TY - JOUR
T1 - Fracturing in the solid Earth
AU - Nagahama, H.
PY - 1991
Y1 - 1991
N2 - In the Solid Earth, fracturing is a pervasive phenomenon: weathering, explosion, impact, faulting, earthquake and so forth. Several empirical studies on fractures have demonstrated a power-law dependence of the cumulative number N (r) of fragments of which sizes are larger than size r, N (r) ~ r-D. This is taken as evidence that the fracturing is a scale-invariant process concerning the size distribution. Therefore, fractures can be described from the viewpoint of a fractal. This description derives mathematically the Gaudin-Schuhmann relation and the Charles' relation and is sufficiently in incorporation of the three theories on size reduction: Rittinger's, Kick's and Bond's theories. -from Author
AB - In the Solid Earth, fracturing is a pervasive phenomenon: weathering, explosion, impact, faulting, earthquake and so forth. Several empirical studies on fractures have demonstrated a power-law dependence of the cumulative number N (r) of fragments of which sizes are larger than size r, N (r) ~ r-D. This is taken as evidence that the fracturing is a scale-invariant process concerning the size distribution. Therefore, fractures can be described from the viewpoint of a fractal. This description derives mathematically the Gaudin-Schuhmann relation and the Charles' relation and is sufficiently in incorporation of the three theories on size reduction: Rittinger's, Kick's and Bond's theories. -from Author
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M3 - Article
AN - SCOPUS:0026282429
VL - 61
SP - 103
EP - 126
JO - Science Reports - Tohoku University, Second Series: Geology
JF - Science Reports - Tohoku University, Second Series: Geology
IS - 2
ER -