Pressure–temperature–time path of a metapelite from Mefjell, Sør Rondane Mountains, East Antarctica
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- TSUBOKAWA Yumiko
- Graduate School of Environment and Information Sciences, Yokohama National University
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- ISHIKAWA Masahiro
- Graduate School of Environment and Information Sciences, Yokohama National University
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- KAWAKAMI Tetsuo
- Department of Geology and Mineralogy, Graduate School of Science, Kyoto University
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- HOKADA Tomokazu
- National Institute of Polar Research
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- SATISH–KUMAR M.
- Department of Geology, Faculty of Science, Niigata University
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- TSUCHIYA Noriyoshi
- Graduate School of Environmental Studies, Tohoku University
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- GRANTHAM Geoffrey H.
- Department of Geology, University of Johannesburg
抄録
<p>A metapelite preserving prograde and retrograde zoning in garnet from Mefjell, southern Sør Rondane Mountains (SRM), East Antarctica is described in detail and U–Th–Pb geochronological data are presented. Garnet, sillimanite, staurolite and biotite are in textural equilibrium in the matrix. The garnet shows three distinct compositional zones comprising core, mantle and rim. From core to the mantle, the spessartine content represents a bell–shaped profile. From mantle to the rim, spessartine content increases and pyrope decreases. Kyanite is present as tiny inclusions in the garnet core. The core also contains aggregates of sillimanite with radial cracks around them, interpreted to have resulted from the inversion of kyanite. The prograde P–T path recorded in the garnet is heating to approximately 700 °C at 5.6 kbar with a slight increase in pressure. U–Th–Pb dating of monazite grains yields a large range of age distribution between 700 and 540 Ma. The inferred prograde metamorphism of the metapelite sample in this study might be related to subduction and/or tectonic loading explained by a collision tectonic model of the SRM (Osanai et al., 2013).</p>
収録刊行物
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- Journal of Mineralogical and Petrological Sciences
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Journal of Mineralogical and Petrological Sciences 112 (2), 77-87, 2017
一般社団法人 日本鉱物科学会
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詳細情報 詳細情報について
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- CRID
- 1390001206545437184
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- NII論文ID
- 130007348403
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- ISSN
- 13493825
- 13456296
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- HANDLE
- 2433/287366
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- IRDB
- Crossref
- CiNii Articles
- KAKEN
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- 抄録ライセンスフラグ
- 使用不可