Grain boundary plane populations in minerals: the example of wet NaCl after low strain deformation

Author:

Pennock G. M.,Coleman M.,Drury M. R.,Randle V.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference61 articles.

1. Bons AJ, Drury MR, Schrijvers D, Zwart HJ (1990) Implications for mass transport processes during low temperature metamorphism. Phys Chem Miner 17:402–408. doi: 10.1007/BF00212208

2. Breunese JN, Van Eijs RMHE, De Meer S, Kroon IC (2003) Observation and prediction of the relation between salt creep and land subsidence in solution mining—the Barradeel case. Solution Mining Research Institute, Conference, Chester, pp 38–57

3. Carter NL, Kronenberg AK, Ross JV, Wiltschko DV (1990) Control of fluids on deformation of rocks. In: Knipe RJ, Rutter EH (eds) Deformation mechanisms, rheology and tectonics, vol 54. The Geological Society, London, Special Publication, Leeds, pp 1–13

4. De Meer S, Spiers CJ, Nakashima S (2005) Structure and diffusive properties of fluid-filled grain boundaries: an in-situ study using infrared (micro) spectroscopy. Earth Planet Sci Lett 232(3–4):403–414. doi: 10.1016/j.epsl.2004.12.030

5. Drury MR, van Roermund HLM (1989) Fluid assisted recrystallization in upper mantle peridotite xenoliths from kimberlites. J Petrol 30:133–152

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