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  1. 極地研刊行誌
  2. 英文誌
  3. 極域地学
  4. Polar geoscience (ISSN 1344-3194)
  5. No.16 (Oct. 2003)

Geochronological evidence for multistage-metamorphic events in ultrahigh-temperature granulites from central Highland Complex, Sri Lanka

https://doi.org/10.15094/00003126
https://doi.org/10.15094/00003126
db806e1c-2c11-4144-bf3f-762efa74fdc7
名前 / ファイル ライセンス アクション
KJ00000044120.pdf KJ00000044120 (2.8 MB)
license.icon
Item type 紀要論文(ELS) / Departmental Bulletin Paper(1)
公開日 2003-10-01
タイトル
言語
言語 eng
キーワード
主題Scheme Other
主題 central Highland Complex
キーワード
主題Scheme Other
主題 Sri Lanka
キーワード
主題Scheme Other
主題 UHT granulites
キーワード
主題Scheme Other
主題 Sm-Nd geochronology
キーワード
主題Scheme Other
主題 multistage metamorphism
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
ID登録
ID登録 10.15094/00003126
ID登録タイプ JaLC
ページ属性
内容記述タイプ Other
内容記述 P(論文)
著者名(英) Sajeev, Krishnan

× Sajeev, Krishnan

WEKO 4463

en Sajeev, Krishnan

Search repository
Osanai, Yasuhito

× Osanai, Yasuhito

WEKO 4398

en Osanai, Yasuhito

Search repository
Suzuki, Satoko

× Suzuki, Satoko

WEKO 43331

en Suzuki, Satoko

Search repository
Kagami, Hiroo

× Kagami, Hiroo

WEKO 65711

en Kagami, Hiroo

Search repository
著者所属(英)
en
Department of Earth and Planetary System Science,Okayama University
著者所属(英)
en
Department of Earth and Planetary System Science, Okayama University
著者所属(英)
en
Graduate School of Science and Technology, Niigata University
著者所属(英)
en
Graduate School of Science and Technology, Niigata University
抄録(英)
内容記述タイプ Other
内容記述 The ultrahigh-temperature (UHT)granulite from the central Highland Complex,Sri Lanka preserves histories of several metamorphic events.The application of geothermobarometries on sapphirine-garnet-orthopyroxene-sillimanite-quartz bearing granulites confirms that metamorphism occurred under the UHT condition. We report a middle Proterozoic age of 1478+-58 Ma from the internal isochron using a garnet core,whole rock and felsic fraction (quartz in the Sm-Nd system from the same rock samples.As this granulite preserves several stages of orthopyroxene formation,the measured isotope composition of orthopyroxene give mixed values.The reference isochron plotted with orthopyroxene and whole rock give an age of 550 Ma.The present results can be interpreted to mean that the middle Proterozoic metamorphic event could have been the thermal peak.During the uplift stage,this granulite might have remetamorphosed at younger stages along with the adjacent rocks.
雑誌書誌ID
収録物識別子タイプ NCID
収録物識別子 AA1130866X
書誌情報 Polar geoscience

巻 16, p. 137-148, 発行日 2003-10
出版者
出版者 National Institute of Polar Research
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