新疆西准噶尔地区位于西伯利亚板块与准噶尔板块的碰撞带。
Western Zhunge 'er of Xinjiang lies at the collision belt between Siberia and Zhunge 'er plate.
三叠纪至古近纪，板块挤压作用减弱，准噶尔盆地由强烈压陷期逐渐进入坳陷沉降阶段。
From Triassic to Palaeogene, the plate squeezing action weakened and Junggar basin gradually entered a depression-subsidence phase from the intense compressive phase.
东准噶尔双泉一带的韧-脆性剪切带是在板块结合带基础上，形成于陆-陆碰撞体制。
Basing on the combination of plates, ductile-brittle shear zone in the ShuangQuan area, Eastern JungGar forms in the system of continental - continental collision.
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