The thermodynamics of the I $$ \overline{1} $$ –P $$ \overline{1} $$ phase transition in Ca-rich plagioclase from an assessment of the spontaneous strain
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,General Materials Science
Link
http://link.springer.com/content/pdf/10.1007/s00269-012-0524-x.pdf
Reference36 articles.
1. Adlhart W, Frey F, Jagodzinski H (1980a) X-ray and neutron investigations of the $$P \overline{1} $$ – $$I \overline{1} $$ transition in pure anorthite. Acta Cryst A 36:450–460
2. Adlhart W, Frey F, Jagodzinski H (1980b) X-ray and neutron investigations of the $$P \overline{1} $$ – $$I \overline{1} $$ transition in anorthite with low albite content. Acta Cryst A 36:461–470
3. Aizu K (1970) Determination of the state parameters and formulation of spontaneous strain for ferroelastics. J Phys Soc Jpn 28:706–716
4. Angel RJ (1988) High-pressure structure of anorthite. Am Miner 73:1114–1119
5. Angel RJ (1992) Order-disorder and the high-pressure $$P \overline{1} $$ – $$I \overline{1} $$ transition in anorthite. Am Miner 77:923–929
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2. Revisiting theI{\overline {\bf 1}} structures of high-temperature Ca-rich plagioclase feldspar – a single-crystal neutron and X-ray diffraction study;Acta Crystallographica Section B Structural Science, Crystal Engineering and Materials;2018-03-17
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