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c, Top view of the breccia-containing block from a note the contrasting appearance of the rock fabric.
It has long been known that rock fabric plays a key role in dictating rock strength and rheology throughout Earth's crust; however the processes and conditions under which rock fabric impacts brittle failure and frictional strength are still under investigation.
Seismic anisotropy is closely related to subsurface lithology, rock fabric and texture, and to its diagenetic history.
This study provides additional experimental data to understand the effects of rock fabric, complex pore network, clay swelling and osmotic potential on imbibition behavior.
This anisotropy is likely related to NW-SE rock fabric in the lower crust thought to originate from the Caledonian deformation.
This indicates differences in the horizontal components of tectonic strain, which finally give rise to differences in the evolution of the rock fabric.
Similar(42)
b e, Additional pieces of the rock sample, showing further examples of the contrasting rock fabrics.
The bowing potential of granitic rocks: rock fabrics, thermal properties and residual strain.
(eds.), Atlas of deformational and metamorphic rock fabrics: Berlin, Springer-Verlag, p. 176-179, 2198211, 1982 (W. Alvarez and T. Engelder).
(eds.), Atlas of deformational and metamorphic rock fabrics: Berlin, Springer-Verlag, p. 206-207, 1982 (T. Engelder and W. Alvarez).
A strong influence on weathering and pedogenesis by micro-scale features of primary minerals and parent rock fabrics is shown.
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