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在新疆佳木地区发现了第四纪台兰河断层, 它是现盆地-山脉耦合的边界断层. 利用断层对不同时代的第四纪沉积造成的不同断距的测量数据, 求得了断层在第四纪造成的盆地-山脉900 m高差, 以及地壳缩短量3.7 km和1.59 mm/a的缩短率. 所造成的山脉隆升量和山脉隆升率分别是1.34 km和0.56 mm/a. 加上盆地边缘古木别孜背斜的贡献, 佳木地区第四纪地壳缩短量和缩短率估计分别达到 4.8 km和2 mm/a. 这些数据与中国新疆库车地区所确定的缩短速度及在吉尔吉斯Issyk湖地区、中国新疆库尔勒-乌鲁木齐地区GPS重复测量的地壳缩短速度相一致, 反映了新第三纪天山南麓再生前陆盆地的冲断作用比较快速的运动.
The Quaternary Tailan fault was discovered in the Jiamu area of Xinjiang, and it is a boundary fault coupled with the basin-mountain range. Using the measured data of different fault distances caused by Quaternary sediments from different epochs, The basin-to-mountain 900 m height difference caused by the Quaternary and the shortening rate of crustal shortening of 3.7 km and 1.59 mm / a resulted in uplift and uplift rates of 1.34 km and 0.56 mm / a, respectively. On the contribution of the ancient Mabisei anticline on the margin of the basin, the shortening and shortening rates of Quaternary crust in Jiamu area are estimated to reach 4.8 km and 2 mm / a, respectively. These data are consistent with the shortening speed determined by the Kuqa region in Xinjiang, China, In the Issyk Lake region, the crustal shortening rate of GPS-repeated measurements in the Korla-Urumqi region, Xinjiang, China is consistent with the relatively rapid thrusting of the reclaimed foreland basin in the southern Tianshan Mountains.