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房総半島中央部,上総-下総堆積盆の地質構造とその形成過程-反射法地震探査からの考察-
https://doi.org/10.24732/NIED.00007085
DOI
1362fe60-b991-4c31-ac08-c2e04b9fe527
名前 / ファイル | ライセンス | アクション |
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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タイトル | ||||||
言語 | ja | |||||
タイトル | 房総半島中央部,上総-下総堆積盆の地質構造とその形成過程-反射法地震探査からの考察- | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Geologic Structure of the Kazusa-Shimousa Sedimentary Basin and its Formation Process in the Central Part of the Boso Peninsula, Japan - A Study Based on Seismic Reflection Explorations - | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
言語 | ja | |||||
主題Scheme | Other | |||||
主題 | 反射法地震探査,地質構造,上総-下総堆積盆,房総半島中央部 | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Seismic reflection exploration, Geologic structure, Kazusa-Shimousa sedimentary basin, Central Boso Peninsula | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | journal article | |||||
ID登録 | ||||||
ID登録 | 10.24732/NIED.00007085 | |||||
ID登録タイプ | JaLC | |||||
著者 |
浅尾, 一巳
× 浅尾, 一巳× 伊藤, 谷生× 佐藤, 比呂志× 須田, 茂幸× 有山, 覚 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 首都圏では,地震災害対策の基礎データを集積するために反射法地震探査等による地下構造探査が精力的に行われてきた.しかし,首都圏は,広く沖積低地や火山灰に覆われた河岸段丘や扇状地が広がっているため,反射法断面に詳細な地下地質層序を描き入れることが困難な状況である.こうした状況を打開するため,本研究において南関東地域の標準地質層序である上総層群と下総層群が地表に露出している房総半島中央部で反射法地震探査と屈折法地震探査を実施し,12 層準に及ぶ鍵反射面を抽出した.そのことによる主要な成果は,第1 に上総-下総層群の堆積盆の形成と成長を東京湾から九十九里沖の広い範囲で考察したことである.我々はこの堆積盆を上総-下総堆積盆と呼ぶことにした.第2 に,抽出した12 鍵反射面のうち,3 鍵反射面は首都圏で広く追跡でき,抽出されたことにより反射断面の解釈を大きく前進させる道を切り拓いたことである. | |||||
言語 | ja | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Seismic reflection surveys have been recently conducted to accumulate fundamental data for earthquake disaster preventions in the Tokyo metropolitan area. However, extensive alluvial lowlands and volcanic-ash covered river terraces/fans in the area obstruct to depict detailed subsurface geological stratigraphy in seismic reflection profiles. In order to overcome this situation, our research focused on conducting seismic reflection and refraction surveys in the central part of the Boso Peninsula, where the standard geological stratigraphy of the Kazusa and the Shimousa Groups is exposed at the surface without these sediments. The first achievement resulting from this study is the elucidation of the formation and growth of the sedimentary basin of the Kazusa and the Shimousa Groups extending over a wide region from Tokyo Bay to the Kujukuri offshore area. We have decided to call the basin the Kazusa - Shimousa sedimentary basin. The second is the 3 key horizons out of extracted of 12 key reflectors can be widely traced into the Tokyo metropolitan area, which will lead to significant advancement on the interpretation of seismic reflection profiles in the Tokyo metropolitan area. | |||||
言語 | en | |||||
内容記述 | ||||||
内容記述タイプ | Other | |||||
内容記述 | (ONLINE先行公開につき、ページ数および発行年情報は仮のものになります。引用にはDOIをご利用ください) | |||||
言語 | ja | |||||
書誌情報 |
ja : 防災科学技術研究所 研究報告 en : Report of the National Research Institute for Earth Science and Disaster Resilience 巻 89, p. 1-35, 発行日 2025-04-25 |
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出版者 | ||||||
言語 | ja | |||||
出版者 | 防災科学技術研究所 | |||||
出版者 | ||||||
言語 | en | |||||
出版者 | National Research Institute for Earth Science and Disaster Resilience | |||||
収録物識別子 | ||||||
収録物識別子タイプ | EISSN | |||||
収録物識別子 | 1347-7471 |