Metadata
Author: WikiMatrix
Data
English[en]
The Alpine orogeny caused extensive folding and faulting of Mesozoic and early Tertiary sediments from the Tethys geosyncline.
Spanish[es]
La orogenia alpina causó extensos pliegues y fallas de sedimentos de la era mesozoica y principios de la era terciaria provenientes del movimiento geosinclinal.