@article{oai:nipr.repo.nii.ac.jp:00002533,
 author = {タガイ, トクヘイ and タケダ, ヒロシ and タチカワ, オサム and カミヌマ, カツタダ / and TAGAI, Tokuhei and TAKEDA, Hiroshi and TACHIKAWA, Osamu and KAMINUMA, Katsutada and KYLE, P.R.},
 journal = {Proceedings of the NIPR Symposium on Antarctic Geosciences},
 month = {Sep},
 note = {P(論文), 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.},
 pages = {66--72},
 title = {MICROSTRUCTURE AND PHASE TRANSITION OF CALCIC ANORTHOCLASE FROM MOUNT EREBUS, ANTARCTICA},
 volume = {1},
 year = {1987}
}