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  1. H150 博物館
  2. H150a 雑誌掲載論文
  3. 学術雑誌

Use of fracture filling mineral assemblages for characterizing water-rock interactions during exhumation of an accretionary complex: An example from the Shimanto Belt, southern Kyushu Japan

http://hdl.handle.net/2237/25101
http://hdl.handle.net/2237/25101
b718c35f-4767-4e26-8233-c58dd075209e
名前 / ファイル ライセンス アクション
Ono_et_al2016.pdf Ono_et_al2016.pdf ファイル公開:2018/06/01 (6.9 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2016-11-25
タイトル
タイトル Use of fracture filling mineral assemblages for characterizing water-rock interactions during exhumation of an accretionary complex: An example from the Shimanto Belt, southern Kyushu Japan
言語 en
著者 Ono, Takuya

× Ono, Takuya

WEKO 67492

en Ono, Takuya

Search repository
Yoshida, Hidekazu

× Yoshida, Hidekazu

WEKO 67493

en Yoshida, Hidekazu

Search repository
Metcalfe, Richard

× Metcalfe, Richard

WEKO 67494

en Metcalfe, Richard

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
権利
言語 en
権利情報 © 2016. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/
キーワード
主題Scheme Other
主題 Fracture fillings
キーワード
主題Scheme Other
主題 Assemblage
キーワード
主題Scheme Other
主題 Accretionary complex
キーワード
主題Scheme Other
主題 Formation process
抄録
内容記述 Various fracture filling minerals and secondary minerals in fracture walls were formed by fluid-rock interaction during the exhumation of the Palaeogene Shimanto Belt of Kyushu, Japan, which is located in an accretionary complex. Each mineral formed under favourable geological conditions and can be used to estimate the conditions of accretion and formation of the related rock sequences. Petrographic observations, mineralogical and geochemical analyses were made on fracture filling minerals and secondary minerals from boreholes of ca. 140 m depth, drilled in the Shimanto Belt. Results reveal that the secondary minerals were formed in three major stages distinguished by the sequential textural relationships of the minerals and the interpreted environment of mineral formation. Filling mineral assemblages show that the studied rock formation has been subducted to a depth of several km and the temperature reached was ca. 200–300 °C. After the subduction, the rock formation was uplifted and surface acidic water penetrated up to 80 m beneath the present ground surface. The acid water dissolved calcite fracture filling minerals to form the present groundwater flow-paths, which allowed recent wall rock alteration to occur. The results shown here imply that filling mineral assemblages can be an effective tool to evaluate the environmental changes during exhumation of an accretionary complex.
言語 en
内容記述タイプ Abstract
出版者
言語 en
出版者 Elsevier
言語
言語 eng
資源タイプ
資源タイプresource http://purl.org/coar/resource_type/c_6501
タイプ journal article
出版タイプ
出版タイプ AM
出版タイプResource http://purl.org/coar/version/c_ab4af688f83e57aa
DOI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 https://doi.org/10.1016/j.jsg.2016.04.009
ISSN
収録物識別子タイプ PISSN
収録物識別子 0191-8141
書誌情報 en : Journal of Structural Geology

巻 87, p. 81-94, 発行日 2016-06
著者版フラグ
値 author
URI
識別子 http://doi.org/10.1016/j.jsg.2016.04.009
識別子タイプ DOI
URI
識別子 http://hdl.handle.net/2237/25101
識別子タイプ HDL
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