Standard

Crystallographic Analysis of the Datolite (CaBSiO 4 OH) to Okaymalite (Ca 2 B 2 SiO 7 ) Structural Transformation under Dehydration. / Borisov, S. V.; Pervukhina, N. V.; Magarill, S. A.

In: Journal of Structural Chemistry, Vol. 60, No. 2, 01.02.2019, p. 268-274.

Research output: Contribution to journal › Article › peer-review

Harvard

Borisov, SV, Pervukhina, NV & Magarill, SA 2019, 'Crystallographic Analysis of the Datolite (CaBSiO 4 OH) to Okaymalite (Ca 2 B 2 SiO 7 ) Structural Transformation under Dehydration', Journal of Structural Chemistry, vol. 60, no. 2, pp. 268-274. https://doi.org/10.1134/S0022476619020112

APA

Borisov, S. V., Pervukhina, N. V., & Magarill, S. A. (2019). Crystallographic Analysis of the Datolite (CaBSiO 4 OH) to Okaymalite (Ca 2 B 2 SiO 7 ) Structural Transformation under Dehydration. Journal of Structural Chemistry, 60(2), 268-274. https://doi.org/10.1134/S0022476619020112

Vancouver

Borisov SV, Pervukhina NV, Magarill SA. Crystallographic Analysis of the Datolite (CaBSiO 4 OH) to Okaymalite (Ca 2 B 2 SiO 7 ) Structural Transformation under Dehydration. Journal of Structural Chemistry. 2019 Feb 1;60(2):268-274. doi: 10.1134/S0022476619020112

Author

Borisov, S. V. ; Pervukhina, N. V. ; Magarill, S. A. / Crystallographic Analysis of the Datolite (CaBSiO 4 OH) to Okaymalite (Ca 2 B 2 SiO 7 ) Structural Transformation under Dehydration. In: Journal of Structural Chemistry. 2019 ; Vol. 60, No. 2. pp. 268-274.

BibTeX

@article{9ea03e0db39540d2a16663c3a2a631bd,
title = "Crystallographic Analysis of the Datolite (CaBSiO 4 OH) to Okaymalite (Ca 2 B 2 SiO 7 ) Structural Transformation under Dehydration",
abstract = " The common “template” of datolite and okayamalite structures is a column-ribbon formed by alternating empty and Si occupied oxygen tetrahedra interconnected by common edges. The columns consolidate with their environment into crystalline structures largely due to the influence of the local symmetry of SiO 4 and BO 4 tetrahedra. As a result, mirror symmetry pseudo-planes of monoclinic datolite transform into okayamalite m planes; the pseudo-axis 4 ¯ becomes the principal axis, whereas both structures contain glide planes and cation sublattices close in size. ",
keywords = "cationic sublattices, crystallographic analysis, datolite -okayamalite transformation, local symmetry, stability factors and symmetry",
author = "Borisov, {S. V.} and Pervukhina, {N. V.} and Magarill, {S. A.}",
year = "2019",
month = feb,
day = "1",
doi = "10.1134/S0022476619020112",
language = "English",
volume = "60",
pages = "268--274",
journal = "Journal of Structural Chemistry",
issn = "0022-4766",
publisher = "Springer GmbH & Co, Auslieferungs-Gesellschaf",
number = "2",

}

RIS

TY - JOUR

T1 - Crystallographic Analysis of the Datolite (CaBSiO 4 OH) to Okaymalite (Ca 2 B 2 SiO 7 ) Structural Transformation under Dehydration

AU - Borisov, S. V.

AU - Pervukhina, N. V.

AU - Magarill, S. A.

PY - 2019/2/1

Y1 - 2019/2/1

N2 - The common “template” of datolite and okayamalite structures is a column-ribbon formed by alternating empty and Si occupied oxygen tetrahedra interconnected by common edges. The columns consolidate with their environment into crystalline structures largely due to the influence of the local symmetry of SiO 4 and BO 4 tetrahedra. As a result, mirror symmetry pseudo-planes of monoclinic datolite transform into okayamalite m planes; the pseudo-axis 4 ¯ becomes the principal axis, whereas both structures contain glide planes and cation sublattices close in size.

AB - The common “template” of datolite and okayamalite structures is a column-ribbon formed by alternating empty and Si occupied oxygen tetrahedra interconnected by common edges. The columns consolidate with their environment into crystalline structures largely due to the influence of the local symmetry of SiO 4 and BO 4 tetrahedra. As a result, mirror symmetry pseudo-planes of monoclinic datolite transform into okayamalite m planes; the pseudo-axis 4 ¯ becomes the principal axis, whereas both structures contain glide planes and cation sublattices close in size.

KW - cationic sublattices

KW - crystallographic analysis

KW - datolite -okayamalite transformation

KW - local symmetry

KW - stability factors and symmetry

UR - http://www.scopus.com/inward/record.url?scp=85065293299&partnerID=8YFLogxK

U2 - 10.1134/S0022476619020112

DO - 10.1134/S0022476619020112

M3 - Article

AN - SCOPUS:85065293299

VL - 60

SP - 268

EP - 274

JO - Journal of Structural Chemistry

JF - Journal of Structural Chemistry

SN - 0022-4766

IS - 2

ER -

ID: 20166342