{"@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/1363670319515179136.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2000jb900386"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000JB900386"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000JB900386"}}],"dc:title":[{"@value":"Spatial distribution of focal mechanisms for interplate and intraplate earthquakes associated with the subducting Pacific plate beneath the northeastern Japan arc: A triple‐planed deep seismic zone"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The northeastern Japan arc is located in one of the most seismically active subduction zones in the world. In this study, we relocated hypocenters and determined focal mechanisms of small earthquakes (<jats:italic>M</jats:italic>≤5) beneath the arc in order to investigate in detail the stress distribution in and around the descending oceanic plate. In the hypocenter relocation we adopted a “source region station correction method” in which station corrections vary with hypocenter locations. We have developed a new focal mechanism determination technique named “master solution method,” which is analogous to the “master event method” in hypocenter determination. We applied the method to <jats:italic>P</jats:italic> and <jats:italic>SH</jats:italic> wave amplitude data to obtain 1106 focal mechanism solutions. From the new mechanism solutions and relocated hypocenters we found that there occur both low‐angle thrust fault (LT) type and downdip compression (DC) type earthquakes at depths from 40 to 70 km near the aseismic front; the DC type events are underlying the LT‐type events. Almost all the earthquake clusters are composed of LT‐type events. The western limit of the region where LT‐type events have occurred is subparallel to the trench axis, although it undulates considerably; it delineates the westernend of the active region of interplate seismicity. Furthermore, we found that normal fault (NF) type events also occur at depths from 70 km in the upper plane of the double‐planed deep seismic zone, which is characterized mainly by DC‐type event. These NF‐type events are distributed only in a thin uppermost portion of the slab close to the plate boundary. Below these, in the lower plane, are downdip extension (DE) type events. This result indicates that the deep seismic zone in the northeastern Japan arc is not double‐planed but triple‐planed, even beneath the land area, which cannot be explained by any simple models.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670319515179137","@type":"Researcher","foaf:name":[{"@value":"Toshihiro Igarashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319515179138","@type":"Researcher","foaf:name":[{"@value":"Toru Matsuzawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319515179008","@type":"Researcher","foaf:name":[{"@value":"Norihito Umino"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319515179136","@type":"Researcher","foaf:name":[{"@value":"Akira Hasegawa"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2001-02-10","prism:volume":"106","prism:number":"B2","prism:startingPage":"2177","prism:endingPage":"2191"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000JB900386"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000JB900386"}],"createdAt":"2004-02-03","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050294045369553664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fault stress inversion reveals seismogenic asperity of the 2011 Mw 9.0 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708772096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismogenic characteristics of the Northern Mariana shallow thrust zone from local array data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216802652928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seafloor observations indicate spatial separation of coseismic and postseismic slips in the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230122225280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic evidence for high pore pressures in the oceanic crust: Implications for fluid‐related embrittlement"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230362713856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Investigation on the Postseismic Deformation Associated with the 2011 Tohoku Earthquake Based on Terrestrial and Seafloor Geodetic Observations: To Evaluate the Further Seismic Hazard Potential on the Plate Interface Beneath the Northeastern Japanese Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235569500416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Double seismic zone in the North Mariana region revealed by long-term ocean bottom array observation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142423994240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Decade of Lessons Learned from the 2011 Tohoku‐Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168746451584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Prevalence of updip rupture propagation in interplate earthquakes along the Japan trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360022306713932160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Low-frequency earthquakes observed in close vicinity of repeating earthquakes in the brittle upper crust of Hakodate, Hokkaido, northern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691686407040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coseismic slip distribution of the 2011 off the Pacific Coast of Tohoku Earthquake (M9.0) refined by means of seafloor geodetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704781222656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial distribution of the faulting types of small earthquakes around the 2011 Tohoku‐oki earthquake: A comprehensive search using template events"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704783286912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Emergence and disappearance of interplate repeating earthquakes following the 2011 <i>M</i>9.0 Tohoku‐oki earthquake: Slip behavior transition between seismic and aseismic depending on the loading rate"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708262632832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Supraslab earthquake clusters above the subduction plate boundary offshore Sanriku, northeastern Japan: Seismogenesis in a graveyard of detached seamounts?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708263913856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Depth-dependent stress field in and around the Atotsugawa fault, central Japan, deduced from microearthquake focal mechanisms: Evidence for localized aseismic deformation in the downward extension of the fault"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617865614848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Presence of interplate channel layer controls of slip during and after the 2011 Tohoku-Oki earthquake through the frictional characteristics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869642496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal–petrological controls on the location of earthquakes within subducting plates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869690496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structural and thermal control of seismic activity and megathrust rupture dynamics in subduction zones: Lessons from the Mw 9.0, 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165919306752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of regional stress state and Young’s modulus by back analysis of mining-induced deformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662987392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Regional extent of the large coseismic slip zone of the 2011 Mw 9.0 Tohoku‐Oki earthquake delineated by on‐fault aftershocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181859862272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamics of Subducting Slabs: Numerical Modeling and Constraints from Seismology, Geoid, Topography, Geochemistry, and Petrology"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088843904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mantle wedge flow pattern and thermal structure in Northeast Japan: Effects of oblique subduction and 3-D slab geometry"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229812451840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Mw 6.0–6.8 Quasi‐Repeating Earthquakes Off Miyagi, Japan, With Variable Moment Release Patterns Due To a Hidden Adjacent Slip Patch"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580230583958400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The 2021 Mw7.0 and Mw6.7 Miyagi‐Oki Earthquakes Nucleated in a Deep Seismic/Aseismic Transition Zone: Possible Effects of Transient Instability Due To the 2011 Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065441664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Pre- and postseismic slow slip surrounding the 2011 Tohoku-oki earthquake rupture"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815491578112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recurrence intervals for M > 7 Miyagi-ken-Oki earthquakes during an M ~ 9 earthquake cycle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855114417536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stress drops of intermediate-depth intraslab earthquakes beneath Tohoku, northern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361975843010362368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Revisiting Intraslab Earthquakes Beneath Kyushu, Japan: Effect of Ridge Subduction on Seismogenesis"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303056768","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Intraslab Seismicity and its Generation Mechanisms"},{"@language":"ja","@value":"スラブ内地震活動とその発生メカニズム"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205359669760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"宮城県沖のスラブ内地震とプレート境界地震の短周期レベルの推定"},{"@language":"en","@value":"Short-period Spectral Level of Intraplate and Interplate Earthquakes Occurring off Miyagi Prefecture"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513467136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Repeating earthquakes and quasi-static slip on the plate boundary east off northern Honshu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207162752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"日本列島下での沈み込みプロセスの多様性"},{"@language":"en","@value":"Variability of Subduction Processes beneath Japan"},{"@language":"ja-Kana","@value":"ニホン レットウ カ デ ノ シズミ コミ プロセス ノ タヨウセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279731840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Interplate Quasi-Static Slip off Miyagi and Fukushima Prefectures Estimated from Small Repeating Earthquake Data"},{"@language":"ja","@value":"小繰り返し地震解析による宮城・福島県沖プレート境界の準静的すべり"},{"@language":"ja-Kana","@value":"ショウ クリカエシ ジシン カイセキ ニ ヨル ミヤギ フクシマケンオキ プレート キョウカイ ノ ジュンセイテキ スベリ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679281458432","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Relocation of Intermediate-depth Earthquakes beneath the NE Japan Arc by Double-Difference Location Method"},{"@language":"ja","@value":"Double-Difference Location 法による東北日本弧下の稍深発地震の震源再決定"},{"@language":"ja-Kana","@value":"Double-Difference Locationホウ ニ ヨル トウホク ニホン コ カ ノ ショウシンパツ ジシン ノ シンゲン サイケッテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679282533248","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"日本列島周辺の地震クラスター"},{"@language":"en","@value":"Earthquake Clusters in the Japanese Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488595328","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The seismicity, fault structures, and stress field in the seismic gap adjacent to the 2004 Mid-Niigata earthquake inferred from seismological observations"},{"@language":"ja-Kana","@value":"seismicity fault structures and stress field in the seismic gap adjacent to the 2004 Mid Niigata earthquake inferred from seismological observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488752000","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Small repeating earthquakes and interplate creep around the 2005 Miyagi-oki earthquake (M=7.2)"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842060075136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Changes in the b value in and around the focal areas of the M6.9 and M6.8 earthquakes off the coast of Miyagi prefecture, Japan, in 2021"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317068449664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0) estimated based on GPS data : was the asperity in Miyagi-oki ruptured？"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317068451072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coupling coefficient, hierarchical structure, and earthquake cycle for the source area of the 2011 off the Pacific coast of Tohoku earthquake inferred from small repeating earthquake data"}]},{"@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"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791998115840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detection of repeating earthquakes and their application in characterizing slow fault slip"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046925952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A trial derivation of seismic plate coupling by focusing on the activity of shallow slow earthquakes"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2000jb900386"},{"@type":"CROSSREF","@value":"10.1029/2011gc003853_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1038/ncomms13506_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.06.013_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1002/grl.50468_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1007/1345_2015_162_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2010.04799.x_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1038/s41598-019-47992-x_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0284-z_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.05.021_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.5610/jaee.4.1_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1029/2020rg000713_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2021.117306_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1029/2012jb009186_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1186/bf03353087_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.07.006_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1002/2015jb012584_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1002/2016jb013914_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1029/2009jb006797_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1029/2010jb007900_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1016/j.ijrmms.2013.05.007_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2014.06.037_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.4294/zisin.59.287_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.357_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1093/gji/ggaa418_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1038/s41598-021-86020-9_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01511-3_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1029/2012gl052220_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-55_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2015.06.021_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.4294/zisin.2017-4_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1029/2022jb025654_references_DOI_9OHt9NDKmyhtTZfV7LKMTqgtgFs"},{"@type":"CROSSREF","@value":"10.1029/2022jb024887_references_DOI_9OHt9NDKmyhtTZfV7LKMTqgtgFs"},{"@type":"CROSSREF","@value":"10.1186/bf03351988_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1186/bf03352664_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1186/s40645-017-0126-9_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.205_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00566-y_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.21203/rs.3.rs-2035979/v1_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02032-5_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1016/b978-0-444-53802-4.00132-9_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1029/2019jb017869_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.03.022_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"},{"@type":"CROSSREF","@value":"10.4294/zisin.59.1_references_DOI_70Gh1vS8xsGpJiPxDosPcofBexE"}]}