{"@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/1390282679309971968.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4157/grj.31.59"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"9972999"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/9972999"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I9972999"}},{"identifier":{"@type":"NAID","@value":"130003566893"}},{"identifier":{"@type":"NAID","@value":"10012799997"}},{"identifier":{"@type":"NAID","@value":"10003547581"}},{"identifier":{"@type":"NAID","@value":"10003547565"}}],"dc:title":[{"@language":"en","@value":"LANDFORM EVOLUTION OF THE KANTÔ PLAIN"},{"@value":"関東平野の地形発達史"},{"@language":"ja-Kana","@value":"カントウ ヘイヤ ノ チケイ ハッタツシ"}],"description":[{"type":"abstract","notation":[{"@language":"en","@value":"The Kanto Plain, in the central part of which Tokyo is situated, is the largest in Japan. This plain is built by the Quaternary series, marine, fluvial and eolian deposits which are considered to be standard series of the Japanese Quaternary.<br> In this paper, first, the author summarized the previous studies on volcanic ash layers, the so-called “Kanto Loam”, which covered almost all of terrce surfaces of the Kantô Plain, then tried to obtain chronological relationships between all of the volcanic ash layers. In the southern Kanto, the Kanto Loam, a part of which is derived from Mt.Fuji, is divided into four beds, and in the northern Kant, that is derived from Mt. Asama and other many volcanoes, into three or four beds. To correlate volcanic ash beds with each other, it is quite effective to trace the characteristic layers such as pumice, scoria or buried soil beds, and also the heavy mineral compositions of the volcanic ashes (Figs. 2 and 3).<br> Secondly, he described the characteristics of landform surfaces in the plain, and chronological horizon of all of them mainly by using relationships between landform surfaces and the volcanic ash beds (Fig. 8). From the a hove mentioned studies, the five stages of landform surfaces, A(Hollocene in age), Du I (upper most Pleistocene), Du b, Dula, and Dl I (middle or Lower Pleistocene), could be classified accordingly.<br> Thirdly, the palaeogeographical maps of each stage of land form surfaces were illustrated (Fig.9) and the evolution of landform of the Kantô Plain was explaind. As can be seen palaeogeographical maps transgression and regression came into being alternately in the Kantô Plain. The landform evolution of the Kantô Plain was, therefore, mainly caused by these transgressions and regressions, but the distribution and the shapes of the landform surfaces were greatly contorolled by the crustal movements in this region since the middle Pleistocene. Broadly speaking, the plain is a large depositional basin surrounded by up-warped belts, in which the southern hilly land shows the greatest upheaval to more than 300 meters since the middle Pleistocene. But precisely speking, there are three down-warped besins. Of the three, the largest one is in the northern part of the Kanto Plain, the second is located in the south-western part and the third is in the Tokyo Bay."},{"@value":"関東平野の第四紀後半の地形面は,関東ロームを鍵とすることによつて編年することができる.そのためには,まず関東ローム自体の層序区分と対比を行う必要があつた.関東ロームの区分や対比には層位学的,地形学的考察とともに,重鉱物組成の調査が有力な手段として用いられた.関東ロームの編年と,主としてそれにもとつく地形面の編年は第8図に模式化して示されている.この編年によつて,関東平野の地形面は, DlI, DuIa, DuIb, DuI, Aの各面に区分され,その地理的分布は第11図に示された.<br>地形面の編年と地形面の性質あるいはその成因についての考察から,区分された各地形面形成時代の古地理図を描くことができ(第9図),そして,関東平野の発達史の概略を知ることができた.それは第2表に要約されている."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030003658986039690","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60086999"},{"@type":"NRID","@value":"1000060086999"},{"@type":"NRID","@value":"9000004596133"},{"@type":"NRID","@value":"9000021567811"},{"@type":"NRID","@value":"9000255735281"},{"@type":"NRID","@value":"9000254752968"},{"@type":"NRID","@value":"9000002496399"},{"@type":"NRID","@value":"9000253273066"}],"foaf:name":[{"@language":"en","@value":"KAIZUKA Sôhei"},{"@language":"ja","@value":"貝塚 爽平"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geographical Institute, Tokyo Metropolitan Univ. ersity"},{"@language":"ja","@value":"東京都立大学理学部地理教室"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167444"},{"@type":"EISSN","@value":"21851719"},{"@type":"NDL_BIB_ID","@value":"000000015311"},{"@type":"ISSN","@value":"00167444"},{"@type":"LISSN","@value":"00167444"},{"@type":"NCID","@value":"AN00148053"}],"prism:publicationName":[{"@language":"en","@value":"Geographical Review of Japan"},{"@language":"ja","@value":"地理学評論"},{"@language":"en","@value":"Geogr. Rev. JPN, Chirigaku Hyoron, Geogr. Rev. of Japan"},{"@language":"ja","@value":"地理評"}],"dc:publisher":[{"@language":"en","@value":"The Association of Japanese Geographers"},{"@language":"ja","@value":"公益社団法人 日本地理学会"}],"prism:publicationDate":"1958","prism:volume":"31","prism:number":"2","prism:startingPage":"59","prism:endingPage":"85"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/9972999"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I9972999"}],"availableAt":"1958","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1363101969044634496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Leaching Behavior of As, Pb, Ni, Fe, and Mn from Subsurface Marine and Nonmarine Depositional Environment in Central Kanto Plain, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204266824576","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"浅層反射法弾性波探査による関東平野中央部の地下地質構造(<特集>最も新しい時代における変動と地震)"},{"@language":"en","@value":"Subsurface geological structure by the shallow seismic reflection survey in the central area of the Kanto plain(<Special issue>Quaternary crustal movement and its relation to seismisity)"},{"@value":"浅層反射法弾性波探査による関東平野中央部の地下地質構造"},{"@language":"ja-Kana","@value":"センソウ ハンシャホウ ダンセイハ タンサ ニヨル カントウ ヘイヤ チュウオ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204266835072","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"下総層群の層序と構造の形成過程(<特集>房総半島における第四系の層序と堆積作用)"},{"@language":"en","@value":"Forming process of marine Pleistocene succession, the Shimousa Group, in the Kanto Tectonic Basin(<Special Issue>Stratigraphy and Sedimentation of the Ouaternary System in Boso Peninsula, Japan)"},{"@value":"下総層群の層序と構造の形成過程"},{"@language":"ja-Kana","@value":"シモウサソウグン ノ ソウジョ ト コウゾウ ノ ケイセイ カテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679213286528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Last 400 ka Landform Evolution of the Kanto Plain"},{"@language":"ja","@value":"過去40万年間の関東平野の地形発達史"},{"@value":"過去40万年間の関東平野の地形発達史 : 地殻変動と氷河性海水準変動の関わりを中心に"},{"@language":"ja-Kana","@value":"カコ 40マンネンカン ノ カントウ ヘイヤ ノ チケイ ハッタツシ : チカク ヘンドウ ト ヒョウガセイカイ スイジュン ヘンドウ ノ カカワリ オ チュウシン ニ"},{"@value":"Last 400 ka landform evolution of the Kanto Plain: under the influence of concurrent glacio-eustatic sea level changes and tectonic activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679243542528","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"下総台地北部における更新世中期以降の地殻変動史(<特集>最も新しい時代における変動と地震)"},{"@language":"en","@value":"Development of crustal movements after Middle Pleistocene, in the northern district of the Shimousa Upland, Central Japan(<Special issue>Quaternary crustal movement and its relation to seismisity)"},{"@value":"下総台地北部における更新世中期以降の地殻変動史"},{"@language":"ja-Kana","@value":"シモウサ ダイチ ホクブ ニ オケル コウシンセイ チュウキ イコウ ノ チカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679401604864","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"群馬県大間々扇状地における地下水水質の空間分布および季節変化特性―硝酸態窒素に着目して―"},{"@language":"en","@value":"Seasonal and spatial changes in groundwater environment in Omama alluvial fan, Gunma Prefecture: focusing on nitrate-nitrogen"},{"@language":"ja-Kana","@value":"グンマケン オオマクリカエシ センジョウチ ニ オケル チカスイ スイシツ ノ クウカン ブンプ オヨビ キセツ ヘンカ トクセイ : ショウサンタイ チッソ ニ チャクモク シテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679440534144","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Shoreline Changes during the Holocene Transgression Based on the Fossil Biatom Asesmblages and the Distribution of Shell Mounds in the Upper Part of the Arakawa Lowland, Central Kanto Region."},{"@value":"珪藻遺骸群集による縄文海進期の想定海岸線と貝塚分布との関係　　埼玉県荒川低地上流域を例にして"},{"@language":"ja-Kana","@value":"ケイソウ イガイ グンシュウ ニヨル ジョウモン カイシンキ ノ ソウテイ カ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679441026176","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"気候地形発達史研究における「斜面不安定期」の概念"},{"@language":"en","@value":"The Concept of “the Period of Slope Instability” in Cliatogenic Geomorphology"},{"@language":"ja-Kana","@value":"キコウ チケイ センダツシ ケンキュウ ニ オケル シャメン フアンテイキ ノ ガイネン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680401427328","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"豊川中・下流域における後期更新世以降の地形発達史"},{"@language":"en","@value":"Late Pleistocene Geomorphic Development of the Coastal Plain in the Middle and Lower Reaches of the Toyo River, Central Japan"},{"@language":"ja-Kana","@value":"トヨカワチュウ カリュウイキ ニ オケル コウキ コウシンセイ イコウ ノ チケ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390294584544546816","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Plio-Pleistocene widespread tephras in and around the Choshi Geopark area, east Chiba Prefecture, central Japan and Introduction of the Choshi Geopark"},{"@language":"ja","@value":"千葉県東部，銚子周辺地域の鮮新-更新世テフラと銚子ジオパーク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238074595968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"戦後日本の地学（昭和20年～昭和40年）〈その6〉─「日本地学史」稿抄─"},{"@language":"en","@value":"Trends of Geosciences after the Pacific War in Japan, 1945 to 1965 Part 6"},{"@language":"ja-Kana","@value":"センゴ ニホン ノ チガク ショウワ 20ネン ショウワ 40ネン ソノ6 : ニホン チガクシ コウショウ"},{"@value":"戦後日本の地学(昭和20年~昭和40年)(その6)「日本地学史」稿抄"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:0036256564"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I9972999"},{"@type":"CROSSREF","@value":"10.4157/grj.31.59"},{"@type":"CIA","@value":"130003566893"},{"@type":"CIA","@value":"10012799997"},{"@type":"OPENAIRE","@value":"doi_dedup___::97103b4369986c8b88ab8d598db3daa9"},{"@type":"CROSSREF","@value":"10.4145/jahs.47.61_references_DOI_CbhDJL4oTAQ9UNOAEeJYE5VvKEo"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2022.0032_references_DOI_CbhDJL4oTAQ9UNOAEeJYE5VvKEo"},{"@type":"CROSSREF","@value":"10.5026/jgeography.122.921_references_DOI_CbhDJL4oTAQ9UNOAEeJYE5VvKEo"},{"@type":"CROSSREF","@value":"10.5026/jgeography.127.835_references_DOI_CbhDJL4oTAQ9UNOAEeJYE5VvKEo"},{"@type":"CROSSREF","@value":"10.3390/geosciences9100435_references_DOI_CbhDJL4oTAQ9UNOAEeJYE5VvKEo"}]}