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Theories of Crystal Growth

  • J. P. Bard
Part of the Petrology and Structural Geology book series (PESG, volume 1)

Abstract

The transition from the ‘nucleus’ phase to the ‘crsytal’ phase is performed through a progressive addition of atoms or molecules at the surface of the nucleus. In a system where liquid → solid transformations are produced, nuclei that have not been absorbed grow faster if the energy level is raised to the high temperatures or if the surrounding solution is oversaturated. In systems with solild → solid transformations, processes of crystal growth are more complicated. As in heterogenous nucleation, they depend on several variables which also define the size and morphology of the newly formed minerals (blast).

Keywords

Crystal Growth Metamorphic Rock Igneous Rock Pressure Solution Differential Stress 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© D. Reidel Publishing Company, Dordrecht, Holland 1986

Authors and Affiliations

  • J. P. Bard
    • 1
  1. 1.Université des Sciences et Techniques du LanguedocMontpellier IIFrance

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