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Operated by multiple sedimentary processes and dynamics, the clastic particles are mixed by corresponding multiple populations of grain sizes within different settings, which is finally recorded in the grain-size distribution (GSD) of the sediments. Many statistical models, such as log-normal, Rosin, log-hyperbolic, Weibull, log-skew-Laplace, gamma, and tangential hyperbolic, have been used to unmix...
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