Standard

(Negative thermal expansion of crystals (statistics and causes). / Filatov, S. K.

в: Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva, Том 111, № 6, 01.01.1982, стр. 674-681.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Filatov, SK 1982, '(Negative thermal expansion of crystals (statistics and causes).', Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva, Том. 111, № 6, стр. 674-681.

APA

Filatov, S. K. (1982). (Negative thermal expansion of crystals (statistics and causes). Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva, 111(6), 674-681.

Vancouver

Filatov SK. (Negative thermal expansion of crystals (statistics and causes). Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva. 1982 Янв. 1;111(6):674-681.

Author

Filatov, S. K. / (Negative thermal expansion of crystals (statistics and causes). в: Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva. 1982 ; Том 111, № 6. стр. 674-681.

BibTeX

@article{c25dbcc011724f9ebb4107826120d2de,
title = "(Negative thermal expansion of crystals (statistics and causes).",
abstract = "Contraction, rather than expansion, during heating occurs more frequently in monoclinic minerals than in those of other systems. The deformation during heating was measured for LiVO3 (diopside-type structure) and ZrO2 (baddelyite), and discussed for wolframite-hubnerite. In six out of seven monoclinic structural types the deformation consists of a shift of the angle of monoclinicity toward 40o, i.e. towards higher symmetry. The cause of the negative thermal expansion is shear deformation. -R.A.H.",
author = "Filatov, {S. K.}",
year = "1982",
month = jan,
day = "1",
language = "English",
volume = "111",
pages = "674--681",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "6",

}

RIS

TY - JOUR

T1 - (Negative thermal expansion of crystals (statistics and causes).

AU - Filatov, S. K.

PY - 1982/1/1

Y1 - 1982/1/1

N2 - Contraction, rather than expansion, during heating occurs more frequently in monoclinic minerals than in those of other systems. The deformation during heating was measured for LiVO3 (diopside-type structure) and ZrO2 (baddelyite), and discussed for wolframite-hubnerite. In six out of seven monoclinic structural types the deformation consists of a shift of the angle of monoclinicity toward 40o, i.e. towards higher symmetry. The cause of the negative thermal expansion is shear deformation. -R.A.H.

AB - Contraction, rather than expansion, during heating occurs more frequently in monoclinic minerals than in those of other systems. The deformation during heating was measured for LiVO3 (diopside-type structure) and ZrO2 (baddelyite), and discussed for wolframite-hubnerite. In six out of seven monoclinic structural types the deformation consists of a shift of the angle of monoclinicity toward 40o, i.e. towards higher symmetry. The cause of the negative thermal expansion is shear deformation. -R.A.H.

UR - http://www.scopus.com/inward/record.url?scp=0019898040&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0019898040

VL - 111

SP - 674

EP - 681

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 6

ER -

ID: 53958687