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GEOREF RECORD

X-ray and HRTEM structure analysis of orientite

Marcello Mellini, Stefano Merlino and Marco Pasero
X-ray and HRTEM structure analysis of orientite
American Mineralogist (February 1986) 71 (1-2): 176-187

Abstract

Orientite is orthorhombic, a 9.044(10), b 6.09(7), c 19.031(20) A, with ideal crystal chemical formula: 265Ca (sub 8) Mn (sub 10) (super 3+) ((SiO (sub 4) ) (sub 3) (Si (sub 3) O (sub 10) ) (sub 3) (OH) (sub 10) ).4H (sub 2) O in the unit cell. A structural model with space group P2mm was proposed on the basis of chemical data, X-ray and HRTEM (High Resolution Transmission Electron Microscopy) analyses. The model was refined to R = 0.069, using 650 independent reflections collected with MoKalpha radiation. The structure is characterized by the regular alternation of the c direction of two distinct structural modules and by the extensive occurrence of microvoids, elongated in the c direction located at the borders between misfitting crystal regions.


ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 71
Serial Issue: 1-2
Title: X-ray and HRTEM structure analysis of orientite
Affiliation: Univ. Pisa, Dip. Sci. Terra, Pisa, Italy
Pages: 176-187
Published: 198602
Text Language: English
Publisher: Mineralogical Society of America, Washington, DC, United States
References: 14
Accession Number: 1986-034637
Categories: Mineralogy of silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 2 tables
N19°49'60" - N23°15'00", W85°00'00" - W74°00'00"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United KingdomTwickenhamUKUnited Kingdom
Update Code: 1986
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