PRELIMINARY REPORT ON STRUCTURES OF FOREFINGER POINT, ENDERBY LAND, EAST ANTARCTICA
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概要
- 論文の詳細を見る
Granulite-facies metamorphic rocks of Forefinger Point, which lie on the Casey Bay coastline in Enderby Land, have been affected by three stages of folding, shear zone formation, and intrusion of pegmatite. The peak metamorphic structural evolution was characterized by the development of F_n isoclinal to close buckling folds. This deformation was associated with the coexistence of orthopyroxene+sillimanite±quartz, and was followed by the formation of cordierite and symplectites of cordierite+sapphirine, orthopyroxene+cordierite+sapphirine in response to subsequent isothermal decompression. These symplectic intergrowths are generally unstrained except in some cordierite domains where cordierite exhibits a weak mineral lineation, implying that intense ductile deformation had ceased before the decompressional reactions : orthopyroxene+sillimanite+quartz=cordierite, orthopyroxene+sillimanite=cordierite+sapphirine, garnet+quartz=orthopyroxene+cordierite. Although the Forefinger Point granulites have undergone high strain deformation under peak metamorphic conditions, they experienced only low and local strain deformation after peak metamorphism. The post-peak-metamorphic structural evolution was characterized by the development of F_<n+1> open to gentle buckling folds, narrow shear zones and emplacement of pegmatite.
- 国立極地研究所の論文
著者
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Fraser G
Research School Of Earth Sciences Australian National University
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Motoyoshi Yoichi
National Institute of Polar Research
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Ishikawa Masahiro
Geological Institute, Yokohama National University
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Ishikawa Masahiro
Institute Of Geology And Paleontology Faculty Of Science Tohoku University:(present Address)geologic
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Ishikawa M
Yokohama National Univ. Yokohama Jpn
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FRASER Geoffrey
Research School of Earth Sciences, Australian National University
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Motoyoshi Y
National Inst. Polar Res. Tokyo Jpn
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Fraser Geoffrey
Research School Of Earth Sciences Australian National University
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Ishikawa Masahiro
Institute Of Geology And Paleontology Faculty Of Science Tohoku University
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