Noun:

অশ্মমঙ্গল,

lithospheric's Usage Examples:

occurs by conductive cooling, which converts hot asthenosphere into lithospheric mantle and causes the oceanic lithosphere to become increasingly thick.

through tectonic compression of oceanic and continental crust during lithospheric flexure.

known as a destructive boundary) is an area on Earth where two or more lithospheric plates collide.

mountain belt causes the lithosphere to bend, by a process known as lithospheric flexure.

configuration of mechanically weaker and stronger lithospheric regions in the EARS.

As extension continues, lithospheric rupture will occur within 10 million years;.

The subcontinental lithospheric mantle (SCLM) is the uppermost solid part of Earth's mantle associated with the continental lithosphere.

The lithospheric mantle is the uppermost solid part of Earth's mantle.

The lithospheric mantle is subdivided into the subcontinental lithospheric mantle.

can occur at any scale, from microscopic to lithospheric, and can be found in all terranes.

In lithospheric-scale tectonics, boudinage of strong layers.

A critical element of the plate tectonic system is these lithospheric plates become negatively buoyant at some point in their evolution, sinking.

Tectonic lithosphere plates consist of lithospheric mantle overlain by one or two types of crustal material: oceanic crust.

an area where the crust of the over-riding plate is lacking a rigid lithospheric mantle component and thus is exposed to hot asthenospheric mantle (for.

function of the lithospheric stress field.

The global distribution of volcanic activity at a given time reflects the contemporaneous lithospheric stress field.

Analysis of mantle xenoliths reveals that the lithospheric mantle of the Deseado Massif is about 2100 to 1000 million years old.

cratons, stable blocks of old crust with deep roots in the subcontinental lithospheric mantle, and less stable terranes, which came together to form the African.

They have a thick crust and deep lithospheric roots that extend as much as several hundred kilometres into Earth's.

The lithospheric flexure (also called regional isostasy) is the process by which the lithosphere (rigid outer layer of the Earth) bends under the action.

of sub-lithospheric small-scale convection and instabilities arising from heterogeneities in the asthenosphere and variations in lithospheric thickness.