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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. 28

Description of sandstones in the Ulaanbaatar area, Mongolia

https://doi.org/10.18999/bulnum.028.03
https://doi.org/10.18999/bulnum.028.03
0db0125f-ffa2-489a-83c1-890e0df97f84
名前 / ファイル ライセンス アクション
No28-3.pdf No28-3.pdf (4.0 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2013-06-11
タイトル
タイトル Description of sandstones in the Ulaanbaatar area, Mongolia
言語 en
著者 Suzuki, Toshiya

× Suzuki, Toshiya

WEKO 48675

en Suzuki, Toshiya

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Nakane, Yuki

× Nakane, Yuki

WEKO 48676

en Nakane, Yuki

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Nuramkhaan, Bakhat

× Nuramkhaan, Bakhat

WEKO 48677

en Nuramkhaan, Bakhat

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Takeuchi, Makoto

× Takeuchi, Makoto

WEKO 48678

en Takeuchi, Makoto

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Tsukada, Kazuhiro

× Tsukada, Kazuhiro

WEKO 48679

en Tsukada, Kazuhiro

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Gonchigdorj, Sersmaa

× Gonchigdorj, Sersmaa

WEKO 48680

en Gonchigdorj, Sersmaa

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Sodnom, Khishigsuren

× Sodnom, Khishigsuren

WEKO 48681

en Sodnom, Khishigsuren

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Nuramkhaan, Manchuk

× Nuramkhaan, Manchuk

WEKO 48682

en Nuramkhaan, Manchuk

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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
抄録
内容記述 The texture and the grain composition of sandstone provide information about the tectonic setting of basins of deposition and associated provenances. The geological history of the Khangay-Khentey belt composed of pre-Carboniferous accretionary complex and Carboniferous shallow-marine strata was linked with the evolution of the Mongol-Okhotsk Ocean. This paper describes the sandstones of the Gorkhi, Altan-Ovoo & Orgioch- Uul Formations and Carboniferous shallow marine system, that occurs around Ulaanbaatar city The sandstones in the Gorkhi and Altan-Ovoo & Orgioch-Uul Formations are classified as feldspathic arenite. They are clast supported and poorly-sorted, with dominantly angular to very angular grains mainly composed of quartz, potassium feldspar, plagioclase and rock fragments of rhyolite and tuff. The modal framework grain analysis shows that sandy detritus was derived from “continental crust” where erosion has cut deep into volcanic cover. The sandstone in the Carboniferous shallow marine system classified as feldspathic wacke is rich in muddy matrix and poorly-sorted, dominantly includes rounded to little angular grains of quartz, potassium feldspar, plagioclase and rock fragments of rhyolite, felsic tuff, andesite and basalt. The Qm-F-Lt diagram suggests that the sandstone is originated from the “transitional arc”. The sandstones from the Gorkhi and Altan-Ovoo & Orgioch-Uul Formations are significantly similar and they can not be distinguished to each other in their textures, grain compositions and poor in rock fragments, and they were originated from the same kinds of source, i.e. continental crust where erosion has cut deep into volcanic cover which related to the subduction of oceanic plate. However, the lithostratigraphies of these formations are quite different each other and they were likely to have been formed at different places, or formed in different ages each other. The volcanism evidenced by the felsic tuff intercalations in the Altan-Ovoo & Orgioch-Uul Formation at the provenance area was likely enough immature which could not provide much volcanic rock fragments to the basin. The sandstone of the “Carboniferous formation,” rich in volcanic rock fragments, strongly indicates that the volcanic activity had developed to supply volcanic rock fragments into the sedimentary basin of this formation.
言語 en
内容記述タイプ Abstract
出版者
言語 ja
出版者 名古屋大学博物館
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
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 10.18999/bulnum.028.03
ID登録タイプ JaLC
ISSN(print)
収録物識別子タイプ PISSN
収録物識別子 1346-8286
書誌情報 ja : 名古屋大学博物館報告

巻 28, p. 27-38, 発行日 2012-12-25
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/18188
識別子タイプ HDL
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