ductilemurtuminen
Ductilemurtuminen, also known as ductile deformation or ductile flow, is a geological process where rocks and other materials undergo permanent deformation without fracturing or breaking. This process occurs under conditions of high temperature and pressure, typically deep within the Earth's crust or in the mantle, where materials behave in a plastic manner rather than in a brittle fashion.
The term "ductile" refers to the ability of a material to undergo significant deformation before it breaks.
Ductilemurtuminen is driven by several factors, including temperature, pressure, strain rate, and the presence of fluids.
This process is significant in understanding the dynamics of the Earth's interior. It contributes to the movement