लिथोस्फेरिक इसके अंग्रेजी अर्थ का उदाहरण

Upon a return to normal subduction, the hot asthenosphere will once again interact with the hydrated mantle, causing wet melting, crustal melting will ensue as mantle melts pass through, and lithospheric thinning and weakening due to the increased heat flow.

Decompression melting can occur in thickened portions of the Earth's crust and may be the result of a variety of processes, including erosion, tectonic denudation, and lithospheric thinning.

These formations are, relative to other lithospheric formations, cooler and less dense but much more isopycnic.

What controls the lithospheric architecture?.

How does lithospheric rheology change in the vicinity of a fault zone?.

How are the crust and lithospheric mantle related?.

The relationship between lithospheric and the upper mantle processes is something that is not completely known, including upper mantle processes below the United States and their effects on the continental lithosphere.

It was created by the collision between the African and European lithospheric plates.