C
Catherine Lerouge
Researcher at University of Strasbourg
Publications - 101
Citations - 2054
Catherine Lerouge is an academic researcher from University of Strasbourg. The author has contributed to research in topics: Dolomite & Pyrite. The author has an hindex of 21, co-authored 94 publications receiving 1661 citations.
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A robust model for pore-water chemistry of clayrock
Eric C. Gaucher,Christophe Tournassat,F.J. Pearson,Philippe Blanc,Catherine Crouzet,Catherine Lerouge,Scott Altmann +6 more
TL;DR: In this paper, an approach for calculating the pore-water compositions of clayrocks from laboratory-measured properties of core samples, including their leachable Cl and SO4 concentrations and analysed exchangeable cations, and from mineral and cation exchange equilibria based on the formation mineralogy is presented.
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Shrimp U–Pb zircon age evidence for Paleoproterozoic sedimentation and 2.05 Ga syntectonic plutonism in the Nyong Group, South-Western Cameroon: consequences for the Eburnean–Transamazonian belt of NE Brazil and Central Africa
Catherine Lerouge,Alain Cocherie,S.F. Toteu,J. Penaye,Jean-Pierre Milesi,Robert Tchameni,Emmanuel N. Nsifa,C. Mark Fanning,Etienne Deloule +8 more
TL;DR: The Nyong Group of the NW corner of the Congo craton is a metasedimentary and metaplutonic rock unit that underwent a high-grade tectono-metamorphic event at ∼2050-Ma associated with charnockite formation as mentioned in this paper.
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On the nature of structural disorder in calcium silicate hydrates with a calcium/silicon ratio similar to tobermorite
Sylvain Grangeon,Francis Claret,Catherine Lerouge,Fabienne Warmont,Tsutomu Sato,Sohtaro Anraku,Chiya Numako,Yannick Linard,Bruno Lanson +8 more
TL;DR: In this article, four calcium silicate hydrates (C-S-H) with structural calcium/silicon (Ca/Si) ratios ranging from 0.82 +/- 0.02 to 0.87 +/- 0.02 were synthesized at room temperature, 50, 80, and 110 degrees C.
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In situ interaction between different concretes and Opalinus Clay
TL;DR: In this paper, interfaces of Opalinus Clay, a potential host-rock in Switzerland, and three concrete formulations emplaced in the Cement-Clay Interaction (CI) Experiment at the Mont Terri Underground Laboratory (St. Ursanne, Switzerland) were analyzed after 2.2 years of interaction.
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5: Late Variscan mineralizing systems related to orogenic processes: The French Massif Central
TL;DR: In this article, two types of gold deposit can be distinguished on the basis of their depth of emplacement: deep-seated gold deposits developed under lithostatic to hydrostatic pressure during rapid exhumation, and shallow gold deposits emplaced under hydrostatic pressures with no significant uplift.