{"@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/1363670319251317632.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1017/cbo9781107297562"}}],"dc:title":[{"@value":"Deep Earthquakes"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Deep earthquakes (earthquakes with origins deeper than 60 km) are of scientific importance and account for approximately one-quarter of all earthquakes. They are occasionally very large and damaging yet provide much of the data that constrain our knowledge of Earth structure and dynamics. This book opens with an explanation of what deep earthquakes are, their significance to science and how they were first discovered. Later chapters provide a description of deep earthquake distribution and clustering in both time and space; a review of observations about source properties; and a discussion of theories for the origin of deep earthquakes. The book concludes with a comprehensive literature review of terrestrial and lunar deep seismicity. Deep Earthquakes presents a comprehensive, topical, historical, and geographical summary of deep earthquakes and related phenomena. It will be of considerable interest to researchers and graduate students in the fields of earthquake seismology and deep Earth structure.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670319251317632","@type":"Researcher","foaf:name":[{"@value":"Cliff Frohlich"}]}],"publication":{"publicationIdentifier":[{"@type":"ISBN","@value":"9780521828697"},{"@type":"ISBN","@value":"9780521123969"},{"@type":"ISBN","@value":"9781107297562"}],"dc:publisher":[{"@value":"Cambridge University Press"}],"prism:publicationDate":"2006-05-04"},"reviewed":"false","dc:rights":["https://www.cambridge.org/core/terms"],"createdAt":"2013-08-05","modifiedAt":"2022-10-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232324688896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic imaging of the Asian orogens and subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302866836299136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Anti-repeating earthquakes and how to explain them"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567180128688640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"An intraslab seismic sequence activated by the 2011 Tohoku‐oki earthquake: Evidence for fluid‐related embrittlement"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092633511808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slow deformation event between large intraslab earthquakes at the Tonga Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567832189952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Preseismic and Postseismic Phases of the 700‐km Deep M7.9 Bonin Islands Earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694368033674240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Significance of Long‐Period Ground Motion at Regional to Teleseismic Distances From the 610‐km Deep <i>M</i><sub><i>w</i></sub> 8.3 Sea of Okhotsk Earthquake of 24 May 2013"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204237718400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"沈み込み帯の地震の発生機構"},{"@language":"en","@value":"Mechanism Generating Earthquakes in Subduction Zones"},{"@value":"沈み込み帯の地震の発生機構 : 地殻流体に規定されて発生する沈み込み帯の地震"},{"@language":"ja-Kana","@value":"シズミ コミ タイ ノ ジシン ノ ハッセイ キコウ : チカク リュウタイ ニ キテイ サレテ ハッセイ スル シズミ コミ タイ ノ ジシン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390017965044104832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Kawai-type multianvil ultrahigh-pressure technology"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791869811968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic imaging of slab metamorphism and genesis of intermediate-depth intraslab earthquakes"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1017/cbo9781107297562"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2017.06.016_references_DOI_U3kTcFGIqS9vzFS3kFhzlQsWsT5"},{"@type":"CROSSREF","@value":"10.1038/s43247-024-01290-1_references_DOI_U3kTcFGIqS9vzFS3kFhzlQsWsT5"},{"@type":"CROSSREF","@value":"10.1002/jgrb.50246_references_DOI_U3kTcFGIqS9vzFS3kFhzlQsWsT5"},{"@type":"CROSSREF","@value":"10.1038/s41598-020-80728-w_references_DOI_U3kTcFGIqS9vzFS3kFhzlQsWsT5"},{"@type":"CROSSREF","@value":"10.1186/s40645-017-0126-9_references_DOI_U3kTcFGIqS9vzFS3kFhzlQsWsT5"},{"@type":"CROSSREF","@value":"10.5026/jgeography.121.128_references_DOI_U3kTcFGIqS9vzFS3kFhzlQsWsT5"},{"@type":"CROSSREF","@value":"10.1029/2019gl085589_references_DOI_U3kTcFGIqS9vzFS3kFhzlQsWsT5"},{"@type":"CROSSREF","@value":"10.2183/pjab.100.013_references_DOI_U3kTcFGIqS9vzFS3kFhzlQsWsT5"},{"@type":"CROSSREF","@value":"10.1029/2019jb018147_references_DOI_U3kTcFGIqS9vzFS3kFhzlQsWsT5"}]}