Flaser-bedding indicates deposition alterna- ting between bed-load and suspension, and is recognized from many different depositional environments. The flaser-bedded section (Fig. 3) shows bifurcating flasers which Alam et al. conclude are most likely formed in tidal envi- ronments. Both wave and current structures

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The occasional May 24, 2012 periodic alternations of the ebb-flood cycle, including lenticular bedding, wavy bedding and flaser bedding (Reineck and Wunderlich, 1968). Flaser bedding within some of the fine-grained sandstones suggests a possible tidal component as well. The depositional environment for the Gorge Dolomitic nisms can form plane bedding: sedimentation from Finer-scale plane bedding ( less than 1 cm thick) is usually called called flaser bedding (Fig. 4.9A, C). Flaser Bedding. Induced Fracture.

Flaser bedding

The flaser-bedded section (Fig. 3) shows bifurcating flasers which Alam et al. conclude are most likely formed in tidal envi- ronments. Both wave and current structures Starved ripple from the Devonian of Ohio, USA. (cross-section view) Three categories of bedforms occur in sand-deficient environments: 1) flaser bedding; 2) wavy bedding; 3) lenticular bedding. The three bedding styles are produced by interbedded muds (in the form of drapes) and sands (in the form of ripples). In nature, a continuum exists among these three bedforms.

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Dune cross bedding: Foresets tend to be more or less regularly spaced or bundled. expressed by alternations in mud drape intensity in the flaser bedding .

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The three bedding styles are produced by interbedded muds (in the form of drapes) and sands (in the form of ripples). In nature, a continuum exists among these three bedforms. At the ends of the Flaser Bedding . Wavy Bedding . Lenticular Bedding . Graded Bedding .
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Reactivation –3.4e+04. 3.6e+05.

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flaser bedding planar bedding structures flow structures soft sediment deformation or turbidity current structures* flute casts bedding plane irregularities fossil ice

Mud drapes are deposited during waning flood phases. The preferential accumulation of curled, desiccated mud laminae in ripple troughs during periods of exposure produces mud streaks resembling classical flaser bedding.

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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

Cross Bedding Erosional Surface Flaser Bedding Bit Size 6 in 16 Caliper 1 6 in 16 Facies Gamma Ray 6 in 16 Gamma Ray Neutron Limestone Porosity Bulk Density 1.95 g/cm3 2.95 Array Laterolog Resistivity 5 0.2 ohm.m 2,000 Array Laterolog 0.2 ohm.m 2,000 Array Laterolog flaser bedding. Verso la sommità gli strati calcarei sono più spessi (centimetrici) e più compatti; la colorazione passa dal rosa-marrone al bianco-rosato (Fig. 2a). Se sottoposta a sollecitazione tettonica, come visi-bile in prossimità dei piani di sovrascorrimento, la Scaglia Rossa sviluppa una fratturazione pervasiva, cross bedding is used. In fact the generic term that is used most commonly is cross bedding (as opposed to cross stratification).

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