Access the full text.
Sign up today, get DeepDyve free for 14 days.
N. K. Goh H. G. Schnering (1985)
H. G. Schnering, N. K. Goh, and K. Peters, Z. Krist. 172, 153 (1985).
F. Cámara A. P. Khomyakov (2010)
10.3749/canmin.48.2.291Can. Mineral., 48
Bruker APEX (2003)
Bruker APEX2 (Bruker AXS Inc., Madison, Wisconsin, USA, 2003).
H. D. Grundy I. Hassan (1984)
10.1107/S0108768184001683Acta Crystallogr. B, 40
S. M. Antao I. Hassan (2004)
10.2138/am-2004-2-315Am. Mineral., 89
P. Woodward B. Kelly (1976)
10.1039/dt9760001314J. Chem Soc. Dalton Trans., 14
Bruker SAINT (2007)
Bruker SAINT (Bruker AXS Inc., Madison, Wisconsin, USA, 2007).
A. N. Sapozhnikov E. V. Kaneva (2017)
10.1134/S1063774517040071Crystallogr. Rep., 62
T. S. Kabrè B. Leclerc (1975)
10.1107/S0567740875005900Acra Crystallogr. B, 31
J. R. Carruthers P. W. Betteridge (2003)
10.1107/S0021889803021800J. Appl. Crystallogr., 36
G. M. Sheldrick (1996)
SADABS, Program for Empirical Absorption Correction of Area Detector Data
J. Gonzalez-Platas R. J. Angel (2014)
R. J. Angel, J. Gonzalez-Platas, and M. Alvaro, Z. Krist. 229, 405 (2014).
E. V. Kaneva A. N. Sapozhnikov (2017)
10.1180/minmag.2016.080.106Mineral. Mag., 81
V. G. Ivanov A. N. Sapozhnikov (1991)
Zap. Vseross. MineralO-va, 120
Z. Natur. P. Bötttcher and R. Keller (1984)
P. Bötttcher and R. Keller, Z. Natur. 39b, 577 (1984).
Z. Natur. P. Bötttcher and G. Trampe (1985)
P. Bötttcher and G. Trampe, Z. Natur. 40b, 321 (1985).
Z. Krist. P. Böttcher (1979)
P. Böttcher, Z. Krist. 150, 65 (1979).
Abstract— A Low-temperature (100 K) analysis of the crystalline structures of Cl-bystrite and sulfhydrylbystrite has been carried out, and the data obtained have been compared with the room-temperature characteristics of these minerals. The framework deformations are considered as a result of change in the ditrigonality of six-membered tetrahedral rings: the decrease in the unit-cell volume at low temperature is determined mainly by the increase in the ditrigonality (compression) of six-membered framework rings. Oblique and vertical (corrugated) rings are distorted to a greater extent than horizontal rings. The deformation mechanisms is shown to be the same for the frameworks of bystrite-subgroup minerals and the sodalite framework.
Crystallography Reports – Springer Journals
Published: Dec 1, 2018
Keywords: Crystallography and Scattering Methods
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.