subsidence
প্রশমন
definition
noun
The early Cretaceous is characterized by relative quiescence and thermal subsidence following late Jurassic rifting.
the gradual caving in or sinking of an area of land.
translation of 'subsidence'
অবনমন
noun
দমন,
অপগমন,
অপগম,
অধোগমন,
অধোগতি,
প্রশমন,
হ্রাস
example
In fact, tectonic 'subsidence' was calculated to be slightly higher in the Early Tertiary High than in the Voorne Trough.
Tertiary sediments cause 'subsidence' of the basin substrata 2.3 km below sea level, as a result of the sediment load.
Quaternary sedimentary fill testifies to recent 'subsidence' of the basin.
Excess accommodation could be created by rapid tectonic 'subsidence' in the centre of a tilt-block basin.
Also, at least on the Atlantic coast, you have both sea level rise and land 'subsidence' going on at the same time.
the race was abandoned because of 'subsidence' of the track
The early Cretaceous is characterized by relative quiescence and thermal 'subsidence' following late Jurassic rifting.
This is because magmatic material thickens the crust, creating uplift rather than 'subsidence' .
'subsidence' damage
We attribute this low rate to the continued post-rift thermal 'subsidence' of the Indian margin.
It could be argued that high 'subsidence' rates of the rift basin there meant that a regressive signal was not recorded.
In particular, we relate apparent Neogene 'subsidence' to modification of the Shelf's basement architecture.
As the basin filled, or the rate of 'subsidence' relative to the influx of material lessened, subaerial fluvial deposits were emplaced.
In this work, the logarithmic theory is used to calculate the amount of land 'subsidence' .
Removal of water from compressible materials such as silt and clay can lead to compaction of the confining unit and 'subsidence' of the land surface.
The forward model predicts approximately 4 km of tectonic 'subsidence' at this point.
The history during this time is characterized by uplift at the most proximal location and an increase in 'subsidence' at the most distal location.
Melt injection leads initially to isostatic uplift followed by 'subsidence' as the melt freezes.
Cover for accidental damage to contents and also for flooding or 'subsidence' are other areas that should be clarified before taking out a policy.
In addition, a drastic decrease in 'subsidence' rates before the onset of the Late Eocene Pyrenean inversion was determined.
Thermal 'subsidence' began to affect the onshore Central Plains area of Thailand.
This would result in the underestimation of the tectonic 'subsidence' that occurred during the deposition of the shales.
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