Research Article| October 01, 2015 Experimental evidence for rock layering development by pressure solution Jean-Pierre Gratier; Jean-Pierre Gratier 1ISTerre, Université Grenoble Alpes, 38041 Grenoble Cedex 9, France2ISTerre, CNRS, 38041 Grenoble Cedex 9, France Search for other works by this author on: GSW Google Scholar Catherine Noiriel; Catherine Noiriel 3Géosciences Environnement Toulouse, Observatoire Midi-Pyrénées, Université Paul Sabatier, CNRS, IRD, 31400 Toulouse, France Search for other works by this author on: GSW Google Scholar François Renard François Renard 1ISTerre, Université Grenoble Alpes, 38041 Grenoble Cedex 9, France2ISTerre, CNRS, 38041 Grenoble Cedex 9, France4Physics of Geological Processes, Department of Geosciences, University of Oslo, 0316 Oslo, Norway Search for other works by this author on: GSW Google Scholar Author and Article Information Jean-Pierre Gratier 1ISTerre, Université Grenoble Alpes, 38041 Grenoble Cedex 9, France2ISTerre, CNRS, 38041 Grenoble Cedex 9, France Catherine Noiriel 3Géosciences Environnement Toulouse, Observatoire Midi-Pyrénées, Université Paul Sabatier, CNRS, IRD, 31400 Toulouse, France François Renard 1ISTerre, Université Grenoble Alpes, 38041 Grenoble Cedex 9, France2ISTerre, CNRS, 38041 Grenoble Cedex 9, France4Physics of Geological Processes, Department of Geosciences, University of Oslo, 0316 Oslo, Norway Publisher: Geological Society of America Received: 17 Feb 2015 Revision Received: 29 Jul 2015 Accepted: 30 Jul 2015 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2015 Geological Society of America Geology (2015) 43 (10): 871–874. https://doi.org/10.1130/G36713.1 Article history Received: 17 Feb 2015 Revision Received: 29 Jul 2015 Accepted: 30 Jul 2015 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Jean-Pierre Gratier, Catherine Noiriel, François Renard; Experimental evidence for rock layering development by pressure solution. Geology 2015;; 43 (10): 871–874. doi: https://doi.org/10.1130/G36713.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Natural deformation of rocks is commonly associated with development of mineralogical layering, leading to irreversible transformations of their microstructure. The mechanisms of such chemical differentiation processes during diagenesis, tectonics, metamorphism, or fault differentiation remain poorly understood, as they are difficult to reproduce experimentally due to the very slow kinetics involved. This paper shows that development of differentiated layering, similar to that observed in natural deformation, is stress driven and can be obtained from indenter experiments. Samples of (1) gypsum plaster mixed with clay, and (2) natural diatomite loosely interbedded with volcanic ash, saturated with aqueous solutions in equilibrium, were subjected to loading for several months at 40 °C and 150 °C, respectively. X-ray microtomography and scanning electron microscopy observations show that layering develops by a self-organized pressure solution process. Stress-driven dissolution of the soluble minerals (either gypsum or silica) is initiated in the areas initially richer in insoluble species (clay or volcanic ash), as diffusive mass transfer along the interface between soluble and insoluble minerals is much faster than along the healed boundaries of the soluble minerals. The passive concentration of the insoluble minerals amplifies the dissolution along layers oriented perpendicularly to the maximum compressive stress. Conversely, in areas with an initial low content of insoluble minerals and clustered soluble minerals, dissolution is slower. Consequently, these areas are less deformed; they host the re-deposition of the soluble species and act as rigid objects that concentrate both stress and dissolution near their boundaries, thus amplifying the differentiation and the development of layered microstructures. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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