[1] Ai, N.S., Wang, Y.X., 1984. Relationship between River System and Neotectonic Stress Field in Yili Basin. Xinjiang Geography, 7(1): 28-34(in Chinese).
[2] Deng, Q.D., Feng, X.Y., Zhang, P.Z., et al., 2000. Active Teconics in Tianshan. Seismological Press, Beijing, 399(in Chinese).
[3] Ge, X.H., Ren, S.M., Ma, L.X., et al., 2006.Multi-Stage Uplifts of the Qinghai-Tibet Plateau and Their Environmental Effects.Earth Science Frontiers, 13(6):118-130(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200606015
[4] He, Z.T., Ma, B.Q., Long, J. Y., et al., 2018. New Progress in Paleoearthquake Studies of the East Sertengshan Piedmont Fault, Inner Mongolia, China. Journal of Earth Science, 29(2): 441-451. https://doi.org/10.1007/s12583-017-0937-z doi:  10.1007/s12583-017-0937-z
[5] Jia, C.Z., 2007.The Characteristics of Intra-Continental Deformation and Hydrocarbon Distribution Controlled by the Himalayan Tectonic Movements in China. Earth Science Frontiers, 14(4):96-104(in Chinese with English abstract). doi:  10.1016/S1872-5791(07)60030-X
[6] Li, J. H., Webb, A. A. G., Mao, X., et al., 2014. Active Surface Salt Structures of the Western Kuqa Fold-Thrust Belt, Northwestern China. Geosphere, 10(6): 1219-1234. https://doi.org/10.1130/ges01021.1 doi:  10.1130/ges01021.1
[7] Li, B.L., Chen, Z.X., Lei, Y.L., et al., 2011.Structural Geology Correlation of Foreland Thrust-Folded Belts between the Southern and Northern Edges of the Tianshan Mountain and Some Suggestions for Hydrocarbon Exploration.Acta Petrolei Sinica, 32(3):395-403(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syxb201103004
[8] Li, C.X., Song, Y.G., Wang, L.M., 2013.The Research Progress on Ili Loess.Marine Geology & Quaternary Geology, 33(1):145-152(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ201301023.htm
[9] Li, J.J., 1999.Studies on the Geomorphological Evolution of the Qinghai-Xizang (Tibetan) Plateau and Asian Monsoon.Marine Geology & Quaternary Geology, 19(1):1-11(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz199901002
[10] Liu, C.R., Yin, G.M., Gao, L., et al., 2010. ESR Dating of Pleistocene Archaeological Localities of the Nihewan Basin, North China—Preliminary Results. Quaternary Geochronology, 5(2-3): 385-390. https://doi.org/10.1016/j.quageo.2009.05.006 doi:  10.1016/j.quageo.2009.05.006
[11] Liu, C.R., Yin, G.M., Gao, L., et al., 2011.Research Advances in ESR Geochronology of Quaternary Deposits.Seismology and Geology, 33(2):490-498(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzdz201102022
[12] Liu, Z.H., Lu, H.F., Jia, C.Z., et al., 2001.Structures and Hydrocarbon Accumulation in Kuqa Rejuvenated Foreland Basin.Oil & Gas Geology, 22(4):297-303(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz200104003
[13] Liu, Z.J., Sun, Y.J., 2007.Uplift of the Qinghai-Tibet Plateau and Formation, Evolution of the Yellow River.Geography and Geo-Information Science, 23(1):79-82, 91(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLGT200701018.htm
[14] Lu, H.F., Chen, C.M., Liu, Z.H., et al., 2000.The Structural Features and Origin of the Kuqa Rejuvenation Foreland Thrust Belt.Acta Petrolei Sinica, 21(3):18-24(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syxb200003004
[15] Lu, H. F., Howell, D. G., Jia, D., et al., 1994. Rejuvenation of the Kuqa Foreland Basin, Northern Flank of the Tarim Basin, Northwest China. International Geology Review, 36(12): 1151-1158. https://doi.org/10.1080/00206819409465509 doi:  10.1080/00206819409465509
[16] Luo, D.G., Liu, J.P., Jin, C., et al., 2017.Instantaneous Seismic Attributes and Response Characteristics of Active Faults.Earth Science, 42(3):462-470(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201703013
[17] Luo, F.Z., Bai, M.X., Chen, J.B., 2003.Study on New Activity Characteristics of the Active Faults in Yining Basin of Xinjiang.Inland Earthquake, 17(1):4-10(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=nldz200301002
[18] Qin, M.K., Wang, Z.B., Zhao, R.Q., 1998.Characteristics of Clay Minerals and Their Relationships with Uranium Mineralization in Uranium Deposit No.512, Yili Basin.Earth Science, 23(5):508-512(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx199805013
[19] Shen, J., Bai, M.X., Shi, G.L., 2011.Brief Introduction on the Seismotectonic Map of Xinjiang and Its Neighborhood.Inland Earthquake, 25(2):97-108(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-LLDZ201102002.htm
[20] Shi, Y.F., Li, J.J., Li, B.Y., et al., 1999.Uplift of the Qinghai-Xizang (Tibetan) Plateau and East Asia Environmental Change during Late Cenozoic.Acta Geographica Sinica, 54(1):10-21(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dlxb199901002
[21] Song, Y.G., Shi, Z.T., Fang, X., et al., 2010. Loess Magnetic Properties in the Ili Basin and Their Correlation with the Chinese Loess Plateau. Science China Earth Sciences, 40 (1): 61-72(in Chinese). doi:  10.1007/s11430-010-0011-5
[22] Sun, J.M., Zhang, Z. Q., 2009. Syntectonic Growth Strata and Implications for Late Cenozoic Tectonic Uplift in the Northern Tian Shan, China. Tectonophysics, 463(1-4): 60-68. https://doi.org/10.1016/j.tecto.2008.09.008 doi:  10.1016/j.tecto.2008.09.008
[23] Song, Y.G., Shi, Z.T., 2010.Distribution and Compositions of Loess Sediments in Yili Basin, Central Asia.Scientia Geographica Sinica, 30(2):267-272(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLKX201002018.htm
[24] Sun, J.M., Xu, Q.H., Huang, B.C., 2007. Late Cenozoic Magnetochronology and Paleoenvironmental Changes in the Northern Foreland Basin of the Tian Shan Mountains. Journal of Geophysical Research: Solid Earth, 112(B4):B04107. https://doi.org/10.1029/2006jb004653 doi:  10.1029/2006jb004653
[25] Sun, Y.G., Fang, H.B., Zhang, K., et al., 2007.Step-Like Landform System of the Gonghe Basin and the Uplift of the Qinghai-Tibet Plateau and Development of the Yellow River.Geology in China, 34(6):1141-1147(in Chinese with English abstract).
[26] Sun, Z.X., Liu, J.H., Zhu, Y.G., et al., 2004.Ore-Forming Process and Redox Zoning of Sandstone-Type U Deposits:Evidence from U Series Disequilibrium.Earth Science, 29(2):224-230(in Chinese with English abstract).
[27] Tian, Z. H., Sun, J. M., Windley, B. F., et al., 2016. Cenozoic Detachment Folding in the Southern Tianshan Foreland, NW China: Shortening Distances and Rates. Journal of Structural Geology, 84: 142-161. https://doi.org/10.1016/j.jsg.2016.01.007 doi:  10.1016/j.jsg.2016.01.007
[28] Wang, X., Suppe, J., Guan, S.H., et al., 2011. Cenozoic Structure and Tectonic Evolution of the Kuqa Fold Belt, Southern Tianshan, China. AAPG Memoir, 94: 215-243.
[29] Wang, Y., Chen, Z.L., Liu, J., et al., 2006.Neotectonics in Southern Yili Basin and Its Control of Sandstone-Type Uranium Deposits.Geotectonica et Metallogenia, 30(4):486-494(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ddgzyckx200604011
[30] Wen, L., Li, Y.J., Zhang, G.Y., et al., 2017. Evolution of Fold-Thrust Belts and Cenozoic Uplifting of the South Tianshan Mountain Range in the Kuqa Region, Northwest China. Journal of Asian Earth Sciences, 135: 327-337. https://doi.org/10.1016/j.jseaes.2017.01.002 doi:  10.1016/j.jseaes.2017.01.002
[31] Wen, L., Yang, H.J., Li, Y.J., et al., 2016.Kuqa Late Cenozoic Fold-Thrust Belt in the Southern Flank of Tianshan Mountains.Acta Petrologica Sinica, 32(3):847-855(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201603016
[32] Wu, G.D., Yin, G.H., 2010.Research on Subsection of Kashi River Fault Zone in Ili of Xinjiang.Inland Earthquake, 24(1):25-30(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=nldz201001005
[33] Yin, G.H., 1993. Neotectonic Movement and Earthquakes in Ili Basin. Inland Earthquake, 7(2): 180-187(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-LLDZ199302013.htm
[34] Yin, G.H., Jiang, J.X., Zhang, Y., et al., 2003.Research on Kashi River Fault in Yili, Xinjiang and Its Activity.Inland Earthquake, 17(2):109-116(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=nldz200302003
[35] Yu, X.J., Guo, Z.J., Zhang, D.W., et al., 2018.Quaternary Shaking:Evidences of Tectonic Intensification from the Qaidam Basin and Its Influence on Multi-Spherical Interaction.Quaternary Sciences, 38(1):39-53(in Chinese with English abstract).
[36] Yuan, S.H., Bai, X.D., Liang, W.T., et al., 2016.Characteristics and Latest Activity of Hongshanzui Fault in Northwestern Yili Basin, Xinjiang.Geological Bulletin of China, 35(1):117-122(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD201601010.htm
[37] Zhang, G.W., Li, S.Z., Liu, J.X., et al., 1999.Structural Feature and Evolution of Yili Basin, Xinjiang.Earth Science Frontiers, 6(4):203-214(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy199904002
[38] Zhang, J., Li, J.Y., Zhu, Z.X., 2009.The Late Cenozoic Deformation of the Wusunshan Mountain in the Yili Basin and Its Significance.Xinjiang Geology, 27(2):101-105(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xjdz200902001
[39] Zhang, P.Z., 2004. Late Cenozoic Tectonic Deformation in the Tianshan Mountain and Its Foreland Basins. Chinese Science Bulletin, 49(4): 311. https://doi.org/10.1360/03wd0488 doi:  10.1360/03wd0488
[40] Zhang, P.Z., Deng, Q.D., Yang, X.P., et al., 1996.Late Cenozoic Tectonic Deformation and Mechanism along the Tianshan Mountain, Northwestern China. Earthquake Research in China, 12(2):127-140(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZGZD199602002.htm
[41] Zhang, Z.L., Sun, J.M., Tian, Z. H., et al., 2016. Magnetostratigraphy of Syntectonic Growth Strata and Implications for the Late Cenozoic Deformation in the Baicheng Depression, Southern Tian Shan. Journal of Asian Earth Sciences, 118: 111-124. https://doi.org/10.1016/j.jseaes.2015.12. 024 doi:  10.1016/j.jseaes.2015.12.024
[42] 艾南山, 王永兴, 1984.伊犁盆地的水系与新构造应力场的关系.新疆地理, 7(1):28-34. http://www.cnki.com.cn/Article/CJFDTotal-GHDL198401005.htm
[43] 邓起东, 冯先岳, 张培震, 等, 2000.天山活动构造.北京:地震出版社, 399.
[44] 葛肖虹, 任收麦, 马立祥, 等, 2006.青藏高原多期次隆升的环境效应.地学前缘, 13(6):118-130. doi:  10.3321/j.issn:1005-2321.2006.06.015
[45] 贾承造, 2007.中国喜马拉雅构造运动的陆内变形特征与油气矿藏富集.地学前缘, 14(4):96-104. doi:  10.3321/j.issn:1005-2321.2007.04.010
[46] 李本亮, 陈竹新, 雷永良, 等, 2011.天山南缘与北缘前陆冲断带构造地质特征对比及油气勘探建议.石油学报, 32(3):395-403. http://d.old.wanfangdata.com.cn/Periodical/syxb201103004
[47] 李传想, 宋友桂, 王乐民, 2013.新疆伊犁黄土研究.海洋地质与第四纪地质, 33(1):145-152. http://d.old.wanfangdata.com.cn/Periodical/dsjyj201005008
[48] 李吉均, 1999.青藏高原的地貌演化与亚洲季风.海洋地质与第四纪地质, 19(1):1-11. http://d.old.wanfangdata.com.cn/Periodical/hydzydsjdz199901002
[49] 刘春茹, 尹功明, 高璐, 等, 2011.第四纪沉积物ESR年代学研究进展.地震地质, 33(2):490-498. doi:  10.3969/j.issn.0253-4967.2011.02.022
[50] 刘志宏, 卢华复, 贾承造, 等, 2001.库车再生前陆盆地的构造与油气.石油与天然气地质, 22(4):297-303. doi:  10.3321/j.issn:0253-9985.2001.04.003
[51] 刘志杰, 孙永军, 2007.青藏高原隆升与黄河形成演化.地理与地理信息科学, 23(1):79-82, 91. doi:  10.3969/j.issn.1672-0504.2007.01.019
[52] 卢华复, 陈楚铭, 刘志宏, 等, 2000.库车再生前陆逆冲带的构造特征与成因.石油学报, 21(3):18-24. doi:  10.3321/j.issn:0253-2697.2000.03.004
[53] 罗登贵, 刘江平, 金聪, 等, 2017.活断层的地震响应特征与瞬时地震属性.地球科学, 42(3):462-470. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201703013.htm
[54] 罗福忠, 柏美祥, 陈建波, 2003.新疆伊宁盆地活动断裂新活动特征研究.内陆地震, 17(1):4-10. doi:  10.3969/j.issn.1001-8956.2003.01.002
[55] 秦明宽, 王正邦, 赵瑞全, 1998.伊犁盆地512铀矿床粘土矿物特征与铀成矿作用.地球科学, 23(5): 508-512. http://www.earth-science.net/article/id/687
[56] 沈军, 柏美祥, 石广岭, 2011.新疆及邻区地震构造图简介.内陆地震, 25(2):97-108. doi:  10.3969/j.issn.1001-8956.2011.02.001
[57] 施雅风, 李吉均, 李炳元, 等, 1999.晚新生代青藏高原的隆升与东亚环境变化.地理学报, (1):10-21. doi:  10.3321/j.issn:0375-5444.1999.01.002
[58] 宋友桂, 史正涛, 2010.伊犁盆地黄土分布与组成特征.地理科学, 30(2):267-272. http://d.old.wanfangdata.com.cn/Conference/7315666
[59] 宋友桂, 史正涛, 方小敏, 等, 2010.伊犁黄土的磁学性质及其与黄土高原对比.中国科学:地球科学, 40(1):61-72. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK201000131332
[60] 孙延贵, 方洪宾, 张琨, 等, 2007.共和盆地层状地貌系统与青藏高原隆升及黄河发育.中国地质, 34(6):1141-1147. doi:  10.3969/j.issn.1000-3657.2007.06.021
[61] 孙占学, 刘金辉, 朱永刚, 等, 2004.砂岩铀矿成矿过程与氧化还原分带:铀系不平衡证据.地球科学, 29(2):224-230. http://www.earth-science.net/article/id/1352
[62] 王勇, 陈正乐, 刘健, 等, 2006.伊犁盆地南部新构造特征及其对砂岩型铀矿的控制作用.大地构造与成矿学, 30(4):486-494. doi:  10.3969/j.issn.1001-1552.2006.04.011
[63] 文磊, 杨海军, 李曰俊, 等, 2016.天山南麓库车晚新生代褶皱-冲断带.岩石学报, 32(3):847-855. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201603016
[64] 吴国栋, 尹光华, 2010.新疆伊犁喀什河断裂带分段性研究.内陆地震, 24(1):25-30. doi:  10.3969/j.issn.1001-8956.2010.01.005
[65] 尹光华, 1993.伊犁盆地新构造运动与地震.内陆地震, 7(2): 180-187. http://www.cnki.com.cn/Article/CJFDTotal-LLDZ199302013.htm
[66] 尹光华, 蒋靖祥, 张勇, 2003.新疆伊犁喀什河断裂带及其活动性研究.内陆地震, 17(2):109-116. doi:  10.3969/j.issn.1001-8956.2003.02.003
[67] 于祥江, 郭召杰, 张道伟, 等, 2018.第四纪悸动:来自柴达木盆地构造增强的证据及其对多圈层的响应.第四纪研究, 38(1):39-53. http://d.old.wanfangdata.com.cn/Periodical/dsjyj201801003
[68] 袁四化, 白相东, 梁文天, 等, 2016.新疆伊犁盆地西北缘红山嘴断裂特征与最新活动.地质通报, 35(1):117-122. doi:  10.3969/j.issn.1671-2552.2016.01.010
[69] 张国伟, 李三忠, 刘俊霞, 等, 1999.新疆伊犁盆地的构造特征与形成演化.地学前缘, 6(4):203-214. doi:  10.3321/j.issn:1005-2321.1999.04.002
[70] 张进, 李锦轶, 朱志新, 2009.伊犁盆地南部乌孙山晚新生代变形特征及意义.新疆地质, 27(2):101-105. doi:  10.3969/j.issn.1000-8845.2009.02.001
[71] 张培震, 邓起东, 杨晓平, 等, 1996.天山的晚新生代构造变形及其地球动力学问题.中国地震, 12(2) :127-140. http://www.cnki.com.cn/Article/CJFDTotal-ZGZD199602002.htm