Flaser bedding: Sand alternates with small drapes of mud. · Wavy bedding: Roughly equal volumes of sand and mud. · Lenticular bedding: Lenses of sand in a

7 Dec 2017 bedding, flaser-wavy bedding, lenticular bedding, planar cross bedding and parallel laminated sandstone. Figure 1: Map of Miri showing the

Wavy bedding: Roughly equal volumes of sand and mud. Lenticular bedding : Lenses of sand in a muddy matrix. Although these can occur in many subaqueous environments, they are particularly characteristic of tidally dominated ones, where there is daily variation in flow regime. 2021-04-11 · flaser bedding A form of heterolithic bedding characterized by cross-laminations draped with silt or clay. Flaser beds form in environments where flow strengths fluctuate considerably, thus permitting the transport of sand in ripples, followed by low-energy periods when mud can drape the ripples.

Flaser wavy lenticular bedding

Wavy bedding occurs when mud is deposited over the whole area of a bed of rippled and/or cross stratified sand. It usually loosely follows the alternating concave-convex nature of the ripples creating a wavy appearance. In wavy bedding the ripples are laterally discontinuous. Wavy bedding marks the boundary between flaser and lenticular bedding.

Sedimentary structures such as cross-stratigication ripple marks, lenticular and wavy bedding, flaser bedding, flute casts, load casts, sandstone concretion and

I Õ 1 3. Flaser, Wavy and Lenticular Bedding The process of alteration of bed load and suspension sedimentation gives rise to variety of flaser, wavy and lenticular bedding.

Tb2 is characterized by flaser, wavy, and lenticular bedding and rare to common clay-lined burrows including Ophiomorpha nodosa. Thickness is 0 to 70 feet. Mafic and Felsic Volcanic Rocks (Proterozoic) at surface, covers 19 % of this area

The bedding thickness ranges from 6 to 10 cm thick. The heterolithic facies (He) can be divided into three sub-facies, namely flaser (Hf), wavy (Hw) and lenticular bedding (Hl). Most of the structural patterns are based on percentage of sand and mud. (1968): Classification and origin of flaser and lenticular bedding. Revisiting the late Jurassic-Early Cretaceous of the NW South Iberian Basin: new ages and sedimentary environments This rock contains wavy, flaser , and lenticular beds along with trace fossils, desiccation cracks, runzel marks, and current-formed ripples. Five sedimentary structures were recognized: flaser bedding, wavy bedding, lenticular bedding, horizontal bedding, and massive layers.

Lenticular Sandstone | Description Flaser Bedding These tiny wavy beds of mudstone with lenticular pods of sandstone are typical of delta sediments. The pound coin is for scale. The classification contains the following main bedding types and intermediary types (Fig.1): 1 Cross‐bedding with flasers. 2 Flaser bedding, subdivided in: (a) simple flaser bedding; (b) bifurcated flaser bedding; (c) wavy flaser bedding; (d) bifurcated wavy flaser bedding. 3 Wavy bedding. 4 Lenticular bedding with thick or flat lenses, subdivided in: (a) continuous lenticular bedding (with connected lenses); (b) broken lenticular bedding (with single lenses).
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Great Investment. #1 in Premium Domains. 300,000 of the World's Best .Com Domains. The classification contains the following main bedding types and intermediary types (Fig.1): 1 Cross‐bedding with flasers.

What depositional environment is represented by these av B Gedda · 1993 — prises 1.7 m flaser bedded heterolites, 0.4 m lenticularly bedded heterolites and 3.5 m of wavy bedded heterolites (Fig. 6).
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The classification contains the following main bedding types and intermediary types (Fig.1): 1 Cross‐bedding with flasers. 2 Flaser bedding, subdivided in: (a) simple flaser bedding; (b) bifurcated flaser bedding; (c) wavy flaser bedding; (d) bifurcated wavy flaser bedding. 3 Wavy bedding. 4 Lenticular bedding with thick or flat lenses, subdivided in: (a) continuous lenticular bedding (with connected lenses); (b) broken lenticular bedding (with single lenses).

Most of the structural patterns are based on percentage of sand and mud.

(a) 70 cm thick set of planar-tabular cross-bedding (top), Little Dantzic Cove. (P.S. 1); (b) ripples, flaser, wavy, and lenticular bedding, interfer- ence ripple

They are commonly found in high-energy environments such as the intertidal and supratidal zones. Flaser bedding is a sedimentary structure characterized by alternating rippled sand and discontinuous mud layers created by the deposition of mud on previously existing sand ripples. Similarly, wavy bedding consists of alternating rippled sand and mud layers, but with thicker, more horizontally continuous mud layers than in flaser bedding . Lenticular bedding: Lenses of sand in a muddy matrix.

Flaser bedding commonly occurs in association with lenticular and wavy bedding. All three sedimentary structures and their interrelationships are hence discussed in this section.