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Special issue"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Shiraishi, Kazuyuki", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "716", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Asami, Masao", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "15136", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Kanaya, Hiroshi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "20394", "nameIdentifierScheme": "WEKO"}]}]}, "item_1_description_1": {"attribute_name": "ページ属性", "attribute_value_mlt": [{"subitem_description": "P(論文)", "subitem_description_type": "Other"}]}, "item_1_description_12": {"attribute_name": "抄録(英)", "attribute_value_mlt": [{"subitem_description": "Syenitic rocks occupying an area of at least 400(km)^2 in the Yamato Mountains, East Antarctica, are classified into three major types on the basis of the field occurrence and petrography; two-pyroxene syenite, clinopyroxene quartz monzo-syenite and clinopyroxene syenite. Major and trace elements Rb, Sr, Zr, Th and U are presented to reveal the petrochemical features of the syenitic rocks. The two-pyroxene syenite which has a charnockitic appearance is the earlier member among the syenitic rocks. The spacial relation between the clinopyroxene quartz monzo-syenite and the clinopyroxene syenite is not observed. All the syenitic rocks show roughly smooth trends in the major elements variation diagrams, but they overlap extensively with increasing SiO_2. The Rb, Th and U contents of the syenitic rocks are similar to those of the average crust, and Sr and Zr are much more enriched than the ordinary granitic rocks. The wide range of SiO_2 in the clinopyroxene quartz monzo-syenite and higher Rb/Sr and K/Rb ratios in the two-pyroxene syenite than the former might not prove the formation of the clinopyroxene quartz monzo-syenite from the two-pyroxene syenite by magmatic differentiation. 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  1. 紀要類
  2. Memoirs of National Institute of Polar Research. Special issue (ISSN 0386-0744)
  3. No.28 (Oct. 1983)

Petrochemical character of the syenitic rocks from the Yamato Mountains, East Antarctica

https://nipr.repo.nii.ac.jp/records/1476
https://nipr.repo.nii.ac.jp/records/1476
91560e9f-62c2-4031-a8aa-2b54474e12dd
名前 / ファイル ライセンス アクション
KJ00000012109.pdf KJ00000012109 (2.1 MB)
license.icon
Item type 紀要論文(ELS) / Departmental Bulletin Paper(1)
公開日 1983-10-01
タイトル
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
ページ属性
内容記述タイプ Other
内容記述 P(論文)
著者名(英) Shiraishi, Kazuyuki

× Shiraishi, Kazuyuki

WEKO 716

en Shiraishi, Kazuyuki

Search repository
Asami, Masao

× Asami, Masao

WEKO 15136

en Asami, Masao

Search repository
Kanaya, Hiroshi

× Kanaya, Hiroshi

WEKO 20394

en Kanaya, Hiroshi

Search repository
著者所属(英)
en
National Institute of Polar Research/Department of Geological Sciences, College of Liberal Arts, Okayama University/Geological Survey of Japan
抄録(英)
内容記述タイプ Other
内容記述 Syenitic rocks occupying an area of at least 400(km)^2 in the Yamato Mountains, East Antarctica, are classified into three major types on the basis of the field occurrence and petrography; two-pyroxene syenite, clinopyroxene quartz monzo-syenite and clinopyroxene syenite. Major and trace elements Rb, Sr, Zr, Th and U are presented to reveal the petrochemical features of the syenitic rocks. The two-pyroxene syenite which has a charnockitic appearance is the earlier member among the syenitic rocks. The spacial relation between the clinopyroxene quartz monzo-syenite and the clinopyroxene syenite is not observed. All the syenitic rocks show roughly smooth trends in the major elements variation diagrams, but they overlap extensively with increasing SiO_2. The Rb, Th and U contents of the syenitic rocks are similar to those of the average crust, and Sr and Zr are much more enriched than the ordinary granitic rocks. The wide range of SiO_2 in the clinopyroxene quartz monzo-syenite and higher Rb/Sr and K/Rb ratios in the two-pyroxene syenite than the former might not prove the formation of the clinopyroxene quartz monzo-syenite from the two-pyroxene syenite by magmatic differentiation. On the other hand, it is possible that the clinopyroxene quartz monzo-syenite and the clinopyroxene syenite may be genetically related judging from their petrochemical similarity.
雑誌書誌ID
収録物識別子タイプ NCID
収録物識別子 AA00733561
書誌情報 Memoirs of National Institute of Polar Research. Special issue

巻 28, p. 183-197, 発行日 1983-10
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