2019-10-02 · The wavy orientation of the streaks indicate flaser-type ripple bedding. Interbedded sandstone and shale (layered) ( 322.5 ) in core. Note that shale interbeds between sandstone beds are thicker than in previous core.

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Flaser bedding

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The association of large-scale cross-bedding (50 to 300 cm) that is intercalated thin shale and sandstone, rare flaser bedding, and local bipolar distribution of Flaser and lenticular deposits (sensu Reineck and Wunderlich) are common in the sedimentary record and generally found associated with rippled seafloors in In fact, flaser bedding and lenticular bedding are more common in the point bar facies during the monsoon months than in the coastal tidal flat environments.

Lär dig definitionen av 'flaser structure'. Kolla in uttalet, synonymer och grammatik. Bläddra i användningsexemplen 'flaser structure' i det stora engelska korpus.

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 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. 4 Lenticular bedding with thick or Flaser bedding commonly occurs in association with lenticular and wavy bedding.

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Flaser Bedding. Wavy Bedding. Lenticular Bedding . Graded Bedding . Evenly Laminated Sand and Horizontal Bedding .

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bed but increased rapidly . 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 muddy matrix.

It is, therefore, the intent of the following text to present Tidal bundles, herringbone cross-bedding, flaser and lenticular bedding, inclined heterolithic stratification Flaser and lenticular deposits (sensu Reineck and Wunderlich) are common in the sedimentary record and generally found associated with rippled seafloors in tidally influenced coastal waters. 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 Lär dig definitionen av 'flaser structure'. Kolla in uttalet, synonymer och grammatik. Bläddra i användningsexemplen 'flaser structure' i det stora engelska korpus.
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Flaser bedding of non‐tidal origin has been described from point bar deposits of the Ajay river, NE India. 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.

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. Se hela listan på baike.baidu.com Define flaser.

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

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: Sand alternates with small drapes of mud.