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Distribution, age, and origin of a submarine landslide deposit in the Pleistocene Kiwada Formation, forearc basin fill on the Boso Peninsula, east‐central Japan: Constraints from tephro‐ and biostratigraphy

The island arc, 2018-07, Vol.27 (4), p.n/a

Utsunomiya, Masayuki

2018

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Speciation of extant Umbilicosphaera (Prymnesiophyceae) during the Pliocene

Marine micropaleontology, 2021-12, Vol.169, p.102037, Article 102037

2021

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Extraordinary cold episodes during the mid-Holocene in the Yangtze delta: Interruption of the earliest rice cultivating civilization

Quaternary science reviews, 2018-12, Vol.201, p.418-428

2018

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Basin-wide erosion and segmentation of the Plio-Pleistocene forearc basin in central Japan revealed by tephro- and biostratigraphy

Progress in earth and planetary science, 2023-12, Vol.10 (1), p.25-26, Article 25

2023

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Reactivation of map-scale faults in response to changes in crustal stress: Examples from Boso Peninsula, Japan

Quaternary international, 2017-10, Vol.456, p.117-124

2017

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Chronostratigraphy of the Pliocene–Pleistocene boundary in forearc basin fill on the Pacific side of central Japan: Constraints on the spatial distribution of an unconformity resulting from a widespread tectonic event

Quaternary international, 2017-10, Vol.456, p.125-137

2017

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Biomarkers in the rock outcrop of the Kazusa Group reveal palaeoenvironments of the Kuroshio region

Communications earth & environment, 2021-05, Vol.2 (1), Article 82

2021

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Evolutionary change of crystallographic orientation and coccolith morphology: Neogene-Quaternary Umbilicosphaera (Prymnesiophyceae) lineage

Marine micropaleontology, 2024-06, Vol.190, p.102370, Article 102370

2024

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Long-chain alkenones in the Shimosa Group reveal palaeotemperatures of the Pleistocene interglacial Palaeo-Tokyo Bays

Progress in earth and planetary science, 2022-07, Vol.9 (1), p.1-13, Article 40

2022

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Formation of excess fluid pressure, sediment fluidization and mass-transport deposits in the Plio-Pleistocene Boso forearc basin, central Japan

Geological Society special publication, 2019-01, Vol.477 (1), p.255-264

2019

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Preferential formation of a slide plane in translational submarine landslide deposits in a Pleistocene forearc basin fill exposed in east-central Japan

Geological Society special publication, 2019-01, Vol.477 (1), p.241-253

2019

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Author Correction: Biomarkers in the rock outcrop of the Kazusa Group reveal palaeoenvironments of the Kuroshio region

Communications earth & environment, 2021-12, Vol.2 (1), Article 141

2021

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An in situ Vesicomyid-dominated Cold-seep Assemblage from the Lowermost Pleistocene Urago Formation, Kazusa Group, Forearc Basin Fill on the Northern Miura Peninsula, Pacific Side of Central Japan

Paleontological research, 2015-01, Vol.19 (1), p.1-20

2015

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Geology and fossil cold-seep assemblages in the Kazusa Group on the northern Miura Peninsula, central Japan

The Journal of the Geological Society of Japan, 2022/12/29, Vol.128(1), pp.313-333

2022

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房総半島に分布する上総層群の広域テフラ: 特に上総層群下部におけるテフラ層序と新たな対比

地質学雑誌, 2019/01/15, Vol.125(1), pp.23-39

2019

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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

地質学雑誌, 2019/09/15, Vol.125(9), pp.655-683

2019

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Late Triassic radiolarians and conodonts from a chert pebble within the Lower Pleistocene Higashihigasa Formation of the Kazusa Group, Boso Peninsula, Japan

Chishitsu chōsa kenkyū hōkoku = Bulletin of the Geological Survey of Japan, 2022-10, Vol.73 (3), p.93-101

2022

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Additional data of calcareous nannofossil assemblage in a sediment sample obtained from the seafloor near the Ishigaki Island (GH18 cruise)

Chishitsu chōsa kenkyū hōkoku = Bulletin of the Geological Survey of Japan, 2023-12, Vol.74 (5-6), p.337-338

UTSUNOMIYA, Masayuki

2023

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Geology and fossil cold-seep assemblages in the Kazusa Group on the northern Miura Peninsula, central Japan

Chishitsugaku zasshi, 2022-12, Vol.128 (1), p.313-333, Article 2022.0030

2022

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Correlation between a Tephra Bed from Deep (2038 m) Underground below Chiba City, and Kd48 in the Lowermost Kiwada Formation (Lower Pleistocene) on the Boso Peninsula

Journal of Geography (Chigaku Zasshi), 2020/06/25, Vol.129(3), pp.355-374

2020

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Forearc tectonics and submarine landslides recorded in the lower part of the Kazusa Group, eastern Boso Peninsula

The Journal of the Geological Society of Japan, 2022/12/08, Vol.128(1), pp.265-280

2022

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三浦半島北部の上総層群の地質と冷湧水性化学合成化石群集

地質学雑誌, 2022/12/29, Vol.128(1), pp.313-333

2022

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房総半島東部，上総層群下部に記録された前弧テクトニクスと海底地すべり

地質学雑誌, 2022/12/08, Vol.128(1), pp.265-280

2022

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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

The Journal of the Geological Society of Japan, 2023/10/31, Vol.129(1), pp.469-487

2023

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Depositional ages of sedimentary rocks obtained from the sea floor around the northern Tokara Islands during GB21-3 cruise, based on calcareous microfossil assemblages, and their geological significance

Chishitsu chōsa kenkyū hōkoku = Bulletin of the Geological Survey of Japan, 2023-12, Vol.74 (5-6), p.245-257

2023

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Distribution, age, and origin of a submarine landslide deposit in the Pleistocene Kiwada Formation, forearc basin fill on the Boso Peninsula, east‐central Japan: Constraints from tephro‐ and biostratigraphy

Speciation of extant Umbilicosphaera (Prymnesiophyceae) during the Pliocene

Extraordinary cold episodes during the mid-Holocene in the Yangtze delta: Interruption of the earliest rice cultivating civilization

Basin-wide erosion and segmentation of the Plio-Pleistocene forearc basin in central Japan revealed by tephro- and biostratigraphy

Reactivation of map-scale faults in response to changes in crustal stress: Examples from Boso Peninsula, Japan

Chronostratigraphy of the Pliocene–Pleistocene boundary in forearc basin fill on the Pacific side of central Japan: Constraints on the spatial distribution of an unconformity resulting from a widespread tectonic event

Biomarkers in the rock outcrop of the Kazusa Group reveal palaeoenvironments of the Kuroshio region

Evolutionary change of crystallographic orientation and coccolith morphology: Neogene-Quaternary Umbilicosphaera (Prymnesiophyceae) lineage

Long-chain alkenones in the Shimosa Group reveal palaeotemperatures of the Pleistocene interglacial Palaeo-Tokyo Bays

Formation of excess fluid pressure, sediment fluidization and mass-transport deposits in the Plio-Pleistocene Boso forearc basin, central Japan

Preferential formation of a slide plane in translational submarine landslide deposits in a Pleistocene forearc basin fill exposed in east-central Japan

Author Correction: Biomarkers in the rock outcrop of the Kazusa Group reveal palaeoenvironments of the Kuroshio region

An in situ Vesicomyid-dominated Cold-seep Assemblage from the Lowermost Pleistocene Urago Formation, Kazusa Group, Forearc Basin Fill on the Northern Miura Peninsula, Pacific Side of Central Japan

Geology and fossil cold-seep assemblages in the Kazusa Group on the northern Miura Peninsula, central Japan

房総半島に分布する上総層群の広域テフラ: 特に上総層群下部におけるテフラ層序と新たな対比

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

Late Triassic radiolarians and conodonts from a chert pebble within the Lower Pleistocene Higashihigasa Formation of the Kazusa Group, Boso Peninsula, Japan

Additional data of calcareous nannofossil assemblage in a sediment sample obtained from the seafloor near the Ishigaki Island (GH18 cruise)

Geology and fossil cold-seep assemblages in the Kazusa Group on the northern Miura Peninsula, central Japan

Correlation between a Tephra Bed from Deep (2038 m) Underground below Chiba City, and Kd48 in the Lowermost Kiwada Formation (Lower Pleistocene) on the Boso Peninsula

Forearc tectonics and submarine landslides recorded in the lower part of the Kazusa Group, eastern Boso Peninsula

三浦半島北部の上総層群の地質と冷湧水性化学合成化石群集

房総半島東部，上総層群下部に記録された前弧テクトニクスと海底地すべり

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

Depositional ages of sedimentary rocks obtained from the sea floor around the northern Tokara Islands during GB21-3 cruise, based on calcareous microfossil assemblages, and their geological significance

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