Stingers of mud in cross-laminated sandy seds. – Flaser bedding • Pods of sandy seds in laminated muddy sediments – Lenticular bedding • Herring bone cross-

Furthermore, Facies 7 (i.e., heterolithic bedding: flaser, wavy, lenticular) is good evidence of alternating deposition during intervals of relatively faster-moving flow (, 0.5 m/s) and extremely

Bidirectional paleocurrent records (a-d) and flaser, wavy to lenticular bedding (e, f) observed in the in the Jindong Formation at Deokhori site. a-c. The paleocurrent (arrows) in the current ripples are in opposed direction. d. Herring-bone cross-lamination (dotted box) e. Flas er bedding.

Flaser wavy lenticular bedding

(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. The mean layer thicknesses with different sedimentary structures range from 116 to 162mm, very close to the mean sedimentation rate estimated for this sampled interval, 135mm/year, indicating that the layers bounded by pure clay lamina with the minimum gray 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.

Looking for online definition of FLASER or what FLASER stands for? FLASER is listed in the World's largest and most authoritative dictionary database of abbreviations and acronyms The Free Dictionary

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.

Flaser, wavy, and lenticular bedding indicate alternation of bedload transport due to tidal currents and suspension fallout during slack-water periods (Reineck and Wunderlich, 1968; Klein, 1971). Upward replacement of tractive bedforms (i.e., current ripples) by mud deposited from suspension indicates decreasing tidal energy, which is consistent with progressive shallowing.

Current ripple bedding (flaser, wavy, lenticular) and ripple cross-lamination are widely developed. Characteristics include abundant low angle planar laminated foresets, flaser-wavy-lenticular bedding between foresets, trough cross-stratified mouth bars and subaqueous terminal distributary channels, and hyperpycnites on the distal delta front to prodelta. flaser, wavy, and lenticular bedding and rare to common clay-lined burrows including . Ophiomorpha nodosa.

The mean layer thicknesses with different sedimentary structures range from 116 to 162mm, very close to the mean sedimentation rate estimated for this sampled interval, 135mm/year, indicating that the layers bounded by pure clay lamina with the minimum gray 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.
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7 Dec 2017 bedding, flaser-wavy bedding, lenticular bedding, planar cross bedding and parallel laminated sandstone. Figure 1: Map of Miri showing the flaser, wavy and lenticular bedding, bimodal palaeocurrents and particular vertical arrangements of lithologies and structures, has provided evidence of intertidal (a) 70 cm thick set of planar-tabular cross-bedding (top), Little Dantzic Cove. (P.S.

layers in tidal deposits: flaser bedding, wavy bedding, lenticular bedding cross- bed sets, featuring planar- or wavy-bedding depending on the current strength. 7 Dec 2017 bedding, flaser-wavy bedding, lenticular bedding, planar cross bedding and parallel laminated sandstone.
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Flaser bedding commonly occurs in association with lenticular and wavy bedding. All three sedimentary structures and their interrelationships are hence discussed in this section.

Flaser, wavy and lenticular bedding is a gradational spectrum of heterolithic deposits with alternating beds/laminae of sand and mud. They may also be produced by episodic flooding on the alluvial plains, or weak storms in the offshore environments, but their primary occurrence is in tidal settings where the regular presence of slack tides favors mud deposition ( Reineck and Singh, 1980 , Dalrymple, 2010 ).