Sentence examples for deposit facies from inspiring English sources

The deposit facies architecture was interpreted to understand particle transport and deposition within the framework of granular flow systematics.

The flow topography interaction can play a fundamental role in the sedimentary processes, and in the resulting deposit facies architecture, as well as can play a dramatic role in the flow behavior, and in the associated volcanic hazard.

Based on the deposit facies observed in this study, we can divide the deposit into three major units (Units A, B, and C).

Comparisons of depositional facies from experimental deposits with natural deposits justify the use of this experimental dataset for deposit volume evaluation (Graettinger et al. 2015a,b; Valentine et al. 2015b).

The horizontally laminated deposits of Facies 1a have been interpreted as autochthonous suspension deposits associated with a low energy environment as water laden with mud gradually filtered into the cave chamber.

Deposits of Facies 1a have also accumulated on ledges in isolated fissures where mud filtered through narrow cracks.

Deposits of Facies 2 accumulated in the area beneath the fissure that forms the entry point into the Dinaledi Chamber, to form a debris cone that sloped into the chamber.

Deposits of Facies 1b are interpreted to represent a higher energy environment involving pulses of para-autochthonous and/or allochtonous sediment deposited in the cave by minor sheet flow, which alternated with periods of quiescence during which Facies 1a muds were deposited.

At some point in time, deposits of Unit 1 would have filled much of the Dinaledi Chamber, and erosion products (i.e., mud clasts) from this unit are the source for much of the mud clast breccia (i.e., deposits of Facies 2; Figure 4E) observed in the cave chamber.

Deposits in the trench wall were divided into five facies (event deposits, marsh deposits, channel fill deposits, artificial fill deposits, and cultivation soil), based on their sediment structure, continuity, and composition (Fig. 6).

The sedimentary layers in the valley can be generalized as coarser sand and gravel layers at the bottom superimposed with layers of sand and clay deposit of lacustrine facies; fluvial deposits from the Bagmati river system make up the topmost layer (Yoshida and Igarashi 1984; Dangol 1985; Shrestha et al. 1998; Sakai 2001).