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1. �ｿｽ_�ｿｽ�ｿｽ�ｿｽHRTEM�ｿｽR�ｿｽ�ｿｽ�ｿｽg�ｿｽ�ｿｽ�ｿｽX�ｿｽg�ｿｽﾌシ�ｿｽ~�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ[�ｿｽV�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾆ観察�ｿｽ�ｿｽ

�ｿｽ_�ｿｽ�ｿｽ�ｿｽHRTEM�ｿｽR�ｿｽ�ｿｽ�ｿｽg�ｿｽ�ｿｽ�ｿｽX�ｿｽg�ｿｽﾌシ�ｿｽ~�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ[�ｿｽV�ｿｽ�ｿｽ�ｿｽ�ｿｽ(�ｿｽ�ｿｽj�ｿｽﾆ観察�ｿｽ�ｿｽ�ｿｽi�ｿｽ�ｿｽ�ｿｽj
Simulation program: MacTempas, acceleration voltage: 200kV, Cs: 0.5mm, spread of focus: 10nm, beam convergence: 1mrad, specimen thickness: 2.5nm, defocus value: -40m. TEM used: JEM-2010UHR
Kogure, T.: "Investigation of micas using advanced TEM." in: Micas: Crystal Chemistry & Metamorphic Petrology, Reviews in Mineralogy and Petrology Vol. 46, Mineralogical Society of America, Washington, D.C., (2002) 281-312.

2. �ｿｽ�ｿｽ�ｿｽ_�ｿｽ�ｿｽ(KAl₂Si₃AlO₁₀(OH)₂)�ｿｽ�ｿｽ<100>�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ

�ｿｽ�ｿｽ�ｿｽ_�ｿｽ�ｿｽiKAl2Si3AlO10(OH)2)�ｿｽ�ｿｽ<110>�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ�ｿｽiJEM-2010UHR at 200kV)
(unpublished data)

3. �ｿｽ�ｿｽ�ｿｽ_�ｿｽ齟��ｿｽﾌ費ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽJ�ｿｽﾊゑｿｽ�ｿｽd�ｿｽq�ｿｽﾆ射にゑｿｽ�ｿｽ�ｿｽ�ｿｽﾅゑｿｽ�ｿｽﾄゑｿｽ�ｿｽ�ｿｽ�ｿｽl�ｿｽq�ｿｽ�捉ゑｿｽ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ

Time –resolved HRTEM images of biotite recorded along Xi-axis, showing that a micro (001) cleavage is being extinguished by electron radiation.
Kogure, T.: "On the structure of cleaved surface in biotite", Mineral. J., 19 (1997) 155-164�ｿｽD

4. �ｿｽC�ｿｽ�ｿｽ�ｿｽC�ｿｽg-1M �ｿｽ�ｿｽ[100]�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ

�ｿｽC�ｿｽ�ｿｽ�ｿｽC�ｿｽg-1M �ｿｽ�ｿｽ[100]�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ�ｿｽD�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾉ層�ｿｽ�ｿｽ]�ｿｽﾉゑｿｽ�ｿｽﾏ層�ｿｽ�ｿｽ�ｿｽﾗゑｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽD
(unpublished data)

5. �ｿｽA�ｿｽX�ｿｽs�ｿｽh�ｿｽ�ｿｽ�ｿｽC�ｿｽg(�ｿｽi�ｿｽg�ｿｽ�ｿｽ�ｿｽE�ｿｽ�ｿｽ�ｿｽO�ｿｽ�ｿｽ�ｿｽﾊ体雲�ｿｽ�ｿｽ)�ｿｽ�ｿｽYi-�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ

�ｿｽA�ｿｽX�ｿｽs�ｿｽh�ｿｽ�ｿｽ�ｿｽC�ｿｽg�ｿｽi�ｿｽi�ｿｽg�ｿｽ�ｿｽ�ｿｽE�ｿｽ�ｿｽ�ｿｽO�ｿｽ�ｿｽ�ｿｽﾊ体雲�ｿｽ�ｿｽj�ｿｽ�ｿｽYi-�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ�ｿｽA�ｿｽX�ｿｽe�ｿｽ�ｿｽ�ｿｽX�ｿｽN�ｿｽﾅ趣ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽw�ｿｽﾔはカ�ｿｽ�ｿｽ�ｿｽE�ｿｽ�ｿｽ�ｿｽﾅ撰ｿｽL�ｿｽ�ｿｽ�ｿｽ黷ｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾅ、�ｿｽ�ｿｽ�ｿｽﾌゑｿｽ�ｿｽﾟ層�ｿｽﾔの包ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾌ包ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ瘧ｱ�ｿｽ蛯ｫ�ｿｽ�ｿｽ�ｿｽﾈゑｿｽ�ｿｽﾄゑｿｽ�ｿｽ�ｿｽD
Kogure, T., Y. Banno and R. Miyawaki: "Interlayer structure in aspidolite, the Na analogue of phlogopite", Eur. J. Mineral., 16 (2004) 891-897.

6. �ｿｽ�ｿｽ�ｿｽs�ｿｽh�ｿｽ�ｿｽ�ｿｽC�ｿｽg�ｿｽ�ｿｽYi�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ

�ｿｽ�ｿｽ�ｿｽs�ｿｽh�ｿｽ�ｿｽ�ｿｽC�ｿｽg�ｿｽ�ｿｽYi�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ�ｿｽD�ｿｽ�ｿｽﾍ鯉ｿｽ�ｿｽﾌ托ｿｽ�ｿｽA�ｿｽ�ｿｽ�ｿｽﾍフ�ｿｽB�ｿｽ�ｿｽ�ｿｽ^�ｿｽ[�ｿｽﾉゑｿｽ�ｿｽ�晶趣ｿｽ�ｿｽm�ｿｽC�ｿｽY�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾌ．�ｿｽﾏ層�ｿｽs�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽAn60°�ｿｽﾌ様�ｿｽX�ｿｽﾈ層�ｿｽ�ｿｽ]�ｿｽ�ｿｽ�ｿｽN�ｿｽ�ｿｽ�ｿｽﾄゑｿｽ�ｿｽ驍ｱ�ｿｽﾆゑｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾄゑｿｽ�ｿｽ�ｿｽD
Kogure, T. and M. Bunno: "Investigation of polytype occurrence in lepidolite by using Electron Back-Scattered Diffraction (EBSD) ", Am. Mineral., 89 (2004) 1680-1684.

7. �ｿｽ_�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ_�ｿｽ齟��ｿｽﾉ鯉ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ2:1�ｿｽw�ｿｽ�ｿｽ�ｿｽﾌ費ｿｽ�ｿｽﾊ体層�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ2�ｿｽ�ｿｽ�ｿｽﾌ四�ｿｽﾊ体シ�ｿｽ[�ｿｽg�ｿｽ�ｿｽ�ｿｽq�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ\�ｿｽ�ｿｽ�ｿｽﾌ面鯉ｿｽ�ｿｽ�ｿｽ

�ｿｽ_�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ_�ｿｽ�ｿｽioxybiotite�ｿｽj�ｿｽ�ｿｽ�ｿｽﾉ鯉ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽA2:1�ｿｽw�ｿｽ�ｿｽ�ｿｽﾌ費ｿｽ�ｿｽﾊ体層�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ2�ｿｽ�ｿｽ�ｿｽﾌ四�ｿｽﾊ体シ�ｿｽ[�ｿｽg�ｿｽ�ｿｽ�ｿｽq�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ\�ｿｽ�ｿｽ�ｿｽﾌ面鯉ｿｽ�ｿｽﾗ．�ｿｽ�ｿｽ�ｿｽ�ｿｽXi�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽA�ｿｽE�ｿｽ�ｿｽYi�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ迪ｩ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾗゑｿｽHRTEM�ｿｽ�ｿｽ�ｿｽD
Kogure, T. and M. Nespolo: "Atomic structures of planar defects in oxybiotite", Am. Mineral., 86 (2001) 336-340.

8. �ｿｽﾐとつのセ�ｿｽ�ｿｽ�ｿｽh�ｿｽi�ｿｽC�ｿｽg(K (Mg, Fe²⁺, Fe³⁺)₂ Si₄O₁₀(OH)₂)�ｿｽﾌ鯉ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ[100]�ｿｽ�ｿｽ[310]�ｿｽ�ｿｽ�ｿｽ迪ｩ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ

�ｿｽﾐとつのセ�ｿｽ�ｿｽ�ｿｽh�ｿｽi�ｿｽC�ｿｽg(K (Mg, Fe²⁺, Fe³⁺)₂ Si₄O₁₀(OH)₂)�ｿｽﾌ鯉ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ[100]�ｿｽi�ｿｽ�ｿｽj�ｿｽ�ｿｽ[310]�ｿｽi�ｿｽ�ｿｽ�ｿｽj�ｿｽ�ｿｽ�ｿｽ迪ｩ�ｿｽ�ｿｽHRTEM�ｿｽ�ｿｽ�ｿｽD[100]�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾍ積層�ｿｽs�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾈゑｿｽ�ｿｽ�ｿｽ�ｿｽA[310]�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾅは托ｿｽ�ｿｽ�ｿｽ�ｿｽﾌ積層�ｿｽs�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾄゑｿｽ�ｿｽ�ｿｽA�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾌ不�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾗゑｿｽ180°�ｿｽﾌ層�ｿｽ�ｿｽ]�ｿｽﾅでゑｿｽ�ｿｽﾄゑｿｽ�ｿｽ驍ｱ�ｿｽﾆゑｿｽ�ｿｽ�か�ｿｽ�ｿｽD
Kogure, T., J. Kameda and V.A. Drits : "Stacking faults with 180° layer rotation in celadonite, iron and magnesium-rich dioctahedral mica", Clays Clay Miner., 56 (2008) 612-621.

9.�ｿｽZ�ｿｽ�ｿｽ�ｿｽh�ｿｽi�ｿｽC�ｿｽg�ｿｽ�ｿｽ800°C�ｿｽﾅ会ｿｽ�ｿｽM�ｿｽ�ｿｽ�ｿｽ驍ｱ�ｿｽﾆにゑｿｽ�ｿｽ`�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽA�ｿｽV�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ\�ｿｽ�ｿｽ�ｿｽ�ｿｽ2:1�ｿｽw�ｿｽiYi�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽj

�ｿｽZ�ｿｽ�ｿｽ�ｿｽh�ｿｽi�ｿｽC�ｿｽg�ｿｽ�ｿｽ800°C�ｿｽﾅ会ｿｽ�ｿｽM�ｿｽ�ｿｽ�ｿｽ驍ｱ�ｿｽﾆにゑｿｽ�ｿｽ`�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽA�ｿｽV�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ\�ｿｽ�ｿｽ�ｿｽ�ｿｽ2:1�ｿｽw�ｿｽiYi�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽj�ｿｽD�ｿｽR�ｿｽ�ｿｽ�ｿｽg�ｿｽ�ｿｽ�ｿｽX�ｿｽg�ｿｽ�ｿｽ�ｿｽ1�ｿｽw�ｿｽ�ｿｽ�ｿｽ�ｿｽ2�ｿｽ�ｿｽ�ｿｽﾌ四�ｿｽﾊ体シ�ｿｽ[�ｿｽg�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽS�ｿｽﾉ鯉ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽ�ｿｽﾄゑｿｽ�ｿｽ驍ｱ�ｿｽﾆゑｿｽ�ｿｽ�か�ｿｽ�ｿｽD
Kogure, T., J. Kameda and V.A. Drits: "Novel 2:1 structure of phyllosilicates formed by annealing Fe³⁺, Mg-rich dioctahedral mica", Am. Mineral., 92 (2007) 1531-1534.