Abstract：Through the detailed research on petrography, mineralogy, contact relation, wallrock structures and forming age, according to the classification principles of tectono-magmatic evolutionary times, the intrusive rocks on the west Alashankou in Xinjiang Region is disintegrated and regrouped as the Carboniferous crust-mantle mixed succession, including eight intrusive sequences, with pulsatile contact relation between each sequence. Considering the form, structure and the deformation and metamorphism of wallrocks, the Kezilezhayilao big batholith is passively emplaced with the balloon-like inflation in the pull-apart stress field that formed between the northwest-trending strike-slip faults.
梁有为, 于海峰, 王福君, 潘明臣, 王志军, 潘玉启, 鲁红峰. 阿拉山口西侧侵入岩的解体及克孜勒扎依劳大岩基就位机制分析[J]. 地质与资源, 2011, 20(2): 149-154.
IANG You-wei, YU Hai-feng, WANG Fu-jun, PAN Ming-chen, WANG Zhi-jun, PAN Yu-qi, LU Hong-feng. THE DISINTEGRATION OF THE INTRUSIVE ROCKS ON THE WEST OF ALASHANKOU AND THE EMPLACEMENT MECHANISM OF THE KEZILEZHAYILAO BIG BATHOLITH. GEOLOGY AND RESOURCES, 2011, 20(2): 149-154.
2011, Vol. 20 
辽公网安备 21010502000112号