The vertical collapsing flow has relatively high particle concentration and high sedimentation rate, resulting in the formation of a massive poorly sorted deposit, which can be transformed into a lateral dilute traction suspension current, as observed in large-scale laboratory experiments using cold pyroclastic materials (e.g., Sulpizio et al. 2014).
Their olive drab boxes and cabinets with yellowing cards stand in contrast to the higher stacks of the clean, pale "new" boxes that contain the massive amount of sorted material.
The first hollow is in a 16-cm thick tsunami deposit layer composed of well-sorted, massive fine sand.
Sand mainly occurs as two different types, with a form of fine- to coarse-grained, massive, or well-sorted, as trough cross-stratified, ripple-laminated sand layers varying in thickness from approximately 5 to 15 m (e.g. 133 118 m) and enclosed by the clay or silt with lenticular structure (e.g., 72 63 m).
The base of the section features a poorly-sorted, primary massive volcaniclastic kimberlite deposit (MVK1) grading upward into a better-sorted and weakly-stratified volcaniclastic kimberlite deposit (MVK2); which is, itself, overlain by ~ 45 m of stratified volcaniclastic kimberlite (SVK).
2) Massive amounts of data are sorted and merged by the data packing technique to reduce the problem scale by aggregators.
Core analysis indicates that the bottom of the sequence is well-sorted medium-fine massive sandstone, with good consistency in seismic response within the whole oil field (Fig. 10).
The sedimentary features mostly include massive bedding and its lithology is well-sorted thick fine sandstone.
The Lower Member is represented by 59 m of white, medium and coarse-grained, poorly to moderately sorted sandstones; with thin and scattered intercalations of purple, massive, sandy mudstones.
Type A paleosols are hosted by well-sorted fine to medium grained trough cross bedded and massive sandstones and preserve abundant vertical to horizontal micritic and microspar calcite tubules, interpreted as rhizoliths.
They were composed mostly of poorly sorted sand and often consisted of one to four normally graded, massive or laminated layers.
