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For 90% of the VHCF failures under axial loading, fractured grain boundaries or inclusions in the interior of the material act as crack starters.
Given that we treat a success as being a fractured grain, then for the microboudinage data set N is the total number of measured grains, y is the number of microboudinaged grains, and p is the ratio of the number of microboudinaged grains to the total number of grains (microboudinaged + intact).
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The fractures are generally characterized by small shear offsets and show no indicators of cataclastic deformation (fractured grains or reduced grain size) or grain dissolution (Fig. 12f, h).
The micro fractures are mainly interlayer fractures, grain boundary fractures and organic matter contraction fractures.
The electrical resistivity method is most frequently used in environmental studies because the electrical resistivity of earth materials is determined by parameters such as fluids, conductivity of the matrix, porosity, permeability, temperature, degree of fracturing, grain size, degree of cementation, rock type and the extent of weathering of the medium (Olorunfemi 2001; Idornigie et al. 2006).
The 90° impingement angle erosion testing resulted in fracturing of WC grains followed by eruption of binder matrix by interlinking of cracks originated from fractured WC grains.
In addition, tektites (fractured sand grains characteristic of meteorite impacts) and the rare-earth element iridium, which is common only deep within Earth's mantle and in extraterrestrial rocks, have been found in deposits associated with the extinction.
A Ga wire growth mechanism based on a catalysis model, which involves fractured Cr2GaC grains as the catalyst, is proposed.
The recent studies by Okudaira et al. (2015, 2017) reported fractured plagioclase grains that were likely formed at lower-crustal conditions based on microstructural observations and analyses for naturally deformed gabbroic and anorthositic rocks.
It took up to 30% less pressure to fracture rice grains that had activated one or both of the puroindoline genes, the researchers report in the February issue of Nature Biotechnology.
Diagenetic events identified in these sandstones include considerable compaction during burial diagenesis at higher temperatures and low flow rates, cementation by clay minerals and iron oxides, dissolution and alteration of unstable clastic grains, and tectonically induced grain fracturing.
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