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  1. 広島大学の刊行物
  2. Journal of science of the Hiroshima University. Series C, Earth and planetary sciences
  3. 11巻1号

Micro-textures of Hematite in the Liesegang Rocks, Found in Pyrophyllite Deposits, Shobara District, Southwest Japan.

https://doi.org/10.15027/53160
https://doi.org/10.15027/53160
06838ff4-2622-4f4a-b489-2e358ebac224
名前 / ファイル ライセンス アクション
JSHUCE_11-1_33.pdf JSHUCE_11-1_33.pdf (3.3 MB)
Item type デフォルトアイテムタイプ_(フル)(1)
公開日 2023-03-18
タイトル
タイトル Micro-textures of Hematite in the Liesegang Rocks, Found in Pyrophyllite Deposits, Shobara District, Southwest Japan.
言語 en
作成者 YAMASHITA, Yoshiko

× YAMASHITA, Yoshiko

en YAMASHITA, Yoshiko

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OHKAWA, Makio

× OHKAWA, Makio

en OHKAWA, Makio

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KITAGAWA, Ryuji

× KITAGAWA, Ryuji

en KITAGAWA, Ryuji

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NAKASHIMA, Akio

× NAKASHIMA, Akio

en NAKASHIMA, Akio

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TAKENO, Setsuo

× TAKENO, Setsuo

en TAKENO, Setsuo

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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
内容記述
内容記述 Characteristic micro-textures of hematite found commonly in the Liesegang rocks collected from pyrophyllite ore deposits, Shobara district, southwest Japan were investigated. Detailed observations of the Liesegang rocks under the high magnification reflection microscope with oil immersion lens reveal that almost all of opaque grains are composed of needle-shaped very fine crystals with less than few microns in width and 5-10 microns in length. Moreover, doughnut-like texture, which is characteristic in the Liesegang rock (Yamashita et al., 1996), is mainly composed of the needle-shaped fine crystals. In many cases, the rings are composed of radiated aggregates of the needle-shaped hematite crystals. The size of the most predominant rings is less than 10µm in diameter, and double, triple and multi rings are also common. The optical properties of these opaque crystals under the reflection microscope are almost similar to those of ordinary hematite, i.e., weak but noticeable bireflectance and distinct anisotropism (e.g., Uytenbogaardt, 1971). X-ray powder diffraction data indicate that most of the opaque minerals are hematite with small amount of goethite. However, under the reflection microscope, distinguishment of the two minerals is not possible.
言語 en
出版者
出版者 Hiroshima University
言語
言語 eng
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
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
ID登録
ID登録 10.15027/53160
ID登録タイプ JaLC
収録物識別子
収録物識別子タイプ ISSN
収録物識別子 0075-4374
収録物識別子
収録物識別子タイプ NCID
収録物識別子 AA11095875
開始ページ
開始ページ 33
書誌情報 Journal of science of the Hiroshima University. Series C, Earth and planetary sciences
Journal of science of the Hiroshima University. Series C, Earth and planetary sciences

巻 11, 号 1, p. 33-40, 発行日 1998-03-30
旧ID 53160
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