Tectonic structure of the “Main Fault” in the Opalinus Clay, Mont Terri rock laboratory (Switzerland)
暂无分享,去创建一个
[1] V. Dietze,et al. Litho- and biostratigraphy of the Opalinus Clay and bounding formations in the Mont Terri rock laboratory (Switzerland) , 2017, Swiss Journal of Geosciences.
[2] F. Amann,et al. High-resolution mini-seismic methods applied in the Mont Terri rock laboratory (Switzerland) , 2017, Swiss Journal of Geosciences.
[3] Peter Connolly,et al. Mont Terri rock laboratory, 20 years of research: introduction, site characteristics and overview of experiments , 2017, Swiss Journal of Geosciences.
[4] C. Nussbaum,et al. Geochemical signature of paleofluids in microstructures from Main Fault in the Opalinus Clay of the Mont Terri rock laboratory, Switzerland , 2017, Swiss Journal of Geosciences.
[5] C. Nussbaum,et al. Microstructures and deformation mechanisms in Opalinus Clay: insights from scaly clay from the Main Fault in the Mont Terri Rock Laboratory (CH) , 2016 .
[6] M. Voutilainen,et al. The Internal Architecture and Permeability Structures of Faults in Shale Formations , 2016 .
[7] A. Berger,et al. Linking megathrust earthquakes to brittle deformation in a fossil accretionary complex , 2015, Nature Communications.
[8] M. Sintubin,et al. Evolution of microstructure and porosity in faulted Opalinus Clay , 2015 .
[9] C. Vollmer,et al. Microstructural evolution of an incipient fault zone in Opalinus Clay: Insights from an optical and electron microscopic study of ion-beam polished samples from the Main Fault in the Mt-Terri Underground Research Laboratory , 2014 .
[10] François Renard,et al. Postseismic pressure solution creep: Evidence and time‐dependent change from dynamic indenting experiments , 2014 .
[11] R. Thöny. Geomechanical analysis of excavation-induced rock mass behavior of faulted opalinus clay at the Mont Terri underground rock laboratory (Switzerland) , 2014 .
[12] F. Chester,et al. Structure and Composition of the Plate-Boundary Slip Zone for the 2011 Tohoku-Oki Earthquake , 2013, Science.
[13] Zeshan Ismat. Block-supported cataclastic flow within the upper crust , 2013 .
[14] C. Marone,et al. Shear zones in clay-rich fault gouge: A laboratory study of fabric development and evolution , 2013 .
[15] J. Urai,et al. Pore morphology and distribution in the Shaly facies of Opalinus Clay (Mont Terri, Switzerland): Insights from representative 2D BIB–SEM investigations on mm to nm scale , 2013 .
[16] Christophe Nussbaum,et al. Analysis of tectonic structures and excavation induced fractures in the Opalinus Clay, Mont Terri underground rock laboratory (Switzerland) , 2011 .
[17] P. K. Kaiser,et al. Influence of tectonic shears on tunnel-induced fracturing , 2010 .
[18] S. Siegesmund,et al. Influence of carbonate microfabrics on the failure strength of claystones , 2009 .
[19] H. Fossen,et al. Internal geometry of fault damage zones in interbedded siliciclastic sediments , 2008 .
[20] Paul Marschall,et al. Characterisation of Gas Transport Properties of the Opalinus Clay, a Potential Host Rock Formation for Radioactive Waste Disposal , 2005 .
[21] B. Clennell,et al. On the nature of scaly fabric and scaly clay , 2003 .
[22] Agust Gudmundsson. Fluid overpressure and flow in fault zones: field measurements and models , 2001 .
[23] T. Blenkinsop. Deformation Microstructures and Mechanisms in Minerals and Rocks , 2000 .
[24] C. Passchier,et al. Shear sense indicators in striped bedding-veins , 2000 .
[25] M. Doblas,et al. Slickenside and fault surface kinematic indicators on active normal faults of the Alpine Betic Cordilleras, Granada, southern Spain , 1997 .
[26] Y. Ogawa,et al. Scaly fabrics in sheared clays from the décollement zone of the Barbados accretionary prism , 1997 .
[27] P. Labaume,et al. Strain decoupling across the decollement of the Barbados accretionary prism , 1996 .