摘要
苏巴什蛇绿混杂岩是北起苏巴什北侧的柳什塔格玄武岩南至乌鲁克库勒盆地南缘蛇绿混杂岩带包括其间所夹陆岛残片在内的一套构造—蛇绿混杂组合 ,它代表了古特提斯洋的活动遗迹 ,是一典型的“软碰撞”缝合带 ,它是欧亚大陆南缘一条陆内缝合带 ,并于早。
The Subashi ophiolite is a set of structural ophiolitic complex that contains the Liushitahe basalt at the north side of Suvasi and the ophiolitic complex belt containing continental island remains in the south margin of the Wulukule basin at the south. It represented the active trace of the old Tethys and is a typical 'soft collision'suture and an intracontinental suture in the south margin of Eurasian continent, which enclosed and resulted in orogeny in the early and middle Triassic period.
出处
《陕西地质》
2001年第2期40-47,66,共9页
Geology of Shaanxi
基金
1:2 5万于田
伯力克幅区域地质调查项目
编号 :1999130 0 0 0 90 6 1
