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  1. B100 理学部/理学研究科
  2. B100d 学位論文
  3. 博士論文(理博・論理博)

Geochemical characteristics and depositional environments of cherts and associated rocks from the Franciscan and Shimanto Terranes

http://hdl.handle.net/2237/6571
http://hdl.handle.net/2237/6571
96a7c292-5bf9-4c5e-a391-fafffdf7247f
名前 / ファイル ライセンス アクション
ot3111.pdf ot3111.pdf (3.7 MB)
Item type 学位論文 / Thesis or Dissertation(1)
公開日 2006-06-21
タイトル
タイトル Geochemical characteristics and depositional environments of cherts and associated rocks from the Franciscan and Shimanto Terranes
言語 en
その他のタイトル
その他のタイトル フランシスカン帯と四万十帯のチャート及びそれに付隨する岩石の地球化学的特徴と堆積環境
言語 ja
著者 Yamamoto, Koshi

× Yamamoto, Koshi

WEKO 12475

en Yamamoto, Koshi

Search repository
山本, 鋼志

× 山本, 鋼志

WEKO 12476

ja 山本, 鋼志

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
抄録
内容記述 Yamamoto, K, 1987. Geochemical characteristics and depositional environments of cherts and associated rocks in the Franciscan and Shimanto Terranes. Sediment. Geol., 51: Analyses of 122 Jurassic-Cretaceous rock samples from the Franciscan Terrane, California, and 24 Cretaceous samples from the Shimanto Terrane, southwest Japan, show that the cherts and associated rocks accompanied by pillow basalts are enriched in Fe and Mn which may have been derived from hydrothermal activities. The results of the fraction analyses for terrigenous, basaltic, hydrothermal, and biogenic end-members in the Franciscan rocks show that hydrothermal emanations caused iron and manganese enrichment in the rock samples and played an important role in the formation of siliceous rocks. Vertical variations of the hydrothermal fraction and TiO2-normalized values for hydrothermal elements such as Fe, Mn, Ni, Zn, Y and Pb show a possibility that the bedded cherts of the Franciscan Terrane were deposited in a hydrothermal field on or near some active oceanic ridge, for more than 30 Ma and were a remnant slice of oceanic crust added to the North American continent. On the other hand, from the field occurrences and vertical variations of TiO2-normalized values of hydrothermal elements, the Shimanto rocks are inferred to have been deposited in a hemipelagic environment such as marginal and inter-arc basins.
言語 en
内容記述タイプ Abstract
内容記述
内容記述 名古屋大学博士学位論文 学位の種類:理学博士 (論文) 学位授与年月日:昭和61年12月25日
言語 ja
内容記述タイプ Other
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_db06
タイプ doctoral thesis
書誌情報
発行日 1986-12-25
学位名
言語 ja
学位名 理学博士
学位授与機関
学位授与機関識別子Scheme kakenhi
学位授与機関識別子 13901
言語 ja
学位授与機関名 名古屋大学
言語 en
学位授与機関名 Nagoya University
学位授与年度
学位授与年度 1986
学位授与年月日
学位授与年月日 1986-12-25
学位授与番号
学位授与番号 乙第3111号
フォーマット
application/pdf
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/6571
識別子タイプ HDL
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