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  1. 掲載誌一覧
  2. 鹿児島大学理学部紀要
  3. vol.35
  1. 理学部
  2. 理学部・紀要論文

Clay Mineralogy of the Weathered Materials from the Serpentinized Peridotite in Minglanilla, Cebu Province, Philippines

http://hdl.handle.net/10232/797
http://hdl.handle.net/10232/797
03892920-54f2-4a64-bd50-e7fbd17f1beb
名前 / ファイル ライセンス アクション
KJ00000042914.pdf KJ00000042914.pdf (1.2 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2008-08-01
タイトル
タイトル Clay Mineralogy of the Weathered Materials from the Serpentinized Peridotite in Minglanilla, Cebu Province, Philippines
著者 ALETA, Dennis Gerald A.

× ALETA, Dennis Gerald A.

WEKO 74099

ALETA, Dennis Gerald A.

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TOMITA, Katsutoshi

× TOMITA, Katsutoshi

WEKO 74100

TOMITA, Katsutoshi

Search repository
ALETA, Josephine T.

× ALETA, Josephine T.

WEKO 74101

ALETA, Josephine T.

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LUCERO, Abraham R.

× LUCERO, Abraham R.

WEKO 74102

LUCERO, Abraham R.

Search repository
KAWANO, Motoharu

× KAWANO, Motoharu

WEKO 74103

KAWANO, Motoharu

Search repository
言語
言語 eng
キーワード
主題Scheme Other
主題 Serpentine
キーワード
主題Scheme Other
主題 chlorite
キーワード
主題Scheme Other
主題 talc
キーワード
主題Scheme Other
主題 smectite
キーワード
主題Scheme Other
主題 saprock
キーワード
主題Scheme Other
主題 saprolite
キーワード
主題Scheme Other
主題 peridotite
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 departmental bulletin paper
要約(Abstract)
内容記述タイプ Other
内容記述 Serpentinized peridotite is an ultramafic rock that intrudes, during Cretaceous time, as widely scattered diapiric bodies along the principal fault zones of central Cebu, Philippines. This rock is exposed to chemical weathering in tropical conditions and through the leaching reactions leave a friable mantle of in situ regolithic materials. It is envisaged that the serpentine was derived from a pyroxene-rich peridotite. The <2μm clay fraction of four regolithic materials obtained from this rockmass in Camp 7,Minglanilla were examined by means of x-ray diffractometry (XRD), differential thermal analysis (DTA), thermogravimetric analysis (TGA), scanning electron microscopy (SEM) and energy dispersive x-ray (EDX). Results of analyses showcase the polymineralic and heterogeneous nature of the weathered specimens with serpentine predominating, and could be differentiated possibly into two distinct assemblages. The first assemblage consists principally of serpentine-talc-chlorite-smectite and the second assemblage consists of serpentine-chlorite-smectite. Kaolinite is present in trace amounts in both suites. It is strongly perceived that these secondary minerals are genetic products from cadence of chemical alterations of primary ferromagnesian minerals particularly orthopyroxenes and clinopyroxenes. The two assemblages appear to interpret the weathering reaction stages that the hypermelanic peridotite protolith had undergone. The first assemblage possibly corresponds to saprock (friable rock zone) which suggests the earlier stage and lesser intensity of weathering while the second assemblage possibly relates to saprolite (argillized solifluxed zone) which indicates the more advanced and greater intensity of weathering. The transition from the first assemblage to the second assemblage appears telescoping as indicated by the gradating loss of talc in the system. Both assemblages appear highly magnesian, ferruginous, siliceous and non-aluminous.
収録雑誌名 鹿児島大学理学部紀要=Reports of the Faculty of Science, Kagoshima University

巻 35, p. 17-30
作成日
日付 2002-12-30
ISSN
収録物識別子タイプ ISSN
ISSN 13456938
NII書誌ID(雑誌)
収録物識別子タイプ NCID
NC ID AA11246904
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
NDC
主題Scheme NDC
主題 400
NIIsubject
主題Scheme Other
主題 自然科学
公開者・出版者
出版者 鹿児島大学
公開者よみ
公開者よみ カゴシマ ダイガク
公開者別名
公開者別名 Kagoshima University
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