thermodilúciós
Thermoclastic is a term used in geology to describe rock deformation that occurs at relatively low temperatures and pressures. This type of deformation is characterized by brittle fracturing and faulting, where the rock breaks rather than flows. The mechanisms involved are typically the creation and propagation of cracks.
In contrast to ductile deformation, which happens under high temperatures and pressures where rocks can flow
Examples of thermoclastic deformation include the formation of faults in the Earth's crust, such as those found