{"@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/1363670319612006784.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/95jb03446"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F95JB03446"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/95JB03446"}}],"dc:title":[{"@value":"Poisson's ratio and crustal seismology"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>New measurements of compressional and shear wave velocities to hydrostatic pressures of 1 GPa are summarized for 678 rocks. Emphasis was placed on obtaining high‐accuracy velocity measurements, which are shown to be critical in calculating Poisson's ratios from velocities. The rocks have been divided into 29 major groups for which velocities, velocity ratios, and Poisson's ratios are presented at several pressures. Observed Poisson's ratios for the monomineralic rocks compare favorably with theoretical Poisson's ratios calculated from single‐crystal elastic constants. Plagioclase feldspar composition is important in understanding rock Poisson's ratios, since Poisson's ratio of albite increases from 0.28 to a predicted value of 0.31 for anorthite. Fe substitution for Mg in pyroxene and olivine also increases Poisson's ratio. Plotting rock compressional wave velocities versus Poisson's ratios reveals a triangular distribution bounded by quartzite with low compressional wave velocity and low Poisson's ratio, dunite with high compressional wave velocity and intermediate Poisson's ratio, and serpentinite with low compressional wave velocity and high Poisson's ratio. For common plutonic igneous rocks, there is a clear trend relating Poisson's ratio to composition, in which Poisson's ratio for granitic rocks increases from 0.24 to 0.29 as composition changes to gabbro and then decreases with decreasing plagioclase and increasing olivine contents to 0.25 in dunite. Changes in Poisson's ratio with progressive metamorphism of mafic and pelitic rocks correlate reasonably well with mineral reactions. There is no simple correlation between Poisson's ratio and felsic and mafic rock compositions; however, a linear correlation of increasing Poisson's ratio with decreasing SiO<jats:sub>2</jats:sub> content is observed for rocks with 55 to 75 wt % SiO<jats:sub>2</jats:sub>. Average Poisson's ratios for continental and oceanic crusts are estimated to be 0.265 and 0.30, respectively.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670319612006784","@type":"Researcher","foaf:name":[{"@value":"Nikolas I. Christensen"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1996-02-10","prism:volume":"101","prism:number":"B2","prism:startingPage":"3139","prism:endingPage":"3156"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F95JB03446"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/95JB03446"}],"createdAt":"2004-02-04","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570393792000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tomographic image of crust and upper mantle off the Boso Peninsula using data from an ocean-bottom 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mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869856025976192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Insight into drilling performance parameters for in-situ detection of lithological transition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869856030331776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic discontinuity in the Martian crust possibly caused by water-filled cracks"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204229977728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Elemental Mobilizations during Hydrothermal Alteration of Oceanic Lithosphere"},{"@language":"ja","@value":"海洋リソスフェアの熱水変質に伴う元素移動"},{"@value":"海洋リンスフェアの熱水変質に伴う元素移動 (特集号 地殻からマントルへ : モホ(面)とは何か?)"},{"@value":"海洋リンスフェアの熱水変質に伴う元素移動"},{"@language":"ja-Kana","@value":"カイヨウ リンスフェア ノ ネッスイ ヘンシツ ニ トモナウ ゲンソ イドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204304147456","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-Dimensional Velocity Structure and Configuration of the Philippine Sea Slab beneath Kanto District, Central Japan, Estimated by Double-Difference Tomography"},{"@language":"ja","@value":"Double-Difference Tomography法による関東地方の3次元地震波速度構造およびフィリピン海プレートの形状の推定"},{"@language":"ja-Kana","@value":"Double Difference Tomographyホウ ニ ヨル カントウ チホウ ノ 3ジゲン ジシンハ ソクド コウゾウ オヨビ フィリピンカイ プレート ノ ケイジョウ ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511586176","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional structure of V<SUB>p</SUB>, V<SUB>s</SUB> and V<SUB>p</SUB>/V<SUB>s</SUB> in the upper crust of the Marmara region, NW Turkey"},{"@value":"Three-dimensional structure of Vp, Vs and Vp/Vs in the upper crust of the Marmara region, NW Turkey"},{"@value":"The three-dimensional structure of Vp, Vs and Vp/Vs in the upper crust of the Marmara region, NW Turkey"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511885696","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal heterogeneity around the Nagamachi-Rifu fault, northeastern Japan, as inferred from travel-time tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679206568448","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"海洋モホ面形成におけるダナイトの役割"},{"@language":"en","@value":"Role of Dunite in the Formation of the Oceanic Mohorovicic Discontinuity"},{"@language":"ja-Kana","@value":"カイヨウ モホメン ケイセイ ニ オケル ダナイト ノ ヤクワリ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279748096","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic Velocity and Electrical Conductivity of Rocks in the Crust and Mantle: Probing Water in Subduction Zones"},{"@language":"ja","@value":"地殻・マントル物質の地震波速度と電気伝導度：沈み込み帯の水を探る"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679281093888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Inference of Shallow Crustal Materials in the Atotsugawa Fault Area Based on Measurements of Elastic Wave Velocities"},{"@language":"ja","@value":"弾性波速度測定に基づく跡津川断層周辺浅部地殻物質の推定"},{"@language":"ja-Kana","@value":"ダンセイハ ソクド ソクテイ ニ モトズク アト ツガワ ダンソウ シュウヘンセンブ チカク ブッシツ ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489345792","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Regional and 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