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.

SUMMARY Ripple, flaser and lenticular bedding are well known, but for describing profiles, they are not sufficiently defined and subdivided. It is, therefore, the intent of the following text to present such a definition and classification. The classification contains the following main bedding types and intermediary types (Fig.1): 1 Cross‐bedding with flasers. 2 Flaser bedding, subdivided

Great Investment. #1 in Premium Domains. 300,000 of the World's Best .Com Domains. Classification and Origin of Flaser and Lenticular Bedding Reineck, Hans-Erich; Geology - Sedimentary Structures Lenticular and flaser bedding. Footage of Sedimentary Structures known as Lenticular and flaser bedding in geology. (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.

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These features are thought to be created by deposition of suspended fine-grained mud onto a rippled sandy seafloor during quiescent periods, followed by migration of sand ripples during periods of strong sample 2.15 - flaser and lenticular bedding - Download Free 3D model by UQ School of Earth and Environmental Sciences (@UQ_SEES) [67fd211] Flaser bedding, vertical section. Flaser beds are a sedimentary, bi-directional, bedding pattern created when a sediment is exposed to intermittent flows, leading to alternating sand and mud layers.

SUMMARY Ripple, flaser and lenticular bedding are well known, but for describing profiles, they are not sufficiently defined and subdivided. It is, therefore, the intent of the following text to present such a definition and classification. The classification contains the following main bedding types and intermediary types (Fig.1): 1Cross-bedding with flasers.

The classification contains the following main bedding types and intermediary types (Fig.1): 1 Cross‐bedding with flasers. 2 Flaser bedding, subdivided sample 2.15 - flaser and lenticular bedding - Download Free 3D model by UQ School of Earth and Environmental Sciences (@UQ_SEES) [67fd211] Flaser bedding: Sand alternates with small drapes of mud.

Flaser and Lenticular Bedding • Other types o ripple bedding • Mixed hydraulic conditions and sed. Types • Stingers of mud in cross-laminated sandy seds.

Lenticular bedding: Lenses of sand in a muddy matrix. 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 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 ( Fig SUMMARY Ripple, flaser and lenticular bedding are well known, but for describing profiles, they are not sufficiently defined and subdivided. It is, therefore, the intent of the following text to present such a definition and classification. The classification contains the following main bedding types and intermediary types (Fig.1): SUMMARY Ripple, flaser and lenticular bedding are well known, but for describing profiles, they are not sufficiently defined and subdivided.

23 Oct 2019 Ripples bedding; is characterized by alternating sand and mud laminae or beds including; flaser, lenticular and wavy bedding (Fig. 4.18).
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The sand formations within the bedding display a 'lens-like' shape, giving the pattern its respected name. They are commonly found in high-energy environments such as the intertidal and supratidal zones. Flaser bedding, subdivided in: (a) simple flaser bedding; (b) bifurcated flaser bedding; (c) wavy flaser bedding; (d) bifurcated wavy flaser bedding. 3 .

1. These facies associations are interpreted as a Start studying GEOL 3200 Sedimentary Structure (7).
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Flaser bedding would generally be coded as 5X3.5 in the Ferm classification. The second digit would depend on the type of sandstone (4=gray, 5=crystalline, 6=hard). Lenticular bedding would be coded as 3X3 and wavy bedding would be coded as 3X2.5.

Both photographs were taken in trenches dug in North Sea tidal flats. 2015-10-24 · Lenticular bedding Top # 5 Facts. Lenticular bedding Top # 5 Facts. Skip navigation Sign in. Search.