摘要
东亚、中亚壳体接合带的形成条件甚为复杂,受所在地区长期演化所成构造背景、地幔蠕动分异作用,以及相邻壳体演化、运动三个因素控制。其中,地幔蠕动是主因。
The forming conditions of the adjoining zone between East Asia and Central Asia crustobodies are quite complicated. It is controled by three elements of the tectonic hack ground, the mantle's creeping and segregating, and the development and movement of adjacent crustobodies, among which the mantle's creeping is the cardinal factor.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1995年第4期291-302,共12页
Geotectonica et Metallogenia
基金
中科院"85"重点资助项目--"历史-因果论大地构造学的建立及其应用"项目的阶段性成果之21
关键词
壳体
地幔蠕动
东亚
中亚
壳体接合带
形成条件
Crustobody, Yinchuan-Kunming tectonic system, The mantle's creeping