On dynamic self-organization: examples from magmatic and other geochemical systems

Standard Liesegang banding is the display of parallel bands of precipitate formed periodically when co-precipitate ions interdiffuse in a gel medium. The most striking resemblance with Liesegang patterns in Nature lies in the diverse scenery of banded textural features commonly observed in some geol...

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Bibliographic Details
Main Authors: Rabih F. Sultan, Abdel-Fattah, M. Abdel-Rahman
Format: Article
Language:English
Published: Marcílio Alves
Series:Latin American Journal of Solids and Structures
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1679-78252013000100006&lng=en&tlng=en