Noun:

लेसर,

flaser's Usage Examples:

Simple flaser bedding is when the flasers do not contact one another.

intrusive masses which may be nearly massive or may have gneissose, flaser or granulitic structures.

molar tooth structures, as well as teepee structures, desiccation cracks, flaser bedding, and other sedimentary structures that indicate deposition in an.

The conglomerate includes planar beds, trough cross-bedding, flaser bedding, mud-drapes on some ripples, U-shaped burrows and escape structures.

is classified by its large quantities of mud relative to sand, whereas a flaser bed consists mostly of sand.

In the lower part of the formation flaser cross bedding in fine grained sandstone is found in abundance, however a.

bedding are simple flaser, bifurcated flaser, wavy flaser, and bifurcated wavy flaser.

that are created by these processes are herringbone cross-stratification, flaser bedding, and interference ripples.

Horizontally laminated and thin bedded fine-grained sandstones as well as flaser- and ripple cross-lamination characterize a low-energy environment within.

It is lenticular, wavy and flaser lamination.

Outcrops of the overlying Båtsfjord Formation are generally not as prominent, but are notable for containing molar tooth structures, as well as teepee structures, desiccation cracks, flaser bedding, and other sedimentary structures that indicate deposition in an inter-tidal, intermittently exposed environment.

These layers contain siltstone beds which locally exhibit flaser bedding, oscillation ripples and hummocky cross-bedding.

upward in cross-bedded sandstone and minor siltstone and claystone with flaser or lenticular bedding that are interpreted as tidal flat and tidal channel.