{"@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/1363670321174248576.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0037-0738(92)90032-m"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:003707389290032M?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:003707389290032M?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"80006876932"}}],"dc:title":[{"@value":"Inferred glacio-eustatic control for high-frequency depositional sequences of the Plio-Pleistocene Kazusa Group, a forearc basin fill in Boso Peninsula, Japan"}],"description":[{"notation":[{"@value":"Abstract   The Plio—Pleistocene forearc basin fill of the Kazusa Group, as much as 3000 m thick, is represented by a series of marine environments ranging from deep-sea basin plain to shallow sea. It developed during about 2.4 to 0.45 Ma, and is well exposed in the Boso Peninsula, Japan. Chronostratigraphic resolution of the Kazusa Group is partly within about 0.05 m.y., based on the combination of fission track dating of volcanic ash layers, and bio- and magneto-stratigraphy. Many volcanic ash layers are intercalated in the Kazusa Group and provide distinct chronostratigraphic surfaces within the heterogeneous lithologies. Detailed outcrop studies on depositional facies discontinuities and lateral terminations of volcanic ash layers allow high-resolution sequence stratigraphic interpretation of the Kazusa Group.  Seventeen depositional sequences were identified in the Kazusa Group. Each depositional sequence was tentatively correlated with the stable oxygen isotope sea-level index, integrated with the age framework of the Kazusa Group. This correlation indicates that frequencies of the depositional sequences can be estimated to be in the range of 0.2-0.02 m.y. and are within fourth- and fifth-order stratigraphic cyclicities. Depositional sequences constitute third-order transgressive and highstand sequence sets and the Kazusa Group is interpreted to represent a third-order composite sequence with a duration of about 1.95 m.y. Development of the third-order composite sequence was also controlled by an overall rise and fall of glacio-eustatic sea levels, overprinted by tectonic events related to fluctuations in oceanic plate motion which occurred at about 2.6 Ma and 0.5 Ma, respectively."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670321174248577","@type":"Researcher","foaf:name":[{"@value":"Makoto Ito"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321174248576","@type":"Researcher","foaf:name":[{"@value":"Yuzo Katsura"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00370738"},{"@type":"NCID","@value":"AA00838854"}],"prism:publicationName":[{"@value":"Sedimentary Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1992-09","prism:volume":"80","prism:number":"1-2","prism:startingPage":"67","prism:endingPage":"75"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:003707389290032M?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:003707389290032M?httpAccept=text/plain"}],"createdAt":"2003-08-07","modifiedAt":"2019-03-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050002213761277952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Millennial-scale hydrographic changes in the northwestern Pacific during marine isotope stage 19: teleconnections with ice melt in the North Atlantic"},{"@value":"Millennial-scale hydrographic changes in the northwestern Pacific during marine isotope stage 19: teleconnection with ice melt in the North Atlantic"}]},{"@id":"https://cir.nii.ac.jp/crid/1050008763985565824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleoclimatic and paleoceanographic records through Marine Isotope Stage 19 at the Chiba composite section, central Japan: A key reference for the EarlyeMiddle Pleistocene Subseries boundary"},{"@value":"Paleoclimatic and paleoceanographic records through Marine Isotope Stage 19 at the Chiba composite section, central Japan: A key reference for the Early–Middle Pleistocene Subseries boundary"},{"@value":"Paleoclimatic and paleoceanographic records of Marine Isotope Stage 19 at the Chiba composite section, central Japan: a reference for the Early–Middle Pleistocene boundary"},{"@value":"Paleoclimatic and paleoceanographic records of Marine Isotope Stage 19 at the Chiba composite section, central Japan: a reference for the Early-Middle Pleisotocene boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1050575520347374080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene"},{"@value":"Millennial-scale northern Hemisphere Atlantic-Pacifc climate teleconnections in the earliest Middle Pleistocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232468992128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reactivation of map-scale faults in response to changes in crustal stress: Examples from Boso Peninsula, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232469004288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-resolution diatom record of paleoceanographic variations across the Early–Middle Pleistocene boundary in the Chiba Section, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232481979264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Warm climate under high CO2 level in the early Pleistocene based on a leaf fossil assemblage in central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142452858880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Biomarkers in the rock outcrop of the Kazusa Group reveal palaeoenvironments of the Kuroshio region"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142621925888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shape difference of mud clasts depending on depositional facies: application of newly modified elliptic Fourier analysis to hybrid event beds"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185481271296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geology and age model of the<scp>L</scp>ower<scp>P</scp>leistocene<scp>N</scp>ojima,<scp>O</scp>funa, and<scp>K</scp>oshiba Formations of the middle<scp>K</scp>azusa<scp>G</scp>roup, a forearc basin‐fill sequence on the<scp>M</scp>iura<scp>P</scp>eninsula, the<scp>P</scp>acific side of central<scp>J</scp>apan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092459150848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Poroelastic Modeling of a Heterogeneous Geologic Medium: A Case Study from Kanto Basin in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229831838720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Downslope variation in hemipelagic sedimentation in an active margin basin: An example from the lower Pleistocene Kiwada and Takamizo formations on the Boso Peninsula, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640787806336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Methane production potential of subsurface microbes in Pleistocene sediments from a natural gas field of the dissolved-in-water type, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846643539107200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Preferential formation of a slide plane in translational submarine landslide deposits in a Pleistocene forearc basin fill exposed in east-central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657350181120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reconstruction of altitudinal transportation range of leaves based on stomatal evidence: An example of the Early Pleistocene Fagus leaf fossils from central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657398972544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High resolution stratigraphy across the early–middle Pleistocene boundary from a core of the Kokumoto Formation at Tabuchi, Chiba Prefecture, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567376396800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Isolation of a member of the candidate phylum ‘Atribacteria’ reveals a unique cell membrane structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593774240000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Depositional process of the <scp>Byk‐E</scp> tephra bed in the Chiba section, central Japan: A marker bed defining the Global Boundary Stratotype Section and Point for the Chibanian Stage"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131414329824640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial Distribution of Mass‐Transport Deposits Deduced From High‐Resolution Stratigraphy"}]},{"@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/1363951794415715584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seabirds (Aves) from the Pleistocene Kazusa and Shimosa groups, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204065364096","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"アーケアによるメタンの生成と間隙水への濃集機構"},{"@language":"en","@value":"Generation of archaeal methane and its accumulation mechanism into interstitial water"},{"@language":"ja-Kana","@value":"アーケア ニ ヨル メタン ノ セイセイ ト カンゲキスイ エ ノ ノウシュウ キコウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204266832640","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"房総半島南端更新統豊房層群の層序と堆積シークェンス(<特集>房総半島における第四系の層序と堆積作用)"},{"@language":"en","@value":"Stratigraphy and depositional sequences of the Pleistocene Toyofusa Group, southernmost part of the Boso Peninsula, central Japan(<Special Issue>Stratigraphy and Sedimentation of the Ouaternary System in Boso Peninsula, Japan)"},{"@value":"房総半島南端更新統豊房層群の層序と堆積シークェンス"},{"@language":"ja-Kana","@value":"ボウソウ ハントウ ナンタン コウシントウ トヨフサソウグン ノ ソウジョ ト"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204434962560","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"中部更新統金剛地層市野々砂泥互層に見られる Rosselia socialis 密集層と海水準ダイナミクス"},{"@language":"en","@value":"The Rosselia socialis-crowded beds in the middle Pleistocene and sea-level dynamics"},{"@language":"ja-Kana","@value":"チュウブ コウシントウ コンゴウ チソウ イチノノ サデイ ゴソウ ニ ミラレ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205218916736","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evaluation of the effect of turbidity currents in the formation of hemipelagic siltstones: An example from the lower Pleistocene Kazusa Group on the Boso Peninsula, Japan"},{"@language":"ja","@value":"半遠洋性シルト岩の形成における混濁流の影響評価:房総半島下部更新統上総層群の解析"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234586368","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magnetostratigraphy and biostratigraphy of the Plio-Pleistocene Chikura and Toyofusa Groups, southernmost part of the Boso Peninsula, central Japan."},{"@value":"房総半島南端地域に分布する千倉・豊房層群（鮮新‐更新統）の古地磁気および微化石層序"},{"@language":"ja-Kana","@value":"ボウソウ ハントウ ナンタン チイキ ニ ブンプスル チクラ トヨフサソウグン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206235215360","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fission track ages of volcanic ash layers of the Kazusa Group in the Boso Peninsula, central Japan."},{"@value":"房総半島上総層群のフィッション・トラック年代"},{"@language":"ja-Kana","@value":"ボウソウ ハントウ カズサソウグン ノ フィッション トラック ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206236847232","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-resolution chronology of the lower Pleistocene Otadai and Umegase Formations of the Kazusa Group, Boso Peninsula, central Japan -Chronostratigraphy of the JNOC TR-3 cores based on oxygen isotope, magnetostratigraphy and calcareous nannofossil-"},{"@language":"ja","@value":"房総半島に分布する下部更新統上総層群大田代層と梅ヶ瀬層の高精度堆積年代―石油公団研究井TR-3コアの酸素同位体比・古地磁気・石灰質ナンノ化石に基づく年代層序―"},{"@language":"ja-Kana","@value":"ボウソウ ハントウ ニ ブンプ スル カブ コウシントウ カズサソウグン オオタダイソウ ト ウメガセソウ ノ コウセイド タイセキ ネンダイ セキユ コウダン ケンキュウイ TR 3 コア ノ サンソ ドウイタイヒ コ チジキ セッカイシツ ナンノ カセキ ニ モトヅク ネンダイソウ ジョ"},{"@value":"High-resolution chronology of the lower Pleistocene Otadai and Umegase formations of the Kazusa group, Boso Peninsula, central JapandChronostratig- raphy of the JNOC TR-3 cores based on oxygen isotope, magnetostratigraphy and calcareous nanofossil"},{"@value":"High-resolution chronology of the lower Pleistocene Otadai and Umegase formations of the Kazusa group, Boso Peninsula, central Japan—Chronostratigraphy of the JNOC TR-3 cores based on oxygen isotope, magnetostratigraphy and calcareous nanofossil"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206497026816","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sea Level Changes and Tectonics Inferred from the Quaternary Deposits and Landforms of Boso Peninsula, Central Japan. Glacioeustatic and Paleoceanographic Changes Documented in Shelf and Deep-water Successions of the Plio-Pleistocene Kazusa Group, Boso Peninsula, 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　　上総層群の陸棚‐深海堆積物に記録された氷河性海水準変動と古海洋変動"},{"@language":"ja-Kana","@value":"カズサソウグン ノ リクダナ シンカイ タイセキブツ ニ キロク サレタ ヒョウガセイカイ スイジュン ヘンドウ ト コ カイヨウ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390002184858780672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cold-seep-dependent fossil assemblages in the middle Pleistocene Kakinokidai Formation at Kawayatsu, Kimitsu City, Japan"},{"@language":"ja","@value":"千葉県君津市川谷地域に露出する中部更新統柿ノ木台層から産出する冷湧水化石群集"},{"@value":"千葉県君津市川谷地域に露出する中部更新統柿ノ木台層から産出する冷湧水化石群集 : その時空分布と共産する自生炭酸塩"},{"@language":"ja-Kana","@value":"チバケン キミツ イチカワ ヤチイキ ニ ロシュツ スル チュウブ コウシントウガキ ノキダイソウ カラ サンシュツ スル レイワキミズ カセキ グンシュウ : ソノ ジクウ ブンプ ト キョウサン スル ジセイ タンサンエン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390016494575405568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"古地磁気層序とテフラ層序に基づく房総半島南部の下部更新統千倉層群と同半島東部の上総層群の対比"},{"@language":"en","@value":"Stratigraphic correlation between the lower Pleistocene Chikura Group in the southern part of the Boso Peninsula and the Kazusa Group in the eastern part of the peninsula, based on magneto- and tephro-stratigraphy"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679038866432","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sedimentological, petrographical, and mathematical researches for the estimation of the distribution of turbidite sandstone reservoirs: Case studies in Neogene to Quaternary Niigata and Boso sedimentary basins, central Japan."},{"@value":"タービダイト砂岩分布予測のための堆積学的・岩石学的・数理学的研究　　新潟および房総における解析例"},{"@language":"ja-Kana","@value":"タービダイト サガン ブンプ ヨソク ノ タメ ノ タイセキガクテキ ガンセキガクテキ スウリガクテキ ケンキュウ ニイガタ オヨビ ボウソウ ニ オケル カイセキレイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207505280","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Depositional Environments and Sequence Stratigraphic Analysis of the Middle Pleistocene Kongochi Formation."},{"@value":"中部更新統金剛地層の堆積環境とシーケンス層序学的解析"},{"@language":"ja-Kana","@value":"チュウブ コウシントウ コンゴウ チソウ ノ タイセキ カンキョウ ト シーケ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679242882048","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"鮮新-更新統に認められる相対的海水準変動とその対比 ―大阪・掛川・魚沼・上総層群を例として―(<特集>指標テフラと鮮新-下部更新統)"},{"@language":"en","@value":"Correlation of relative sea-level changes in Plio-Pleistocene forearc and backarc basin-fill successions of the Osaka, Kakegawa, Kazusa and Uonuma Groups, Japan(<Special issue>Tephrochronology and Plio-Lower Pleistocene in 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Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681211492608","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Depositional sequences in turbidite successions of the lower Kazusa Group, the Plio-Pleistocene forearc basin fill in the Boso Peninsula, Japan."},{"@language":"ja","@value":"房総半島,鮮新・更新統上総層群下部のタービダイト堆積シーケンス"},{"@value":"房総半島,鮮新・更新統上総層群下部のタービダイト堆積シーケンス〔英文〕"},{"@language":"ja-Kana","@value":"ボウソウ ハントウ センシン コウシントウ カズサソウグン カブ ノ タービダ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681216690304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Lithology and upper boundary of the Olduvai Subchronozone in a core recovered from the middle Kazusa Group (Lower Pleistocene) on the Miura Peninsula, Pacific side of central Japan"},{"@language":"ja","@value":"三浦半島北部の上総層群中部（下部更新統）で掘削されたコアの堆積相とオルドバイ正磁極亜帯の上限"},{"@language":"ja-Kana","@value":"ミウラ ハントウ 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