Speleogenetic effects of interaction between deeply derived fracture-conduit flow and intrastratal matrix flow in hypogene karst settings

In carbonate rocks, especially in those with high primary porosity such as most Cenozoic carbonates, the interaction between deeply derived rising flow through sub-vertical fracture-controlled conduits and intrastratal matrix flow of shallower systems can invoke mixing cor- rosion and result in prom...

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Bibliographic Details
Main Authors: Tymokhina Elizaveta, Amelichev Gennadiy, Klimchouk Alexander
Format: Article
Language:English
Published: University of South Florida Libraries 2012-07-01
Series:International Journal of Speleology
Subjects:
Online Access:http://scholarcommons.usf.edu/cgi/viewcontent.cgi?article=1067&context=ijs

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