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déplacement des plaques lithosphériques sur la surface du globe--) modifie la paléontologie de la surface de notre planète ---) Alternance de cycles de phases fracturation/dislocation de supercontinents ---)créent de nouveaux océans -----)et de phases de disparition de lithosphère océanique-----------) rapprochement de masses continentales à l'origine de collisions et de chaines de montagnes-Phase de réunion de blocs continentaux --)formation d'un supercontinent unique ---) regroupement l'ensemble de masses continentales =cycle orogénique ou cycle de wilson --) croissance du volume de lithosphère continentale -) phase de suture ---)accumule de nouveaux matériaux magmatismes de subduction---Portion de lithosphère océanique intégrés aux chaines de montagnes
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