HYDROTHERMAL INTERACTION OF WYOMING BENTONITE AND OPALINUS CLAY

Author:

Sauer KirstenORCID,Caporuscio Florie,Rock Marlena,Cheshire Michael,Jové-Colón Carlos

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Soil Science,Water Science and Technology

Reference64 articles.

1. Adler, M., Mäder, U. K., & Waber, H. N. (1999). High-pH alteration of argillaceous rocks: an experimental study. Schweizerische Mineralogische und Petrographische Mitteilungen, 79, 445–454.

2. Benning, L. G., Wilkin, R. T., & Barnes, H. L. (2000). Solubility and stability of zeolites in aqueous solution: II. Calcic clinoptilolite and mordenite. American Mineralogist, 85, 495–508. https://doi.org/10.2138/am-2000-0411 .

3. Bish, D. L., & Aronson, J. L. (1993). Paleogeothermal and paleohydrologic conditions in silicic tuff from Yucca Mountain, Nevada. Clays and Clay Minerals, 41, 148–161. https://doi.org/10.1346/CCMN.1993.0410204 .

4. Bossart, P.J. & Thury, M. (2008). Mont Terri Rock Laboratory: Project, Programme 1996 to 2007 and Results, no. 3. Reports of the Swiss Geological Survey, Wabern.

5. Bossart, P. & Milnes, A.G. (2017). Mont Terri Rock Laboratory, 20 Years: Two Decades of Research and Experimentation on Claystones for Geological Disposal of Radioactive Waste (Vol. 5): Birkhäuser.

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