MICROSTRUCTURE AND PHASE TRANSITION OF CALCIC ANORTHOCLASE FROM MOUNT EREBUS, ANTARCTICA
スポンサーリンク
概要
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Monoclinic-triclinic inversion and exsolution phenomena in calcic anorthoclase were investigated by means of high temperature X-ray diffraction, X-ray microprobe analysis and analytical transmission electron microscope on natural calcic anorthoclase from Mout Erebus, Antarctica. Mt. Erebus anorthoclase is the most calcic one-phase anorthoclase which was twinned according to the albite-and pericline-laws in the course of monoclinic-triclinic inversion, whose temperature was measured to be 750℃. The occurrence of the one-phase anorthoclase was closely related with the eruption mechanism of Mt. Erebus.
- 国立極地研究所の論文
著者
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Takeda Hiroshi
Mineralogical Institute, University of Tokyo
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KAMINUMA Katsutada
National Institute of Polar Research
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Tagai Tokuhei
Mineralogical Institute Faculty Of Science University Of Tokyo
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Tachikawa Osamu
Mineralogical Institute Faculty Of Science University Of Tokyo
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KYLE P.R.
Department of Geoscience, New Mexico Institute of Mining and Technology
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Kyle P.r.
Department Of Geoscience New Mexico Institute Of Mining And Technology
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Takeda Hiroshi
Mineralogical Institute Faculty Of Science University Of Tokyo
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