Ailaoshan-Jingshajiang belt 哀牢山
The oblique strike slip structure is resulted from the closing of little Jingshajiang regeneration ocean basin and the oblique intercontinental collision in late Triassic.
滇西北拖顶地区斜向走滑构造是金沙江再生小洋盆关闭、陆-陆斜向碰撞构造转化的结果。
youdao
应用推荐
模块上移
模块下移
不移动