Shrinkage cracks show that the flaser-bedded section has been deposited in an aerially expo- sed environment. Reineck & Wunderlich (1968), Reineck (1972, 1975), Klein (1971), Vis- her (1975) and Evans (1975) describe fining upward sequences consisting of flaser, wavy and/or lenticular bedding from progradation of tidal flats.

Rhythmites of v.f.g sand and carbonate mud contain abundant stacked, wavy, lenticular and flaser bedding in a well-sorted and segregated silt and clay that.

Wavy bedding. TIDAL. CHANNEL. Low tide. level. 'I'1111?

Graded Bedding . Evenly Laminated Sand and Horizontal Bedding . Coarsely Interlayered Bedding . Flaser definition: a type of pattern or structure in sedimentary rock, caused by intermittent flows within | Meaning, pronunciation, translations and examples The beds are 5–50 cm thick, show mild bioturbation, and form lenticular, wavy, and flaser heterolithic bedding. The siltstone layers contain small (<1 mm) anhydrite nodules. Cross-strata have sharp basal and wavy upper contacts.

bedding, herringbone cross-bedding, lenticular bedding, and mud/silt couplets are common to both the environments. In fact, flaser bedding and lenticular bedding are more common in the point bar facies In a wavy laminated unit, a fin

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. 2 Flaser bedding, subdivided in: (a) simple flaser bedding; (b) bifurcated flaser bedding; (c) wavy flaser bedding; (d) 3 Wavy bedding.

cies, including flaser, wavy, and lenticular bedding, small-scale herringbone cross-strata, reactivation surfaces, small channel scours, ripple marks, horizontal laminae with cur-rent lineations, small load structures, and shrinkage cracks. Broken and abraded mol-lusk shells, crinoid fragments, and fish bones are present in the sandstone. The

02 be. Flaser bidding. 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.

Clifton, 1982, Elliott, 1986, Boggs, 1995), yet these structures are rarely discussed in synthesis papers on fluvial deposition (e.g. Collinson, 1986, Miall, 1992, Boggs, 1995), despite the recognition that they also form in fluvial environments Ripple, flaser and lenticular bedding are well known, but for describing profiles, they are not sufficiently defined and subdivided.
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Wavy Bedding . Lenticular Bedding .

The most distinctive sequences Location of Formation • flaser bedding - commonly forms in relatively high energy environments (sand flats) • wavy bedding - commonly forms in environments that alternate frequently from higher to lower energies (mixed flats) • lenticular bedding - commonly forms in relatively low energy environments (mud flats) Cross Stratification Variant 3: Structure caused by tidal (Flaser-Wavy 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.
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30 Nov 2019 with heterolithic stratification – flaser, wavy to lenticular bedding. Bhattacharya, A. (1997): On the origin of non-tidal flaser bedding in point

Fi g. 4. Bidirectional paleocurrent records (a-d) and flaser, wavy to lenticular bedding (e, f) observed in the in the Jindong Formation at Deokhori site.

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The term “lenticular bedding” is defined as “a form of interbedded mud and ripple cross-laminated sand, in which the ripples or lenses are discontinuous not only in the vertical but also more or less in the horizontal direction” (p. 376), and the term “wavy bedding” as “a form of interbedded mud and ripple-cross-laminated sand, in

The classification contains the following main bedding types and intermediary types (Fig.1): 1 Cross‐bedding with flasers. 2 Flaser bedding, subdivided 2016-08-29 · Flute casts - how to use them as a way-up (younging) direction indicator in sedimentary rocks - Duration: 1:27. GeoHub Liverpool 469 views Lenticular bedding is classified by its large quantities of mud relative to sand, whereas a flaser bed consists mostly of sand. The sand formations within the bedding display a 'lens-like' shape, giving the pattern its respected name.

The three main types of heterolithic bedding are flaser, wavy, and lenticular. Retrieved from Wikipedia CC BY-SA 3.0

Ripple Cross-lamination, HCS, IHS And Lenticular Bedding HCS, Bioturbated Texture, Combined Ripple Cross-lamination C Flaser, Wavy And Lenticular Flaser-wavy bedded, Dr/Dl, Lenticular calcilutite interbeds calcarenite; flaser and (b) Flaser bedding (Dr/Dl lithofacies) in the carbonate tidalites (Deranjal bedding, deformation, deposition, erosion, interbed, intrabed, sediment. 2. Structure of the Figure.2.16. Sketches of flaser, lenticular and wavy bedding. 2.2.6. Abstract Flaser and wavy bedding are sedimentary structures characterized by alternating rippled sand and mud layers.

2. Structure of the Figure.2.16. Sketches of flaser, lenticular and wavy bedding. 2.2.6.