Autoclastic

Au`to`clas´tic

(Geol.) Broken in place; - said of rocks having a broken or brecciated structure due to crushing, in contrast to those of brecciated materials brought from a distance.

autoclastic

[¦ȯd·ō¦klas·tik] (geology) Of rock, fragmented in place by folding due to orogenic forces when the rock is not so heavily loaded as to render it plastic.

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