The role of grain boundaries and transient porosity in rocks as fluid pathways for reaction front propagation

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The role of grain boundaries and transient porosity in rocks as fluid pathways for reaction front propagation

The pseudomorphic replacement of Carrara marble by calcium phosphates was used as a model system in order to study the influence of different fluid pathways for reaction front propagation induced by fluid–rock interaction. In this model, grain boundaries present in the rock as well as the transient...

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Bibliographic Details
Main Authors:	Jonas, L., John, T., King, H., Geisler, T., Putnis, Andrew
Format:	Journal Article
Published:	Elsevier Science BV 2014
Subjects:	apatite marble fluidpathways oxygenisotopes hydrothermalreplacement
Online Access:	http://hdl.handle.net/20.500.11937/41122

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