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Detailed Stratigraphical and Geological Characteristics of Volcanic and Epiclastic Deposits Burying a Roman Villa on the Northen Flank of Mt. Vesuvius(Italy)
https://doi.org/10.15083/0000032478
https://doi.org/10.15083/000003247808ea3f03-658f-4fad-bf6f-994b8988c678
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
IHO82201.pdf (7.82MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2008-02-28 | |||||
| タイトル | ||||||
| タイトル | Detailed Stratigraphical and Geological Characteristics of Volcanic and Epiclastic Deposits Burying a Roman Villa on the Northen Flank of Mt. Vesuvius(Italy) | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Vesuvius | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | volcanoes | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | burial process | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | excavation site | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Roman Villa | |||||
| 資源タイプ | ||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||
| タイプ | departmental bulletin paper | |||||
| ID登録 | ||||||
| ID登録 | 10.15083/0000032478 | |||||
| ID登録タイプ | JaLC | |||||
| その他のタイトル | ||||||
| その他のタイトル | イタリア・ヴェスヴィオ火山北麓のローマ遺跡を埋没した火山性堆積物の層序と特徴 | |||||
| 著者 |
Niihori, Kenji
× Niihori, Kenji× Nagai, Masashi× Kaneko, Takayuki× Fujii, Toshitsugu× Nakada, Setsuya× Yoshimoto, Mitsuhiro× Yasuda, Atsushi× Aoyagi, Masanori |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124294 | |||||
| 姓名 | 新堀, 賢志 | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124295 | |||||
| 姓名 | 長井, 雅史 | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124296 | |||||
| 姓名 | 金子, 隆之 | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124297 | |||||
| 姓名 | 藤井, 敏嗣 | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124298 | |||||
| 姓名 | 中田, 節也 | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124299 | |||||
| 姓名 | 吉本, 充宏 | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124300 | |||||
| 姓名 | 安田, 敦 | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124301 | |||||
| 姓名 | 青柳, 正規 | |||||
| 著者所属 | ||||||
| 著者所属 | Earthquake Research Institute of Tokyo University | |||||
| 著者所属 | ||||||
| 著者所属 | Institute of Natural Sciences, College of Humanities anda Sciences, Nihon University | |||||
| 著者所属 | ||||||
| 著者所属 | Department of Earth Science, Faculty of Science, Hokkaido University | |||||
| 著者所属 | ||||||
| 著者所属 | National Museum of Western Art | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | An archaeological excavation site at the northern foot of Mt. Vesuvius in Italy provided a three-dimensional outcrop with a height of 8m to study its volcanic succession. Through a stratigraphical study of sediments and chemical analyses of juvenile materials, the timing and the sequence of the burial processes of the villa, which is attributed to Emperor Augustus, have been revealed. The sediments filling the villa can be divided into five stratigraphical units (Group1, Group2, Group3A, Group3B, and Group3C) by the presence of soil. The lowermost unit (Group1) directly covering the partially collapsed Roman building includes air-fall deposits, surge deposit, and epiclastic flow deposits. One of charcoals found in this unit give an age of 1500yBP, and the juvenile scoria have the same compositional range as ejecta of the AD472 Sub-plinian eruption, and differ from ejecta of major eruptions. The next three units (Group2, Group3A, and Group3B) include thick epiclastic flow deposits interbedding air-fall deposits. The uppermost unit (Group3C) consists of alternating scoria and ash-fall layers and an overlying ash-fall layer. The petrographical features and the composition of juvenile materials coincide with those of the AD1631 Sub-plinian eruption. From these geological and geochemical features, the burial process of the Roman villa is described as follows. When the AD472 eruption started, the villa had partially collapsed. This damaged building was mantled by an air-fall deposit a few tens of centimeters thick. The remaining building was soon struck by several phases of lahars, and was buried up to a height of 5m. The villa experienced at least five eruptions, and their ejecta and subsequent lahars buried the building further. The last eruption, which completely buried the villa, was the AD1631 eruption. This reconstructed scenario suggests lahars generated just after the eruptions were major agents in the burial of the Roman villa. | |||||
| 書誌情報 |
Bulletin of the Earthquake Research Institute 巻 82, 号 2, p. 119-178, 発行日 2007 |
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| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 00408972 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AN00162258 | |||||
| フォーマット | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | application/pdf | |||||
| 日本十進分類法 | ||||||
| 主題Scheme | NDC | |||||
| 主題 | 051.1 | |||||
| 出版者 | ||||||
| 出版者 | Earthquake Research Institute, University of Tokyo | |||||
| 出版者別名 | ||||||
| 東京大学地震研究所 | ||||||
