ivolved in the Occurrence of Slow Earthquakes Based on Temporal Inland and Offshore Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257255897216","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26109002"},{"@type":"JGN","@value":"JP26109002"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-26109002/"}],"notation":[{"@language":"ja","@value":"内陸地殻の強度と応力の解明"},{"@language":"en","@value":"Clarification of strength and stress of the inland crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257259871104","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26257206"},{"@type":"JGN","@value":"JP26257206"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26257206/"}],"notation":[{"@language":"ja","@value":"沈み込み帯浅部のスロースリップはトラフ軸まで到達するか？"},{"@language":"en","@value":"Slow slip to the trench  ?"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202761516800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dynamic deformation of the accretionary prism excites very low frequency earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001339107234432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Connecting slow earthquakes to huge earthquakes"},{"@value":"Connecting slow earthquakes to large earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282810792973312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Episodic tremor and slip near the Japan Trench prior to the 2011 Tohoku-Oki earthquake"},{"@value":"Episodic tremor and slip near the Japan Trench prior to the 2011 Tohoku‐Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235955794048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slow slip near the trench at the Hikurangi subduction zone, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142419703168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Ocean's Impact on Slow Slip Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144574343040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Very low frequency earthquakes off the Pacific coast of Tohoku, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145299277696","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Comparison of the coseismic rupture with the aftershock distribution in the Hyuga‐nada Earthquakes of 1996"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146029635072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Short‐term slow slip and correlated tremor episodes in the Tokai region, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708269006208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal Variation of Tectonic Tremor Activity Before the Tohoku‐Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617909770624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nonvolcanic Deep Tremor Associated with Subduction in Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619531072896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The synchronous occurrence of shallow tremor and very low frequency earthquakes offshore of the Nicoya Peninsula, Costa Rica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620347635840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Statistical test of the tidal triggering of earthquakes: contribution of the ocean tide loading effect"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168402592768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Migrating tremor off southern Kyushu as evidence for slow slip of a shallow subduction interface"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183240083328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A slip pulse model with fault heterogeneity for low‐frequency earthquakes and tremor along plate interfaces"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092886026112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Generic Mapping Tools: Improved Version Released"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092886258944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low-frequency earthquakes in Shikoku, Japan, and their relationship to episodic tremor and slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093963187840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An earthquake‐like magnitude‐frequency distribution of slow slip in northern Cascadia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340508721536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal Distribution of Shallow Tremors Along the Nankai Trough, Southwest Japan, as Determined From Waveform Amplitudes and Cross‐Correlations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641728624512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Striations, duration, migration and tidal response in deep tremor"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993924969984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatio‐temporal variation of the tidal triggering effect on earthquake occurrence associated with the 1982 South Tonga earthquake of Mw 7.5"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370575859840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low‐frequency continuous tremor around the Moho discontinuity away from volcanoes in the southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370947380352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low friction and fault weakening revealed by rising sensitivity of tremor to tidal stress"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843997021312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Segmentation in episodic tremor and slip all along Cascadia"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844242379392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844667273600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slip rate and tremor genesis in Cascadia"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321123220224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mechanism of deep low frequency earthquakes: Further evidence that deep non‐volcanic tremor is generated by shear slip on the plate interface"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793844016640","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rapid, continuous streaking of tremor in Cascadia"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793876146816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slow slip events and seismic tremor at circum‐Pacific subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268877534592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source characteristics of the 1992 Nicaragua tsunami earthquake inferred from teleseismic body waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1370004229807854592","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Detecting tectonic tremor through frequency scanning at a single station: Application to the Cascadia margin, Earth Planet"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512583680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Very low frequency earthquakes excited by the 2004 off the Kii peninsula earthquakes: A dynamic deformation process in the large accretionary prism"},{"@value":"Very low frequency earthquake excited by the 2004 off the Kii peninsula earthquake: a dynamic deformation process in the large accretionary prism"},{"@value":"Very low frequency earthquakes excited by the 2004 off Kii peninsula earthquakes: a dynamic deformation process in the large accretionary prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489624960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Repeating short- and long-term slow slip events with deep tremor activity around the Bungo channel region, southwest Japan"},{"@value":"Repeating short- and long-term slow slip events with deep tremor activity around Bungo channel region, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1520854805118488704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ocean Tide Models Developed by Assimilating TOPEX/POSEIDON Altimeter Data into Hydrodynamical Model:A Global Model and a Regional Model around Japan"},{"@language":"ja-Kana","@value":"Ocean Tide Models Developed by Assimilating TOPEX POSEIDON Altimeter Data into Hydrodynamical Model A Global Model and a Regional Model around Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854175844018560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source process of the Hyuga-nada Earthquake of April 1, 1968 (Mjma 7.5), and its relationship to the subsequent seismicity"},{"@value":"Source process of the Hyuga‐nada Earthquake of April 1, 1968 (M\n                  JMA 7.5), and its relationship to the subsequent seismicity"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417124529847168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effects of the Long-period Ocean Tide on Earth Rotation, Gravity and Crustal Deformation Predicted by Global Barotropic Model-periods from Mtm to Sa-"},{"@value":"Effects of the long period ocean tides on earth rotation, gravity and crustal deformation predicted by global barotropic model—Periods from Mtm to Sa"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367085226240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Discriminating seismic events using 1D and 2D CNNs : applications to volcanic and tectonic datasets"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317020017024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatio-temporal changes in the seismic velocity induced by the 2011 Tohoku-Oki earthquake and slow slip event revealed from seismic interferometry, using ocean bottom seismometer’s records"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996267023639040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Regional and global variations in the temporal clustering of tectonic tremor activity"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2017gl074060"},{"@type":"KAKEN","@value":"PRODUCT-21905965"},{"@type":"KAKEN","@value":"PRODUCT-21454926"},{"@type":"KAKEN","@value":"PRODUCT-21933739"},{"@type":"KAKEN","@value":"PRODUCT-21625980"},{"@type":"KAKEN","@value":"PRODUCT-21647202"},{"@type":"KAKEN","@value":"PRODUCT-21697940"},{"@type":"OPENAIRE","@value":"doi_dedup___::deb14342f5daecc15566943551ece89c"},{"@type":"CROSSREF","@value":"10.1029/2020gl087273_references_DOI_TxVePGVPD95l7BNvHv0mGH9fLNp"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01696-1_references_DOI_TxVePGVPD95l7BNvHv0mGH9fLNp"},{"@type":"CROSSREF","@value":"10.1029/2018jb016651_references_DOI_TxVePGVPD95l7BNvHv0mGH9fLNp"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0240-3_references_DOI_TxVePGVPD95l7BNvHv0mGH9fLNp"},{"@type":"CROSSREF","@value":"10.1029/2022jb024403_references_DOI_TxVePGVPD95l7BNvHv0mGH9fLNp"}]}