The continental orogenesis is characterized with the following features, such as sudden start, global synchronicity and horizontal movement, occurring mainly in the upper part of the crust and weakening with depth, and so on.
The continental orogenesis is characterized with the following features, such as sudden start, global synchronicity and horizontal movement, occurring mainly in the upper part of the crust and weakening with depth, and so on.
摘要大陆皱造山运动具有突发性、全球同步性，以水平运动为主，主要表现在地壳上部且具有上强下弱等特征，除水平运动一项外，与基于地幔对流的板块构造理论缺少共同之处。