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  List of Accepted Contributions - MPRG13 The extrapolation of lab data to nature (co-listed in GD, GMPV & TS)

Please, click Abstract Number to find the corresponding abstract as PDF file; if necessary, download Adobe Acrobat Reader 4.0 first to open the file. Any abstract may be freely reproduced for non-commercial, scientific purposes; however, the moral right of the author(s) to be identified as the author(s) of such abstracts is asserted.

Llana-Fúnez, S.; Brodie, K.H.; Rutter, E.H.; Arkwright, J.C.
Experimental dehydration kinetics of intact lizardite serpentinite specimens under effective stress

Gueydan, F.
Transient creep regime during strain localization: a field and numerical perspective

Sassier, C.; Lefebvre, C.; Leloup, P.H.
Testing paleo-piezometers: constraints from a natural example.

Mondol, N. H.; Bjørlykke, K.; Jahren, J.
Experimental mechanical compaction and elastic properties of smectite, kaolinite and their mixtures - relevance to seismic interpretation and basin modelling

Schiano, P.; Provost, A.; Clocchiatti, R.; Faure, F.
Transcrystalline melt migration driven by natural thermal gradients

Herwegh, M.; Ebert, A.; de Bresser, J.H.P
Microstructural variation in natural mylonites and their consequences for rheological extrapolations from laboratory to nature

Armann, M.; Burlini, L.; Kunze, K.; Burg, J.-P.
Experimental deformation of synthetic rocksalt to large strain in torsion

Delle Piane, C.; Burlini, L.; Kunze, K.
Superimposed deformation of Carrara marble: reverted torsion experiments

Nover, G.
The role of shear movement on graphitisation of organic matter - In-situ analysis done by energy dispersive X-Ray diffraction and electrical impedance spectroscopy

Kellermann Slotemaker, A.; De Bresser, J.H.P
Dynamic grain growth in laboratory experiments, microstructural modelling and naturally deformed rocks

Prior, D; Wightman, R; Little, T
Explaining transient microstructures from the base of the seismogenic zone. What gives: experiment, nature or mechanism models?

Wheeler, J
Models for diffusion creep – the destroyer of crystallographic preferred orientation?

Evans, B.
Scales of microstructure during dislocation creep in minerals

Keulen, N; Stünitz, H; Heilbronner, R
Healing rates of natural and experimental granitoid Fault Gouges.

Keulen, N; Heilbronner, R; Stünitz, H; Ramseyer, K
Microstructures of healed granitoid Fault Gouge – a Combination of Cathodoluminescence and BSE-Contrast SEM Imaging.

Heilbronner, R.; Tullis, J.
Texture dependent grain size in experimentally deformed quartzite

Precigout, J; Gueydan, F; Gapais, D
Strain localisation in the Ronda peridotites induced by grain size reduction and grain boundary sliding

Lippmann-Pipke, J.; Niedermann, S.; Erzinger, J.; Zimmer, M.; Onstott, T.C.
Implications for the timing of gas release: Crush-degassing experiments (lab), continuous gas monitoring (near-field) and analysis of >1.5Ma old crustal fluids (regional), Wits Basin, South Africa

Heilbronner, R.; Menegon, L.
From lab strain rates of quartz to geological strain rates of granites

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