{"@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/1363388844569174912.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0040-1951(99)00297-8"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195199002978?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195199002978?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"80011711155"}}],"dc:title":[{"@value":"Three-dimensional attenuation structure beneath the northeastern Japan arc estimated from spectra of small earthquakes"}],"description":[{"notation":[{"@value":"Abstract   A fine-scale three-dimensional attenuation structure beneath the northeastern Japan arc has been obtained using a joint inversion for source parameters, site response and Q values. Data used for this study are P wave spectra of microearthquakes occurring in the subducting Pacific plate. The subducting plate is found to have higher Q values than the overlying mantle. There is an along-arc variation in the distribution of low-Q zones in the crust and the mantle wedge within the study area. For the southern part of the study area, low-Q zones are distributed in the crust beneath the volcanic front. They extend into the mantle wedge and become deep toward the west, that is, toward the backarc region. On the other hand, the northern part of the study area has low-Q zones at two depth ranges; at shallower depths just beneath the volcanic front and at the deeper part of the mantle wedge beneath the backarc region. The region without active volcanoes along the volcanic front has relatively high mantle Q values. Seismic activity in the lower plane of the double-planed deep seismic zone is high beneath this relatively high-Q region of the mantle wedge. Spatial distribution of low-Q zones found in the present study is nearly consistent with that of the low-velocity zones estimated from studies of travel times tomography. Partial melting zones in the mantle wedge, whose existence has been suggested from the study of seismic velocity structure and laboratory experiments, are located in the low Q zones obtained in the present study. These results suggest that spatial distribution of Q values is closely related to heterogeneous distribution of temperature in the mantle wedge."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1580009751809493888","@type":"Researcher","foaf:name":[{"@value":"N. Tsumura"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844569174914","@type":"Researcher","foaf:name":[{"@value":"S. Matsumoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844569174913","@type":"Researcher","foaf:name":[{"@value":"S. Horiuchi"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844569174912","@type":"Researcher","foaf:name":[{"@value":"A. Hasegawa"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2000-04","prism:volume":"319","prism:number":"4","prism:startingPage":"241","prism:endingPage":"260"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0040195199002978?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0040195199002978?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2025-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050845760702676096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Direct estimation of near-surface damping based on normalized energy density"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229801701248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along‐arc variation in the 3‐D thermal structure around the junction between the Japan and Kurile arcs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232173877504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic anisotropy tomography: New insight into subduction dynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523299840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheological structure of northeastern Japan lithosphere based on geophysical observations and rock mechanics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691152066304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheological contrast between serpentine species and implications for slab–mantle wedge decoupling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704777524736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic attenuation beneath northeastern Japan: Constraints on mantle dynamics and arc magmatism"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704779118208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detailed seismic attenuation structure beneath Hokkaido, northeastern Japan: Arc‐arc collision process, arc magmatism, and seismotectonics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500020224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Autocorrelation analysis of ambient noise in northeastern Japan subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711231218944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of late Cenozoic magmatism and the crust–mantle structure in the NE Japan Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565167509823744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A water wall in the Tohoku forearc causing large crustal earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168144255488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial distribution of scattering loss and intrinsic absorption of short-period<i>S</i>waves in the lithosphere of Japan on the basis of the Multiple Lapse Time Window Analysis of Hi-net data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088993664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"P-wave attenuation in the Pacific slab beneath northeastern Japan revealed by the spectral ratio of intraslab earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185523045632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional attenuation structure of intrinsic absorption and wide-angle scattering of S waves in northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232380379648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Moho, slab and tomography of the East Japan forearc derived from seafloor S-net data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584341811226880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic anisotropy and geodynamics of the East Japan subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641639157632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Experimental study of attenuation and dispersion over a broad frequency range: 1. The apparatus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657103918720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magma genesis beneath Northeast Japan arc: A new perspective on subduction zone magmatism"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657254682240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Complex slab structure and arc magmatism beneath the Japanese Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658218875520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Experimental study of attenuation and dispersion over a broad frequency range: 2. The universal scaling of polycrystalline materials"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660499608960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Envelope broadening characteristics of crustal earthquakes in northeastern Honshu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848661269048832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical Resistivity Structure and Helium Isotopes around Naruko Volcano, Northeastern Japan and Its Implication for the Distribution of Crustal Magma"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707157648384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along-arc heterogeneous rheology inferred from post-seismic deformation of the 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412893259515776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Arc-arc collision caused the 2018 Eastern Iburi earthquake (M 6.7) in Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204229981952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismological Imaging of the Mantle Wedge Structure beneath the Northeastern Japan Arc and its Interpretation"},{"@language":"ja","@value":"東北日本弧下のマントルウエッジの地震学的構造とその解釈"},{"@language":"ja-Kana","@value":"トウホク ニホン コカ ノ マントル ウエッジ ノ ジシンガクテキ コウゾウ ト ソノ カイシャク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230485248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Review of the Mechanical Properties of Solid-liquid Composites"},{"@value":"固液複合系の力学物性"},{"@language":"ja-Kana","@value":"コエキ フクゴウケイ ノ リキガク ブッセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303080960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"西南日本の三次元P波減衰構造"},{"@language":"en","@value":"Three-dimensional P-wave Attenuation Structure beneath Southwest Japan"},{"@language":"ja-Kana","@value":"セイナン ニホン ノ サンジゲン Pハ ゲンスイ コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204304016256","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional Attenuation Structure beneath the Tokai Region, Central Japan Derived Using Local Earthquake Spectra"},{"@value":"東海地域下の三次元地震波減衰構造"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204304599552","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source Effects of the Intraslab and Interplate Earthquakes off Miyagi Prefecture in Northeastern Japan Based on Spectral Inversion"},{"@language":"ja","@value":"スペクトルインバージョンに基づく宮城県沖のスラブ内地震とプレート境界地震の震源特性"},{"@language":"ja-Kana","@value":"スペクトルインバージョン ニ モトズク ミヤギケンオキ ノ スラブ ナイ ジシン ト プレート キョウカイ ジシン ノ シンゲン トクセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204305498880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"北海道および東北日本沈み込み帯におけるS波偏向異方性とマントルウェッジ内の二次対流"},{"@language":"en","@value":"Shear-wave Polarization Anisotropy and Upwelling Flow in the Mantle Wedge beneath Hokkaido and Tohoku, Japan"},{"@language":"ja-Kana","@value":"ホッカイドウ オヨビ トウホク ニホン シズミ コミ タイ ニ オケル Sハ ヘンコウ イホウセイ ト マントルウェッジ ナイ ノ 2ジ タイリュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204305811328","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"2001年芸予地震の強震動分布と深部地下構造"},{"@language":"en","@value":"The Distribution of Strong Ground Motion from the 2001 Geiyo Earthquake and the Deep Underground Structure"},{"@language":"ja-Kana","@value":"2001ネン ゲイヨ ジシン ノ キョウシンドウ ブンプ ト シンブ チカ コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240339712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rheological profile across the northeastern Japan lithosphere toward precise modeling of the 2011 Tohoku Oki Earthquake"},{"@language":"ja","@value":"東日本太平洋沖地震後の余効変動解析へ向けた東北日本弧レオロジー断面"},{"@language":"ja-Kana","@value":"ヒガシニホン タイヘイヨウオキ ジシン ゴ ノ ヨコウヘンドウ カイセキ エ ムケタ トウホク ニホン コ レオロジー ダンメン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496172928","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"微小地震スペクトルを用いたQトモグラフィ<br/>—震源パラメターとQ値の同時推定法の中越地震震源域への適用例—"},{"@language":"en","@value":"<i>Q</i> Tomography using small earthquake spectra<br/>—Application of combined inversion of source parameters and <i>Q</i> values to the data derived in the 2004 Mid-Niigata earthquake source region—"},{"@value":"微小地震スペクトルを用いたQトモグラフィ--震源パラメターとQ値の同時推定法の中越地震震源域への適用例"},{"@language":"ja-Kana","@value":"ビショウ ジシン スペクトル オ モチイタ Qトモグラフィ シンゲン パラメター ト Qチ ノ ドウジ スイテイホウ ノ チュウエツ ジシン シンゲンイキ エ ノ テキヨウ レイ"},{"@value":"<i>Q</i> Tomography using small earthquake spectra<br/>&mdash;Application of combined inversion of source parameters and <i>Q</i> values to the data derived in the 2004 Mid-Niigata earthquake source region&mdash;"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496439296","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地殻・上部マントルでの減衰<br/>─トモグラフィ手法によるQ値評価とその利用─"},{"@language":"en","@value":"Attenuation structure at crust and upper mantle<br/>—Estimation of Q<sub>s</sub>-value by tomographic analysis and its applications—"},{"@value":"地殻・上部マントルでの減衰 : トモグラフィ手法によるQ値評価とその利用"},{"@language":"ja-Kana","@value":"チカク ・ ジョウブ マントル デ ノ ゲンスイ : トモグラフィ シュホウ ニ ヨル Qチ ヒョウカ ト ソノ リヨウ"},{"@value":"Attenuation structure at crust and upper mantle<br/>&mdash;Estimation of Q<sub>s</sub>-value by tomographic analysis and its applications&mdash;"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496703232","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"P wave attenuation structure by spectral inversion of seismic waveforms"},{"@language":"ja","@value":"スペクトルインヴァージョンによるP波減衰構造"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512652288","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Two-layer Qs structure of the slab near the southern Kurile trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1390016117753728768","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Intrinsic Attenuation Structure of the Mantle Wedge beneath Hokkaido, Japan, Inferred from Seismic Wave Propagation Simulations of Deep-focus Earthquake"},{"@language":"ja","@value":"深発地震の地震波動伝播シミュレーションに基づく北海道下マントルウェッジの内部減衰構造"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679121738240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic imaging of mantle wedge corner flow and arc magmatism"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679281358080","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東北日本弧下のマグマ供給源の分布 : b値とS波速度から推定される島弧走向方向の変化"},{"@language":"en","@value":"Along-arc Variation of Magma Source in the Subducted Slab beneath the NE Japan Arc : Estimation from b-value and S-wave Velocity Distributions"},{"@value":"寄書 東北日本弧下のマグマ供給源の分布--b値とS波速度から推定される島弧走行方向の変化"},{"@language":"ja-Kana","@value":"キショ トウホク ニホン コ カ ノ マグマ キョウキュウ ゲン ノ ブンプ bチ ト Sハ ソクド カラ スイテイ サレル シマ コ ソウコウ ホウコウ ノ ヘンカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679282207232","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"震度データから検証する宮城県沖で発生する被害地震の繰り返し"},{"@language":"en","@value":"Verification of the Sequence of Disastrous Earthquakes off Miyagi Prefecture Based on Seismic Intensity Data"},{"@language":"ja-Kana","@value":"シンド データ カラ ケンショウ スル ミヤギケンオキ デ ハッセイ スル ヒガイ ジシン ノ クリカエシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680313423872","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geophysical techniques for detecting magmas and high-temperature fluids;"},{"@language":"ja","@value":"地下深部のマグマ・高温流体等の地球物理学的調査技術"},{"@value":"地下深部のマグマ・高温流体等の地球物理学的調査技術--鬼首・鳴子火山地域および紀伊半島南部地域への適用"},{"@language":"ja-Kana","@value":"チカ シンブ ノ マグマ コウオン リュウタイ トウ ノ チキュウ ブツリガクテキ チョウサ ギジュツ オニコウベ ナルゴ カザン チイキ オヨビ キイハントウ ナンブ チイキ エ ノ テキヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473380352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evolution of Late Cenozoic Magmatism in the NE Honshu Arc and Its Relation to the Crust-Mantle Structures"},{"@value":"後期新生代，東北本州弧における火成活動史と地殻・マントル構造"},{"@language":"ja-Kana","@value":"コウキ シンセイダイ トウホクホンシュウ コ ニ オケル カセイカツドウシ ト チカク マントル コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417119872384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geological structures controlled the rupture process of the 2011 M9.0 Tohoku-Oki earthquake in the Northeast Japan Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266985502336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Attenuation contrast in mantle wedge across the volcanic front of northeastern Japan that controls propagations of high-frequency S-wave later phases"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/s0040-1951(99)00297-8"},{"@type":"CIA","@value":"80011711155"},{"@type":"OPENAIRE","@value":"doi_dedup___::0a30d1310080009cb197efd22d66a9f7"},{"@type":"CROSSREF","@value":"10.1002/2014gc005394_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2011.03.002_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.3124/segj.58.617_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.4294/zisin.67.57_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2013.08.027_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2011.09.019_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0026_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1002/2013jb010388_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1002/2014jb011099_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1144/sp385.15_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2018.02.032_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.3327/jnuce.11.147_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.4294/zisin.67.105_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01361-z_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.4294/zisin.2022-19_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1093/gji/ggu381_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2009.04394.x_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1186/bf03351952_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1093/gji/ggt104_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2012.05438.x_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2009.05.006_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.5026/jgeography.117.76_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.4294/zisin.65.175_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2022.229452_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1016/j.jog.2023.101975_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1029/2011jb008382_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1029/2011jb008384_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2010.04657.x_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1155/2010/738139_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2012.12.031_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.3124/segj.63.509_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01212-3_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1093/gji/ggac063_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2015.05.008_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.1038/s41598-019-50305-x_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.3124/segj.65.67_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"},{"@type":"CROSSREF","@value":"10.2183/pjab.94.015_references_DOI_9QlWL6uI1HlTglWqRPOWp7f1ecW"}]}