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Opalinus Shale

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Journal Article
Published: 01 April 2017
Clays and Clay Minerals (2017) 65 (2): 135–153.
.... The effects of diagenesis on the microfabric, pore size distribution, and porosity of Opalinus shale were measured by comparing the behavior of natural and reconstituted specimens. The parent material (Opalinus shale) was reconstituted through multiple grinding operations, sedimentation from a dispersed...
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Journal Article
Journal: Clay Minerals
Published: 01 June 2000
Clay Minerals (2000) 35 (3): 515–524.
...H. TAUBALD; A. BAUER; T. SCHÄFER; H. GECKEIS; M. SATIR; J. I. KIM Abstract The alteration and transformation behaviour of the Tertiary Hammerschmiede Smectite and the Jurassic Opalinus Shale in an alkaline solution was studied in column experiments. The Hammerschmiede Smectite is proposed...
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Journal Article
Published: 01 June 1993
Clays and Clay Minerals (1993) 41 (3): 365–372.
Journal Article
Published: 01 December 1992
Clays and Clay Minerals (1992) 40 (6): 650–658.
Journal Article
Published: 01 June 2008
Clays and Clay Minerals (2008) 56 (3): 285–306.
... a relatively weak alignment of clay minerals and a random distribution for calcite. Opalinus shales from Benken and Mont Terri show strong alignment of illite-smectite, kaolinite, chlorite, and calcite. This intrinsic contribution to anisotropy is consistent with macroscopic physical properties where...
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The PMMA, Berea sandstone, Bentheim sandstone, and <span class="search-highlight">Opalinus</span> <span class="search-highlight">shale</span> samples. ...
Published: 28 December 2017
Figure 1. The PMMA, Berea sandstone, Bentheim sandstone, and Opalinus shale samples. Standard samples, 60 mm long, were used for experimental measurements first; then, thin-disc samples 15 mm long were cut out of the standard plugs. The Opalinus shale sample shown in the figure is before cutting.
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Grain-size distribution (a) of the Mont Terri <span class="search-highlight">Opalinus</span> <span class="search-highlight">shale</span>, (b) mineral p...
Published: 01 April 2017
Figure 1. Grain-size distribution (a) of the Mont Terri Opalinus shale, (b) mineral phase map of the ground shale showing disintegration and breakage of particles and clay aggregates.
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SEM photomicrographs of the broken surface of a natural <span class="search-highlight">Opalinus</span> <span class="search-highlight">shale</span> spec...
Published: 01 April 2017
Figure 4. SEM photomicrographs of the broken surface of a natural Opalinus shale specimen with (a, b) pyrite framboids and (c, d) Foraminifera microfossils within the highly oriented clay structure that is parallel to the fissility plane.
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BSE photomicrograph of a broad surface of a natural <span class="search-highlight">Opalinus</span> <span class="search-highlight">shale</span> sample: ...
Published: 01 April 2017
Figure 6. BSE photomicrograph of a broad surface of a natural Opalinus shale sample: (a) the particle orientations and structures can be detected and the horizontal fissility planes and inter-particle cracks are visible, (b) EDS map of the same section provides information on the distribution
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Photographs of (a, b) natural <span class="search-highlight">Opalinus</span> <span class="search-highlight">shale</span> that show the fissility direct...
Published: 01 April 2017
Figure 8. Photographs of (a, b) natural Opalinus shale that show the fissility direction, natural fracture, and non-clay mineral inclusions and (c) photographs of a reconstituted Opalinus shale (Recon.9) consolidated to effective stress of σ’ v = 32 MPa. The natural variability is evident
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BSE photomicrographs of natural and reconstituted <span class="search-highlight">Opalinus</span> <span class="search-highlight">shale</span>: (a, b) re...
Published: 01 April 2017
Figure 10. BSE photomicrographs of natural and reconstituted Opalinus shale: (a, b) reconstituted shale at 2MPa; (c, d) reconstituted shale at 16 MPa; (e, f) reconstituted shale at 50 MPa under one-dimensional K 0 -condition; and (g, h) natural shale.
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Cumulative void ratios ( e  GH ) of the reconstituted <span class="search-highlight">Opalinus</span> <span class="search-highlight">shale</span> at dif...
Published: 01 April 2017
Figure 11. Cumulative void ratios ( e GH ) of the reconstituted Opalinus shale at different consolidation stress levels and the natural shale.
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Natural and reconstituted <span class="search-highlight">Opalinus</span> <span class="search-highlight">shale</span> specimen N 2  adsorption-desorptio...
Published: 01 April 2017
Figure 14. Natural and reconstituted Opalinus shale specimen N 2 adsorption-desorption isotherms at liquid N 2 (–197.3°C) temperature.
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Pore (entrance) size distribution (PSD) functions of reconstituted <span class="search-highlight">Opalinus</span>...
Published: 01 April 2017
Figure 13. Pore (entrance) size distribution (PSD) functions of reconstituted Opalinus shale samples at different consolidation stress levels and the PSD of the natural shale. A clear transition from a double-structure to a single structure fabric occurred as a result of the increased
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Graph of consolidation stress  vs . void ratio and porosity of the reconsti...
Published: 01 April 2017
Figure 9. Graph of consolidation stress vs . void ratio and porosity of the reconstituted Opalinus shale in the present study along with sedimentation compression curves that were compiled for normally consolidated argillaceous sediments (modified from Skempton, 1969 ).
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SEM photomicrographs (a, b, c, d) of an Ar ion-milled surface of a natural ...
Published: 01 April 2017
Figure 5. SEM photomicrographs (a, b, c, d) of an Ar ion-milled surface of a natural Opalinus shale specimen. The micron-scale pores resulted from the enhanced porosities along the boundaries of microfossils and non-clay particles or due to the presence of microcracks.
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Measured       V    P       and       V    S       on the set of standard a...
Published: 28 December 2017
Figure 4. Measured V P and V S on the set of standard and thin samples made of four different materials. Experimental errors are shown for measurements on thin samples. Shear velocity V S on the Opalinus shale is the velocity of the S-wave propagating
Journal Article
Journal: Clay Minerals
Published: 01 April 2000
Clay Minerals (2000) 35 (2): 459.
... on the Opalinus Shale and the Hammerschmiede Smectite J.-F. Alcover, Y. Qi, M. Al-Mukhtar, S. Bonnamy and F. Bergaya. Hydromechanical effects: (I) on the Na-smectite microtexture M. Al-Mukhtar, Y. Qi, J.-F. Alcover, J. Conard and F. Bergaya. Hydromechanical effects: (II) on the water-Na-smectite system...
Journal Article
Journal: Geophysics
Published: 28 December 2017
Geophysics (2018) 83 (2): MR47–MR56.
...Figure 1. The PMMA, Berea sandstone, Bentheim sandstone, and Opalinus shale samples. Standard samples, 60 mm long, were used for experimental measurements first; then, thin-disc samples 15 mm long were cut out of the standard plugs. The Opalinus shale sample shown in the figure is before cutting. ...
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Journal Article
Published: 01 April 2020
Clays and Clay Minerals (2020) 68 (2): 144–160.
... fragments) were observed, and, in some cases, pyrite grains were contained within calcite ( Fig. 8c ). Analcime–wairakite crystals were not identified. The clay mineralogies of the reacted Wyoming bentonite and Opalinus Clay fractions were also characterized. Discrete Opalinus Clay shale fragments (~1–5...
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