Abstract:The Nalati-Hongliuhe suture zone between the Kazakhstan-Junggar plate and Tarim plate along the Western Tianshan tectonic belt plays an important role in the tectonic evolution of Western Tianshan. The regional metamorphic rocks and dynamometamorphic rocks (including mylonite and cataclasite) distributed along the suture zone constitute an intact evolutionary sequence, which are the product of different evolutionary stages (time) and different evolutionary levels (space). From the spatiotemporal evolution characteristics of the metamorphic rocks, it can be seen that, since the Early Ancient South Tianshan Ocean closed in Devonian period, the Western Tianshan tectonic belt has been strongly rising in the north-south compressive stress field.
梁有为, 于海峰, 王志军, 潘明臣, 潘玉, 鲁红峰, 李红梅, 王福君, 郭洪方. 西天山那拉提-红柳河缝合带变质岩特征及演化[J]. 地质与资源, 2014, 23(2): 158-163,134.
LIANG You-wei, YU Hai-feng, WANG Zhi-jun, PAN Ming-chen, PAN Yu-qi, LU Hong-feng, LI Hong-mei, WANG Fu-jun, GUO Hong-fang. CHARACTERISTICS AND EVOLUTION OF THE METAMORPHIC ROCKS IN THE NALATI-HONGLIUHE SUTURE ZONE IN WESTERN TIANSHAN. GEOLOGY AND RESOURCES, 2014, 23(2): 158-163,134.