{"@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/1390282681473698176.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4116/jaqua.40.251"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"5798035"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/5798035"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I5798035"}},{"identifier":{"@type":"NAID","@value":"10007431026"}}],"dc:title":[{"@language":"en","@value":"Sea Level Changes and Tectonics Inferred from the Quaternary Deposits and Landforms of Boso Peninsula, Central Japan. Chronology of the Shimosa Group and Movement of the \"Kashima\" Uplift Zone, Central Japan."},{"@value":"房総半島の第四紀　　地層・地形から読む海水準変動とテクトニクス　　下総層群の年代と“鹿島”隆起帯の運動"},{"@language":"ja-Kana","@value":"シモウサソウグン ノ ネンダイ ト カシマ リュウキタイ ノ ウンドウ"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"The age of the marine Pleistocene Shimosa Group ranges between 450, 000 and 80, 000 years, based on the correlation of dated marker tephras and comparison with the marine oxygen isotope curve. The Shimosa Group is chracterized by cyclic depositional sequences. Each formation boundary of the group corresponds to a low sea level period, as demonstrated by the existence of terrestrial deposits and unconformity. The standard stratigraphy of the Shimosa Group established in the Kisarazu-Anesaki region is applicable to the entire northern part of Chiba Prefecture based on the traces and the correlation of the tephras.<br>In the northeast part of Chiba Prefecture, the upper part of the massive silt layer which is considered to be the Kazusa Group is newly correlated with the Jizodo Formation. The depositional depth of the silt layer is deeper than that of the Jizodo Formation distributed to the southwest or further. Therefore, remarkable activity of the “Kashima” uplift zone was not noted in this district during the period of the Jizodo Formation. In addition, some regional differences of tilting are seen according to the distribution and structure of the Pleistocene. It is thought that these differences indicate the segmentation of the Kashima-Boso uplift zone. In particular, the northeast part of Chiba Prefecture tilted rapidly during the period of the Yabu Formation. The “Kashima” uplift zone became more active during the period of the Yabu Formation, and contributed to the formation of the barrier island system in this area."},{"@value":"下総層群は,年代値の得られているテフラの対比および酸素同位体比曲線との対比から約45万年前～8万年前の年代を占める.各累層境界は陸成層や不整合の存在から海面低下期に対応する.千葉県の木更津-姉崎地域で確立された下総層群の標準層序は,テフラの追跡・対比により木更津市以北の千葉県北部全域に適用できる.<br>成田市-東金市以東の千葉県北東部において,従来上総層群に対比されていた塊状シルト層の上部は,テフラの対比によって地蔵堂層に対比され,その堆積深度はより南西側の地蔵堂層に比べ深い.したがって,地蔵堂層堆積期までには,この地域における“鹿島”隆起帯の顕著な活動は認められない.さらに,下総層群の各累層基底面等高線図から,これらの面の傾動速度の経時変化を求めると,地域によって違いが認められる.その境界は千葉-八潮断層の延長線,成田-多古を結ぶライン,利根川沿いにあると考えられ,鹿島-房総隆起帯の運動にブロック化が認められる.特に千葉県北東部は藪層堆積期に急激な傾動を受けた.“鹿島”隆起帯が顕在化する時期は藪層堆積期であり,その影響によりこの地域ではバリヤー島システムが形成された."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030003658486772225","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00373225"},{"@type":"NRID","@value":"1000000373225"},{"@type":"NRID","@value":"9000411495801"},{"@type":"NRID","@value":"9000410505763"},{"@type":"NRID","@value":"9000363137058"},{"@type":"NRID","@value":"9000363136756"},{"@type":"NRID","@value":"9000363136885"},{"@type":"NRID","@value":"9000363140447"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/geo_gw"}],"foaf:name":[{"@language":"en","@value":"Nakazato Hiroomi"},{"@language":"ja","@value":"中里 裕臣"}],"jpcoar:affiliationName":[{"@language":"en","@value":"National Institute for Rural Engineering"},{"@language":"ja","@value":"農業工学研究所"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681211981570","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000004609474"}],"foaf:name":[{"@language":"en","@value":"Sato Hiroyuki"},{"@language":"ja","@value":"佐藤 弘幸"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Shizuoka Seikogakuin Junior & Senior High School"},{"@language":"ja","@value":"静岡聖光学院"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"04182642"},{"@type":"LISSN","@value":"04182642"},{"@type":"EISSN","@value":"18818129"},{"@type":"NDL_BIB_ID","@value":"000000014125"},{"@type":"ISSN","@value":"04182642"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/04182642"},{"@type":"NCID","@value":"AN0034136X"}],"prism:publicationName":[{"@language":"en","@value":"The Quaternary Research (Daiyonki-Kenkyu)"},{"@language":"ja","@value":"第四紀研究"},{"@language":"en","@value":"The Quaternary Res."},{"@language":"en","@value":"The Quat. Res."},{"@language":"en","@value":"The Quat. Res. (Daiyonki-Kenkyu)"},{"@language":"ja","@value":"第四紀研究"},{"@language":"en","@value":"Daiyonki-kenkyu"}],"dc:publisher":[{"@language":"en","@value":"Japan Association for Quaternary Research"},{"@language":"ja","@value":"日本第四紀学会"}],"prism:publicationDate":"2001","prism:volume":"40","prism:number":"3","prism:startingPage":"251","prism:endingPage":"257"},"reviewed":"false","url":[{"@id":"http://id.ndl.go.jp/bib/5798035"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I5798035"}],"availableAt":"2001","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=%E4%B8%8B%E7%B7%8F%E5%B1%A4%E7%BE%A4","dc:title":"下総層群"},{"@id":"https://cir.nii.ac.jp/all?q=%E3%83%86%E3%83%95%E3%83%A9","dc:title":"テフラ"},{"@id":"https://cir.nii.ac.jp/all?q=%E6%B0%B7%E6%B2%B3%E6%80%A7%E6%B5%B7%E6%B0%B4%E6%BA%96%E5%A4%89%E5%8B%95","dc:title":"氷河性海水準変動"},{"@id":"https://cir.nii.ac.jp/all?q=%E9%B9%BF%E5%B3%B6-%E6%88%BF%E7%B7%8F%E9%9A%86%E8%B5%B7%E5%B8%AF","dc:title":"鹿島-房総隆起帯"},{"@id":"https://cir.nii.ac.jp/all?q=%E5%82%BE%E5%8B%95","dc:title":"傾動"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360025431093837312","@type":"Article","resourceType":"学術雑誌論文(journal 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カンヒ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204233010432","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"千葉県北東部,中部更新統八日市場層における化石棲管連結ロッセリア : 地層形成と造営動物の反応"},{"@language":"en","@value":"Stacked Rosselia socialis from the middle Pleistocene Yokaichiba Formation, Chiba Prefecture, central Japan : Sedimentation and responses of Rosselia animal"},{"@language":"ja-Kana","@value":"チバケン ホクトウブ チュウブ コウシントウ ヨウカイチバソウ ニ オケル カセキ セイカン レンケツ ロッセリア チソウ ケイセイ ト ゾウエイ ドウブツ ノ ハンノウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205196020224","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Pollen assemblages of Fukasaku A-1 drilling core, Saitama Prefecture, central Kanto plain, Japan"},{"@language":"ja","@value":"埼玉県さいたま市で掘削された深作A-1ボーリングコアの花粉化石群集"},{"@language":"ja-Kana","@value":"サイタマケン サイタマシ デ クッサク サレタ シンサク A 1 ボーリングコア ノ カフン カセキ グンシュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238095616","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Temporal changes in the paleoenvironment of the inner part of paleo-Tokyo Bay during the middle Pleistocene (MIS 11 and MIS 9):"},{"@language":"ja","@value":"中期更新世（MIS11およびMIS 9）における古東京湾湾奥の環境変遷"},{"@value":"中期更新世(MIS11およびMIS9)における古東京湾湾奥の環境変遷--埼玉県菖蒲コアの下総層群産貝形虫化石の群集解析"},{"@language":"ja-Kana","@value":"チュウキ コウシン セイ MIS11 オヨビ MIS9 ニ オケル コ トウキョウワンワン オウ ノ カンキョウ ヘンセン サイタマケン ショウブ コア ノ シモウサソウグンサン カイケイチュウ カセキ ノ グンシュウ カイセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238946304","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sequence stratigraphy of the Pleistocene Kioroshi Formation, Shimosa Group beneath the Omiya Upland, central Kanto Plain, central Japan"},{"@language":"ja","@value":"大宮台地の地下に分布する更新統下総層群木下層のシーケンス層序学的研究"},{"@language":"ja-Kana","@value":"オオミヤ ダイチ ノ チカ ニ ブンプ スル コウシントウ シモウサソウグン キノシタソウ ノ シーケンスソウ ジョガクテキ ケンキュウ"},{"@value":"Sequence Stratigraphy of the Pleistocene Kioroshi Formation, Shimousa Group beneath the Omiya Upland, Central Kanto Plain, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206239091840","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tephrochronology of the Middle to Late Pleistocene sediments in the northern part of the Boso Peninsula, central Japan"},{"@value":"房総半島北部の中・上部更新統のテフロクロノロジー"},{"@language":"ja-Kana","@value":"ボウソウ ハントウ ホクブ ノ ナカ ジョウブ コウシントウ ノ テフロクロノ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240254848","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stratigraphy and tectonics of the Plio-Pleistocene beneath the central Kanto Plain, central Japan"},{"@language":"ja","@value":"関東平野中央部の地下に分布する鮮新-更新統の層序と構造運動"},{"@language":"ja-Kana","@value":"カントウ ヘイヤ チュウオウブ ノ チカ ニ ブンプ スル センシン-コウシントウ ノ ソウ ジョ ト コウゾウ ウンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240754048","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Molluscan fossil assemblages and their stratigraphic positions in the Semata, Kamiizumi and Narita Formations of the Kisarazu-Ichihara area, Boso Peninsula"},{"@value":"木更津-市原地域の瀬又,上泉および成田層の貝化石群とその産出層準"},{"@language":"ja-Kana","@value":"キサラズ-イチハラ チイキ ノ セ マタ,カミイズミ オヨビ ナリタソウ ノ カイカセキグン ト ソノ サンシュツソウ ジュン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241660544","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Pleistocene Deposits in the Northern District of Naruto-machi, Chiba Prefecture"},{"@value":"千葉県成東町北方の第四系"},{"@language":"ja-Kana","@value":"チバケン ナルトウマチ ホッポウ ノ ダイ4ケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206242171520","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Chronostratigraphy of 1505 m long hot spring well drilled in the central Kanto Plain, central Japan"},{"@language":"ja","@value":"関東平野中央部埼玉県大利根町で掘削された1505 m温泉ボーリングの年代層序"},{"@language":"ja-Kana","@value":"カントウ ヘイヤ チュウオウブ サイタマケン オオトネマチ デ クッサク サレタ 1505m オンセン ボーリング ノ ネンダイソウ ジョ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496031872","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Flood Deposit of the Middle Pleistocene Kiyokawa Formation, Shimosa Group, Eastern Japan"},{"@language":"ja","@value":"更新統下総層群清川層にみられる海水準上昇初期の洪水堆積物"},{"@language":"ja-Kana","@value":"コウシントウ シモウサソウグン キヨカワソウ ニ ミラレル カイスイジュン ジョウショウ ショキ ノ コウズイ タイセキブツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496371968","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tephrochronological study on the middle Pleistocene deposits in the Kanto and Kinki districts, Japan"},{"@value":"南関東と近畿の中部更新統の対比と編年"},{"@language":"ja-Kana","@value":"ミナミ カントウ ト キンキ ノ チュウブ コウシントウ ノ タイヒ ト ヘン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496511104","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Identification and Chronostratigraphy of Middle to Upper Quaternary Marker Tephras Occurring in the Anden Coast Based on Comparison with ODP Cores in the Sea of Japan."},{"@value":"ＯＤＰ日本海試料との対比に基づく男鹿半島安田海岸更新世中‐後期テフラの同定と年代"},{"@language":"ja-Kana","@value":"ODP ニホンカイ シリョウ ト ノ タイヒ ニ モトズク オガ ハントウ ア"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496979200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stratigraphy and changes in the sedimentary environment since the Middle Pleistocene in the interior of the Kanto Plain, Japan"},{"@language":"ja","@value":"関東平野内陸部，吹上～行田地域における中・上部更新統の地下層序と堆積環境変化"},{"@language":"ja-Kana","@value":"カントウ ヘイヤ ナイリクブ フキアゲ ギョウダ チイキ ニ オケル ナカ ジョウブ コウシントウ ノ チカソウ ジョ ト タイセキ カンキョウ ヘンカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390019358131336576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geological structure of the Pleistocene Shimosa Group revealed by three-dimensional geological modeling in Tsukuba City and its surroundings, Ibaraki Prefecture"},{"@language":"ja","@value":"3次元地質モデリングにより明らかになった茨城県つくば市および周辺地域の更新統下総層群の地質構造"}]},{"@id":"https://cir.nii.ac.jp/crid/1390021094410320640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Oblique intersection of lithostratigraphic units and a tephra layer in the Pleistocene Shimosa Group beneath central Kanto Plain, central Japan."},{"@language":"ja","@value":"関東平野中央部における更新統下総層群の岩相層序区分とテフラの斜交"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207645568","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"南関東における第四紀中期のテフラの対比とそれに基づく編年"},{"@language":"en","@value":"Correlation and Chronology of the Middle Pleistocene Tephra Layers in South Kanto"},{"@language":"ja-Kana","@value":"ミナミカントウ ニ オケル ダイ4キ チュウキ ノ テフラ ノ タイヒ ト ソレニ モトズク ヘンネン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679211007232","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"茨城県南東部の更新統で確認された液状化-側方流動の痕跡と小断層群の形成"},{"@language":"en","@value":"Liquefaction-lateral flow features and minor faults in Pleistocene in the southeastern area of Ibaraki 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