Rheid

Source: Wikipedia, the free encyclopedia.

In

S. Warren Carey in 1953, has the same Greek root as rheology, the science of viscoelasticity
and nonlinear flow.

Types of rheids

Almost any type of

shear waves, it may be deduced that it is a solid and, therefore, behaving as a rheid when it undergoes said convection. Granite has a measured viscosity at standard temperature and pressure of about 4.5×1019 Pa·s [1]
so it should be considered a rheid. Similarly
stress. Through this mechanism, salt domes and other structures may form. In some areas, such as the Gulf of Mexico, these structures often serve as traps for petroleum and natural gas
.

References


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