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  1. H150 博物館
  2. H150b 紀要
  3. 名古屋大学博物館報告
  4. 26

シリア段丘に見られる石膏(Gypsum: CaSO4・2H2O)ノジュールの形成と環境についての一考察

https://doi.org/10.18999/bulnum.026.09
bde58f73-d47c-4e00-b998-869cb46b6287
名前 / ファイル ライセンス アクション
No26-9.pdf No26-9.pdf (1.7 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2011-04-27
タイトル
タイトル シリア段丘に見られる石膏(Gypsum: CaSO4・2H2O)ノジュールの形成と環境についての一考察
その他のタイトル
その他のタイトル Formation of Gypsum nodule in Euphrates flood plain, Syria
著者 吉田, 英一

× 吉田, 英一

WEKO 40114

吉田, 英一

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YOSHIDA, Hidekazu

× YOSHIDA, Hidekazu

WEKO 40115

YOSHIDA, Hidekazu

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星野, 光雄

× 星野, 光雄

WEKO 40116

星野, 光雄

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HOSHINO, Mitsuo

× HOSHINO, Mitsuo

WEKO 40117

HOSHINO, Mitsuo

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田中, 剛

× 田中, 剛

WEKO 40118

田中, 剛

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TANAKA, Tsuyoshi

× TANAKA, Tsuyoshi

WEKO 40119

TANAKA, Tsuyoshi

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中村, 俊夫

× 中村, 俊夫

WEKO 40120

中村, 俊夫

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NAKAMURA, Toshio

× NAKAMURA, Toshio

WEKO 40121

NAKAMURA, Toshio

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束田, 和弘

× 束田, 和弘

WEKO 40122

束田, 和弘

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TSUKADA, Kazuhiro

× TSUKADA, Kazuhiro

WEKO 40123

TSUKADA, Kazuhiro

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齊藤, 毅

× 齊藤, 毅

WEKO 40124

齊藤, 毅

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SAITO, Takeshi

× SAITO, Takeshi

WEKO 40125

SAITO, Takeshi

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桂田, 祐介

× 桂田, 祐介

WEKO 40126

桂田, 祐介

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KATSURADA, Yusuke

× KATSURADA, Yusuke

WEKO 40127

KATSURADA, Yusuke

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抄録
内容記述 Euphrates f lood plain includes modern channels, oxbow lakes, banks and marshes, and contains of river terraces. These sedimentary phases of terraces are mainly unconsolidated dry silty to fine sand materials with poorly sorted gravels provided from the Bishiri Mountains. The study of sedimentary features is therefore enable us to know the environment of Tell Gahnem al- Ali had built. From the last field survey of terraces, we found many types of gypsum nodules in the soft terrace sediments. The size of nodule is about 1-2 cm diameter with several cm long. Sometimes, it has several tens cm grown vertically to the sedimentary layer and cross the bedding plane. The occurrence suggests that the nodule has been formed after the deposition of terrace sediments as following steps. First of all, the sediments deposited about several Ka ago. The age of sedimentation is estimated by the structural relation with Tell Gahnem al-Ali and the building process. Of course with the isotope carbon data, if available, would be shown more precise time of the building and sedimentation periods. After the deposition, sediments still has certain about of pore-water (wet) and the composition is presumably becoming very high contents of Ca. This is estimated by the present river water contents of Euphrates, and also the dissolution of gypsum that has provided from the basement rocks. During the compaction of continuing the terrace deposition, pore-water has been isolated and concentrated beyond the solubility limit of calcium. On the other hand, sediments contain also sulfate from the organic matters. Due to the diagenetic alteration such geochemical setting had formed, finally hydrous calcium sulfate has been precipitated and the nodule has been formed. It is however, the shape of nodule is quite unique, i.e. similar to the root plaque of plant growing in the flood plane, and that the precise formation is still necessary to analyze.
内容記述タイプ Abstract
出版者
出版者 名古屋大学博物館
言語
言語 jpn
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 10.18999/bulnum.026.09
ID登録タイプ JaLC
ISSN(print)
収録物識別子タイプ ISSN
収録物識別子 1346-8286
書誌情報 名古屋大学博物館報告

巻 26, p. 79-83, 発行日 2010-12-25
著者版フラグ
値 publisher
URI
識別子 http://www.num.nagoya-u.ac.jp/outline/report.html
識別子タイプ URI
URI
識別子 http://hdl.handle.net/2237/14681
識別子タイプ HDL
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