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NESPOLO, Massimo, TAKEDA, Hiroshi (1999) Inhomogeneous mica polytypes. 8-layer polytype of the 2M1 structural series determined by the Periodic Intensity Distribution (PID) analysis of the X-ray diffraction pattern. Mineralogical Journal, 21 (3) 103-118 doi:10.2465/minerj.21.103

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Reference TypeJournal (article/letter/editorial)
TitleInhomogeneous mica polytypes. 8-layer polytype of the 2M1 structural series determined by the Periodic Intensity Distribution (PID) analysis of the X-ray diffraction pattern.
JournalMineralogical Journal
AuthorsNESPOLO, MassimoAuthor
TAKEDA, HiroshiAuthor
Year1999Volume21
Issue3
PublisherJapan Association of Mineralogical Sciences
DOIdoi:10.2465/minerj.21.103Search in ResearchGate
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Mindat Ref. ID81982Long-form Identifiermindat:1:5:81982:8
GUID0
Full ReferenceNESPOLO, Massimo, TAKEDA, Hiroshi (1999) Inhomogeneous mica polytypes. 8-layer polytype of the 2M1 structural series determined by the Periodic Intensity Distribution (PID) analysis of the X-ray diffraction pattern. Mineralogical Journal, 21 (3) 103-118 doi:10.2465/minerj.21.103
Plain TextNESPOLO, Massimo, TAKEDA, Hiroshi (1999) Inhomogeneous mica polytypes. 8-layer polytype of the 2M1 structural series determined by the Periodic Intensity Distribution (PID) analysis of the X-ray diffraction pattern. Mineralogical Journal, 21 (3) 103-118 doi:10.2465/minerj.21.103
In(1999) Mineralogical Journal Vol. 21 (3) Japan Association of Mineralogical Sciences

See Also

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Nespolo, Massimo, Takeda, Hiroshi, Kogure, Toshihiro, Ferraris, Giovanni (1999) Periodic intensity distribution (PID) of mica polytypes: symbolism, structural model orientation and axial settings. Acta Crystallographica Section A Foundations of Crystallography, 55 (4). 659-676 doi:10.1107/s0108767398017735
NESPOLO, Massimo (1999) Analysis of family reflections of OD mica polytypes, and its application to twin identification. Mineralogical Journal, 21 (2) 53-85 doi:10.2465/minerj.21.53
NESPOLO, Massimo, TAKEDA, Hiroshi, FERRARIS, Giovanni, KOGURE, Toshihiro (1997) Composite twins of lM mica: derivation and identiffcation. Mineralogical Journal, 19 (4) 173-186 doi:10.2465/minerj.19.173
Kogure, Toshihiro, Nespolo, Massimo (1999) A TEM study of long-period mica polytypes: determination of the stacking sequence of oxybiotite by means of atomic resolution images and Periodic Intensity Distribution (PID) Acta Crystallographica Section B Structural Science, 55 (4) 507-516 doi:10.1107/s0108768199003845
MIN, Eun-gi, OHSUMI, Kazumasa (1976) New CdI2 polytype, 20H7: its structure and X-ray diffraction pattern. Mineralogical Journal, 8 (3) 151-157 doi:10.2465/minerj.8.151
Takeda, Hiroshi (1967) Review of Complex Mica Polytypes. Journal of the Mineralogical Society of Japan, 8. 39-41 doi:10.2465/gkk1952.8.special1_39
Sadanaga, Ryoichi, Takeda, Hiroshi (1969) Description of Mica Polytypes by New Unit Layers. Journal of the Mineralogical Society of Japan, 9 (3) 177-184 doi:10.2465/gkk1952.9.177
Nespolo, Massimo, Ferraris, Giovanni, Takeda, Hiroshi (2000) Identification of two allotwins of mica polytypes in reciprocal space through the minimal rhombus unit. Acta Crystallographica Section B Structural Science, 56 (4) 639-647 doi:10.1107/s0108768100002044
Nespolo, Massimo (2001) Perturbative Theory of Mica Polytypism. Role of the M2 Layer in the Formation of Inhomogeneous Polytypes. Clays and Clay Minerals, 49 (1) 1-23 doi:10.1346/ccmn.2001.0490101
TABIRA, Yasunori, MARUMO, Fumiyuki (1992) Local structures around Fe and Cr atoms in glasses of the systems CaMgSi2O6-CaFeAlSiO6 and CaMgSi2O6/CaCrAlSiO6 determined by X-ray diffraction method. Mineralogical Journal, 16 (1) 21-27 doi:10.2465/minerj.16.21
SUGIYAMA, Kazumasa, WASEDA, Yoshio (1989) Structural study of the metamict states by X-ray diffraction: In the case of naegite. Mineralogical Journal, 14 (7) 303-309 doi:10.2465/minerj.14.303
 
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