crustal's Usage Examples:

The largest of these fault blocks are called crustal blocks.

Large crustal blocks broken off from tectonic plates are called terranes.

accumulated polar ice mass destabilizes the Earth's rotation, causing crustal displacement but not disturbing the Earth's axial orientation.

plates consist of lithospheric mantle overlain by one or two types of crustal material: oceanic crust (in older texts called sima from silicon and magnesium).

elevation of a region can only occur in response to tectonic processes of crustal thickening (such as mountain building events), changes in the density distribution.

Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets.

Variation in crustal thickness, magmatic and volcanic activities, impact-induced Moho-uplift.

\beta ={\frac {t_{1}}{t_{0}}}\,,} t0 is the initial crustal thickness and t1 is the final crustal thickness.

elements in Earth's crust is shown in tabulated form with the estimated crustal abundance for each chemical element shown as mg/kg, or parts per million.

Continental crustal fragments, partially synonymous with microcontinents, are pieces of continents that have broken off from main continental masses to.

variety of associated phenomena, including crustal deformation, crustal thickening, crustal thinning and crustal melting as well as magmatism, metamorphism.

and Sims, 1963); a major gravity low (Isaacson and Smithson, 1976); low-crustal velocities; and high heat flow (Decker et al.

Mantle and crustal melts migrate upwards through the crust where they are thought to be stored in magma chambers or trans-crustal crystal-rich mush.

Three major hypotheses have been proposed for the origin of the crustal dichotomy: endogenic (by mantle processes), single impact, or multiple.

Ovda Regio is a Venusian crustal plateau located near the equator in the western highland region of Aphrodite Terra that stretches from 10°N to 15°S and.

Earth's crust on a large scale, relative to crustal-scale features or the geoid.

The movement of crustal plates and accommodation spaces created by faulting.

Earth tide (also known as solid Earth tide, crustal tide, body tide, bodily tide or land tide) is the displacement of the solid earth's surface caused.

the crustal material, which will be different from the ratio in the mantle material.

Samarium–neodymium dating allows us to determine when the crustal material.

The crustal block or fragment preserves its own distinctive geologic history, which.

Thick-skinned deformation is a geological term which refers to crustal shortening that involves basement rocks and deep-seated faults as opposed to only.