Off Topic — HabitableZone

Off Topic » in reply to You should describe what you mean by plastic.

I'm afraid you're right...Plastic deformation, then.

Or permanent strain (deformation) without rupture.

At mantle temps and pressures, silicate crystalline rocks deform at a molecular level by changes in the crystal lattice structure.

In the upper mantle, ultra-mylonitic shear zones have been recognized using geopyhsics.

I'll try to be more precise in the future! :-)

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