PRESSURE-INDUCED PHASE-TRANSITION IN BETA-EUCRYPTITE (LIALSIO4)

被引：14

作者：

MOROSIN, B ^{[1
]}

PEERCY, PS ^{[1
]}

机构：

[1] SANDIA LABS,ALBUQUERQUE,NM 87115

来源：

关键词：

D O I：

10.1016/0375-9601(75)90506-X

中图分类号：

O4 [物理学];

学科分类号：

0702 ;

摘要：

引用

页码：147 / 148

页数：2

共 7 条

[1] HORNYAK EJ, 1969, THESIS U MICHIGAN
[2] JOHNSON RT, 1975, B AM PHYS SOC, V20, P330
[3] MOROSIN B, 1971, S CAROLINA M AM CRYS
[4] STRUCTURAL RELATIONS BETWEEN LOW-TEMPERATURE AND HIGH-TEMPERATURE FORMS OF BETA-EURCYPTITE (LIALSIO4) AND LOW AND HIGH QUARTZ .2. HIGH-TEMPERATURE FORM OF BETA-EUCRYPTITE AND HIGH QUARTZ
SCHULZ, H
TSCHERRY, V
[J]. ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL CRYSTALLOGRAPHY AND CRYSTAL CHEMISTRY, 1972, B 28 (JUL15): : 2174 - &
[5] AVERAGE AND SUPER STRUCTURE OF BETA EUCRYPTITE (LIALSIO4) .1. AVERAGE STRUCTURE
TSCHERRY, V
SCHULZ, H
LAVES, F
[J]. ZEITSCHRIFT FUR KRISTALLOGRAPHIE KRISTALLGEOMETRIE KRISTALLPHYSIK KRISTALLCHEMIE, 1972, 135 (3-4): : 161 - &
[6] TSCHERRY V, 1972, Z KRIST, V135, P172
[7] WEAVER HT, TO BE PUBLISHED