Letter. Direct observations of pseudomorphism: compositional and textural evolution at a fluid- solid interface

By C. Putnis, K. Tsukamoto, Y. Nishimura. 2005

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Mineral Replacement Reactions (2009, methodology): “Real time phase-shift interferometry (Putnis et al. 2005) also confirms that the dissolution and precipitation process is confined to a fluid boundary layer at the reaction interface, which has a different composition to the fluid in the bulk.”
Mechanism of leached layer formation during chemical weathering of silicate minerals (2012, background): “The existence of such an interfacial fl uid layer, defi ned by steep cation concentration gradients close to the surface of the mineral, was observed by Putnis et al. (2005) during mineral replacement reactions using real-time phase-shift interferometry.”
Letter: Gold-telluride nanoparticles revealed in arsenic-free pyrite (2012, background): “…(Cook and Chryssoulis 1990) in pyrite for Au exploitation have driven substantial research aimed at characterizing, quantifying, and understanding how and why invisible gold, either as lattice bound or as NPs, occurs (Palenik et al. 2004; Reich et al. 2005; Large et al. 2009; Deditius et al. 2011).”
The AFm phase in Portland cement (2007, background): “[33] have recently described a novel mechanism for pseudomorphic replacement of one phase by another and this may have relevance for themechanism of transformations amongstAFmphases driven by anion exchanges.”