Hostname: page-component-cd9895bd7-jn8rn Total loading time: 0 Render date: 2024-12-23T23:51:07.404Z Has data issue: false hasContentIssue false

Analyzing the Growth of Magmatic Crystals — An Electron Microprobe Analysis Study

Published online by Cambridge University Press:  14 March 2018

Robert Sturm*
Affiliation:
Department of Materials Engineering and Physics, University of Salzburg, Austria

Extract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Since the pioneering mineralogical and crystallographic studies of the 1960s and 1970s it has been regarded as a fundamental tenant of earth sciences that the growth of minerals, and especially of magmatic mineral phases, depends upon the physico-chemical state of the growth environment. Meanwhile, based on extensive empirical and experimental approaches, some factors controlling crystal growth and, as a consequence of that, crystal shape or morphology can be detected and documented. Therefore, the chemistry and temperature of the growth environment, as well as its content of volatile phases, have been found to be key to understanding the crystallization processes.

Type
Research Article
Copyright
Copyright © Microscopy Society of America 2007

References

(1) Sunagawa, I. (1984): Growth of crystals in nature. In: Sunagawa, I. (ed.), Materials science of the Earth's interior, Terra Scientific, Tokyo, 63–15.Google Scholar
(2) Caruba, R. (1978): Morphologie de zircons synthétiques: corrélations pétrogénétiques. Can. Mineral. 16, 315323.Google Scholar
(3) Vavra, G. (1994): Systematics of internal zircon morphology in major Variscan granitoid types. Contrib. Mineral. Petrol. 117, 331344.CrossRefGoogle Scholar
(4) Speer, J. A. (1982): Zircon. In: Ribbe, P. H. (ed.), Orthosilicates, MSA, Washington DC, 67112.CrossRefGoogle Scholar
(5) Pupin, J. P., Turco, G. (1972): Une typologie originale du zircon accessoire. Bull. Soc. Fr. Minéral Cristallogr. 95, 348359.Google Scholar
(6) Pupin, J. P. (1980): Zircon and granite petrology. Contrib. Mineral. Petrol. 73, 207220.CrossRefGoogle Scholar
(7) Vavra, G. (1990): On the kinematics of zircon growth and its petrogenetic significance: a cathodoluminescence study. Contrib. Mineral. Petrol. 106, 9099.CrossRefGoogle Scholar
(8) Paterson, B. A., Stephens, W. E., Rogers, G., Williams, I. S., Hinton, R. W., Herd, D. A. (1992): The nature of zircon inheritance in 2 granite plutons. Trans. R. Soc. Edinburgh : EarthSci.Edinburgh : Earth Sci. 83, 459471.CrossRefGoogle Scholar
(9) Sturm, R. (1999): Longitudinal and cross section of zircon: a new method for the investigation of morphological evolutional trends. Schweiz. Mineral. Petrogr. Mitt. 79, 309316.Google Scholar