Abstract
Transmission electron microscopic study of synthetic CaAl2Ge2O8-feldspar revealed two types of antiphase domains: type “b”-antiphase domains with the displacement vector 1/2 [110] and type “c”-antiphase domains with the displacement vector 1/2 [111]. The “b”-domains were on the order of 0.1 μm in size, while the “c”-domains displayed wall to wall distances mostly between 0.1 and 1 μm. The formation of the two types of antiphase domains is due to reductions in translational symmetry associated with the phase transitions \(C\bar 1 \to I\bar 1 \to P\bar 1\). The antiphase domain textures of CaAl2Ge2O8-feldspar are very similar to the textures found in natural and synthetic anorthite, CaAl2Si2O8.
Similar content being viewed by others
References
Adlhart W, Frey F, Jagodzinski H (1980) X-ray and neutron investigations of the \(P\bar 1 - I\bar 1\) transition in pure anorthite. Acta Crystallogr A36:450–460
Bambauer HU, Kroll H, Nager HE, Pentinghaus H (1974) Feld-spat-Mischkristalle — Eine Übersicht. Bull Mineral 97:313–345
Heuer AH, Nord GL (1976) Polymorphic phase transitions in minerals. In: Wenk HR (ed) Electron Microscopy in Minerals. Springer, Berlin Heidelberg New York, pp 274–303
John RJ (1986) Zur Ordnungskinetik in Anorthit (CaAl2Si2O8) und Wollastonite (CaSiO3). Doctoral Thesis, submitted to the Fachbereich Geowissenschaften und Geographie der Technischen Hochschule Darmstadt
Kroll H, Müller WF (1980) X-ray and electron-optical investigation of synthetic high-temperature plagioclases. Phys Chem Minerals 5:255–277
Müller WF, John RJ, Kroll H (1984) On the origin and growth of antiphase domains in anorthite. Bull Mineral 107:489–494
Müller WF, Wenk HR, Bell WL, Thomas G (1973) Analysis of the displacement vectors of antiphase domain boundaries in anorthites (CaAl2Si2O8). Contrib Mineral Petrol 40:63–74
Müller WF, Wlotzka F (1982) Mineralogical study of the Leoville meteorite (CV3): macroscopic texture and transmission electron microscopic observations. Lunar Planet Sci 13:910–911
Pentinghaus H (1976) T3+/T4+-disorder and nonstoichiometry in alkaline earth feldspars A2+[T 3+2 T 4+2 O8]. Third European Crystallographic Meeting, Collected Abstracts, 63–64
Pentinghaus H (1980) Polymorphie in den feldspatbildenden Systemen A+ T3+ T 4+3 O8 und A2+ T 3+2 T 4+2 O8. Habilitationsschrift im Fachbereich Chemie der Universität Münster
Ribbe PH (1983) Average structures of alkali and plagioclase feldspars: systematics and applications. In: Brown WL (ed) Feldspars and Feldspathoids, NATO ASI series, Series C, Vol 137, D Reidel Publishing Company, Dordrecht, Holland, pp 1–54
Smith JV (1974) Feldspar Minerals. Vol 1: Crystal structure and physical properties. Springer, Berlin Heidelberg New York
Smith JV (1984) Phase relations of plagioclase feldspars. In: Brown WL (ed) Feldspars and Feldspathoids, NATO ASI series, Series C, Vol 137, D Reidel Publishing Company, Dordrecht, Holland, pp 55–94
Wenk HR, Kroll H (1984) Analysis of \(P\bar 1,I\bar 1\) and \(C\bar 1\) plagioclase structures. Bull Mineral 107:467–487
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Müller, W.F., Vojdan-Shemshadi, Y. & Pentinghaus, H. Transmission electron microscopic study of antiphase domains in CaAl2Ge2O8-Feldspar. Phys Chem Minerals 14, 235–237 (1987). https://doi.org/10.1007/BF00307987
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF00307987