Observations of pore systems of natural siliciclastic mudstones
(2016)
Book Chapter
Aplin, A., & Moore, J. (2016). Observations of pore systems of natural siliciclastic mudstones. In T. Schäfer, R. Dohrmann, & H. Greenwell (Eds.), Filling the gaps - from microscopic pore structures to transport properties in shales (33-44). Clay Minerals Society. https://doi.org/10.1346/cms-wls-21.3
Grains within siliciclastic muds are deposited either as flocs, in which grains are generally ,10 mm, or as single grains: “sortable silt,” generally .10 mm. When clay-size (,2 mm diameter) particles form .30% of mudstones, pore-size distributions ar... Read More about Observations of pore systems of natural siliciclastic mudstones.