[1] Aitchison, J. C., Ali, J. R., Davis, A. M., 2007. When and Where did India and Asia Collide?. Journal of Geophysical Research Atmospheres, 112(B5):B05423. https://doi.org/10.1029/2006jb004706
[2] Aitchison, J. C., Davis, A. M., Badengzhu, et al., 2003. The Gangdese Thrust:A Phantom Structure That did not Raise Tibet. Terra Nova, 15(3):155-162. https://doi.org/10.1046/j.1365-3121.2003.00480.x
[3] Deng, S. H., Lu, Y. Z., 2008. Fossil Plants from Lower Cretaceous of the Jiuquan Basin, Gansu, Northwest China and Their Palaeoclimatic Implications. Acta Geologica Sinica, 82(1):104-114 (in Chinese with English abstract).
[4] Feng, Z., Schneider, J. W., Labandeira, C. C., et al., 2015. A Specialized Feeding Habit of Early Permian Oribatid Mites. Palaeogeography, Palaeoclimatology, Palaeoecology, 417:121-125. https://doi.org/10.1016/j.palaeo.2014.10.035
[5] Hu, Y.X., 2004. Early Cretaceous Ostracods from the Xiagou Formation of Hongliuxia in the Yumen Area, Gansu of NW China. Acta Micropalaeontologica Sinica, 21(4):439-451 (in Chinese with English abstract). http://europepmc.org/abstract/cba/466245
[6] Li, B. S., Yan, M. D., Zhang, W. L., et al., 2018. Paleomagnetic Rotation Constraints on the Deformation of the Northern Qaidam Marginal Thrust Belt and Implications for Strike-Slip Faulting along the Altyn Tagh Fault. Journal of Geophysical Research:Solid Earth, 123(9):7207-7224. https://doi.org/10.1029/2018jb015753
[7] Li, B.S., Yan, M.D., Zhang, W.L., et al., 2019. The Mechanisms of Arcuate Structures on the South Side of the Altyn Tagh Fault and Their Tectonic Implications. Seismology and Geology, 41(2):300-319 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZDZ201902004.htm
[8] Li, F.Q., Wang, C.S., Wang, C.X., 2006. Tectonic Characteristics and Origin of Jiuquan Basin Group. Acta Geologica Sinica, 80(2):181-191 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_acta-geologica-sinica_thesis/0201252709930.html
[9] Li, H. B., Yang, J. S., 2004. Evidence for Cretaceous Uplift of the Northern Qinghai-Tibetan Plateau. Earth Science Frontiers, 11(4):345-359 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200404002.htm
[10] Li, H. B., Yang, J. S., Xu, Z. Q., et al., 2006. The Constraint of the Altyn Tagh Fault System to the Growth and Rise of the Northern Tibetan Plateau. Earth Science Frontiers, 13 (4):59-79 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY200604005.htm
[11] Li, X. B., Chen, Q. L., Wei W., et al., 2006. Distribution of Cretaceous Proto-Basin and Basin-Mountain Frame Work in Inner Mongolia-Gansu-Qinghai Area. Journal of Earth Sciences and Environment, 28 (3):24-30 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-XAGX200603005.htm
[12] Liu, Z. S., 2000. Early Cretaceous Sporopollen Assemblage from the Hanxia of Yumen in Gansu, NW China. Acta Micropalaentologica Sinica, 17 (1):73-84 (in Chinese with English abstract). http://europepmc.org/abstract/cba/334720
[13] Rowley, D. B., 1998. Minimum Age of Initiation of Collision between India and Asia North of Everest Based on the Subsidence History of the Zhepure Mountain Section. The Journal of Geology, 106(2):220-235. https://doi.org/10.1086/516018
[14] Su, J. P., Wu, B. X., Lei, H. Y., et al., 2002. Sedimentary Formation and Analyses for Dynamic Evolution of Jiuxi Cretaceous Basin, Gansu Province. Acta Sedimentologica Sinica, 20 (4):568-573(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-CJXB200204005.htm
[15] Tang, W. H., Zhang, Z. C., Li, J. F., et al., 2012. Geochemical Characteristics and Tectonic Significance of the Cretaceous Volcanic Rocks in the Eastern Terminal of the Altyn Tagh Fault Zones. Earth Science Frontiers, 19 (4):51-62 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY201204006.htm
[16] Tian, N., Wang, Y., Philippe, M., et al., 2016. New Record of Fossil Wood Xenoxylon from the Late Triassic in the Sichuan Basin, Southern China and Its Paleoclimatic Implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 464:65-75. https://doi.org/10.1016/j.palaeo.2016.02.006
[17] Tian, Q. J., Ding, G. Y., 1998. The Tectonic Feature of a Quasi-Trijunction in the Northeastern Corner of Qinghai-Xizang Plateau. Earthquake Research in China, 14(4):27-35 (in Chinese with English abstract). http://www.cqvip.com/QK/84216X/199903/3000836655.html
[18] Wang, G. C., Cao, K., Zhang, K. X., et al., 2011. Spatial and Temporal Pattern of Cenozoic Tectonic Uplift in the Qinghai-Tibet Plateau. Science in China (Series D:Earth Sciences), 41 (3):332-349 (in Chinese).
[19] Wang, X. F., Zhang, Z. C., Guo, Z. J., et al., 2004. Geochemical Characteristics and Tectonic Significance of the Early Cretaceous Volcanic Rocks in the Southern Margin of Jiuxi Basin. Geological Journal of China Universities, 10(4):569-577 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-gxdx200404010.htm
[20] Wang, X. L., Zhou, H. R., Wang, Z. T., et al., 2018. Late Early Cretaceous Magmatic Event in Hongliuxia in Eastern Sector of the Altyn Tagh Fault, and Its Regional Tectonic Implications. Geoscience, 32 (1):1-15 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-XDDZ201801001.htm
[21] Wei, X. X., Zhang, X. H., Huang, X., et al., 2016. Palaeoclimate Reconstruction of Middle Permian in Tuha Basin:Evidence from the Fossil Wood Growth Rings. Earth Science, 41 (10):1771-1780 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DQKX201610012.htm
[22] Whipple, K. X., Shirzaei, M., Hodges, K. V., et al., 2016. Active Shortening within the Himalayan Orogenic Wedge Implied by the 2015 Gorkha Earthquake. Nature Geoscience, 9(9):711-716. https://doi.org/10.1038/ngeo2797
[23] Xie, S. C., Yin, H. F., Liu, D., et al., 2018. On Development from Paleontology to Geobiology:Overview of Innovation and Expansion of Application Fields. Earth Science, 43 (11):3823-3836 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201811003.htm
[24] Xu, X. W., Tapponnier, P., van der Woerd, J., et al., 2003a. Study of the Late Quaternary Left-Lateral Strike-Slip Rate of the Altyn Fault Zone and Its Tectonic Movement Transformation Model. Science in China(Series D:Earth Sciences), 33(10):967-974 (in Chinese).
[25] Xu, X. W., Wen, X. Z., Zheng, R. Z., et al., 2003b. The Late Tectonic Modification Pattern and Dynamic Sources of the Active Blocks in Sichuan-Yunnan Region. Science in China (Series D:Earth Sciences), 33 (Suppl.1):151-162 (in Chinese).
[26] Yang, G. L., Feng, B. Z., Zheng, F. J., et al., 2019. New Evidence of Early Cretaceous Petrified Wood in Yumen, North-Western Gansu, China and Its Palaeogeographical Implication. Historical Biology, 6:1-6. https://doi.org/10.1080/08912963.2019.1630831
[27] Yin, A., Harrison, T. M., 2000. Geologic Evolution of the Himalayan-Tibetan Orogen. Annual Review of Earth and Planetary Sciences, 28(1):211-280. https://doi.org/10.1146/annurev.earth.28.1.211
[28] Yin, H. F., Yu, J. X., Luo, G. M., et al., 2018. Biotic Influence on the Formation of Icehouse Climate in Geologic History. Earth Science, 43 (11):3809-3822 (in Chinese with English abstract).
[29] Yu, J. X., Pang, J. Z., Wang, Y. Z., et al., 2019. Mid-Miocene Uplift of the Northern Qilian Shan as a Result of the Northward Growth of the Northern Tibetan Plateau. Geosphere, 15 (2):423-432. https://doi.org/10.1130/GES01520.1
[30] Zhang, M. Z., Dai, S., Chen, S. Q., et al., 2013. Early Cretaceous Silicied Woods from the Yingen-Ejinaqi Basin, Inner Mongolia and Their Sedimentary Environment. Acta Geologica Sinica, 87(8):1059-1066(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201610012.htm
[31] Zhang, S. H., Zhao, Y., 2006. A Review on Tectonic Rotations Related to Large Strike-Slip Faults. Geological Science and Technology Information, 25 (3):29-34 (in Chinese with English abstract). doi: 10.3799/dqkx.2018.169
[32] Zhang, P. Z., Zheng, D. W., Yin. G. M., et al., 2006. Discussion on Late Cenozoic Growth and Rise of Northeastern Margin of the Tibetan Plateau. Quaternary Sciences, 26(1):5-13 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DSJJ200601001.htm
[33] Zhou, W. L., 2014. The Identification Characteristics, Causes and Classification Evaluation Research of Silicified Wood. Journal of the Graduates Sun Yat-Sen University (Natural Sciences, Medicine), 35(1):8-13 (in Chinese).
[34] Zuza, A. V., Wu, C., Wang, Z., et al., 2019. Underthrusting and Duplexing beneath the Northern Tibetan Plateau and the Evolution of the Himalayan-Tibetan Orogen. Lithosphere, 11(2):209-231. https://doi.org/10.1130/L1042.1
[35] 邓胜徽, 卢远征, 2008.甘肃酒泉盆地早白垩世植物化石及其古气候意义.地质学报, 82(1):104-114. http://www.cnki.com.cn/Article/CJFDTotal-DZXE200801016.htm
[36] 胡艳霞, 2004.甘肃玉门红柳峡早白垩世下沟组的介形类.微体古生物学报, 21(4):439-451. http://www.cnki.com.cn/Article/CJFDTOTAL-WSGT200404008.htm
[37] 栗兵帅, 颜茂都, 张伟林, 等, 2019.阿尔金断裂南侧弧形地貌单元成因及其构造意义.地震地质, 41(2):300-319. http://www.cnki.com.cn/Article/CJFDTotal-DZDZ201902004.htm
[38] 李奋其, 王成善, 王崇孝, 2006.酒泉早白垩世盆地群构造特征和成因.地质学报, 80(2):181-191. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200602001.htm
[39] 李海兵, 杨经绥, 2004.青藏高原北部白垩纪隆升的证据.地学前缘, 11(4):345-359. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200404002.htm
[40] 李海兵, 杨经绥, 许志琴, 等, 2006.阿尔金断裂带对青藏高原北部生长、隆升的制约.地学前缘, 13(4):59-79. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200604005.htm
[41] 李相博, 陈启林, 魏伟, 等, 2006.蒙甘青地区白垩纪原型盆地分布特征及盆山格局.地球科学与环境学报, 28(3):24-30. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX200603005.htm
[42] 刘兆生, 2000.甘肃玉门旱峡早白垩世孢粉组合.微体古生物学报, 17(1):73-84. http://www.cnki.com.cn/Article/CJFDTOTAL-WSGT200001007.htm
[43] 苏建平, 吴保祥, 雷怀彦, 等, 2002.甘肃酒西白垩纪盆地沉积构成及盆地演化动力学分析.沉积学报, 20(4):568-573. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200204005.htm
[44] 汤文豪, 张志诚, 李建锋, 等, 2012.阿尔金断裂东端白垩纪火山岩地球化学特征及其地质意义.地学前缘, 19(4):51-62. http://d.wanfangdata.com.cn/Periodical/dxqy201204006
[45] 田勤俭, 丁国瑜, 1998.青藏高原东北隅似三联点构造特征.中国地震, 14(4):27-35. http://www.cqvip.com/Main/Detail.aspx?id=3305185
[46] 王国灿, 曹凯, 张克信, 等, 2011.青藏高原新生代构造隆升阶段的时空格局.中国科学(D辑:地球科学), 41(3):332-349. http://www.cnki.com.cn/Article/CJFDTotal-JDXK201103006.htm
[47] 王晓丰, 张志诚, 郭召杰, 等, 2004.酒西盆地南缘旱峡早白垩世火山岩地球化学特征及其构造意义.高校地质学报, 10(4):569-577. http://www.cqvip.com/Main/Detail.aspx?id=11387320
[48] 王训练, 周洪瑞, 王振涛, 等, 2018.阿尔金断裂东段红柳峡早白垩世晚期岩浆事件及其区域构造意义.现代地质, 32(1):1-15. http://www.cnki.com.cn/Article/CJFDTotal-XDDZ201801001.htm
[49] 魏信祥, 张雄华, 黄兴, 等, 2016.吐哈盆地中二叠世古气候重建:来自木化石年轮的证据.地球科学, 41 (10):1771-1780. doi: 10.3799/dqkx.2016.525
[50] 谢树成, 殷鸿福, 刘邓, 等, 2018.再谈古生物学向地球生物学的发展:服务领域的拓展与创新.地球科学, 43 (11):3823-3836. http://d.wanfangdata.com.cn/periodical/dqkx201811003
[51] 徐锡伟, Tapponnier, P., van der Woerd, J., 等, 2003a.阿尔金断裂带晚第四纪左旋走滑速率及其构造运动转换模式讨论.中国科学(D辑:地球科学), 33(10):967-974. http://d.wanfangdata.com.cn/Periodical/zgkx-cd200310007
[52] 徐锡伟, 闻学泽, 郑荣章, 等, 2003b.川滇地区活动块体最新构造变动样式及其动力来源.中国科学(D辑:地球科学), 33(z1):151-162.
[53] 殷鸿福, 喻建新, 罗根明, 等, 2018.地史时期生物对冰室气候形成的作用.地球科学, 43 (11):3809-3822. doi: 10.3799/dqkx.2018.117
[54] 张明震, 戴霜, 陈世强, 等, 2013.内蒙古银根-额济纳旗盆地白垩系中硅化木化石及其沉积环境.地质学报, 87(8):1059-1066. http://www.cnki.com.cn/Article/CJFDTotal-DZXE201308003.htm
[55] 张拴宏, 赵越, 2006.与大型走滑断裂相关的旋转.地质科技情报, 25 (3):29-34.
[56] 张培震, 郑德文, 尹功明, 等, 2006.有关青藏高原东北缘晚新生代扩展与隆升的讨论.第四纪研究, 26(1):5-13.
[57] 周维丽, 2014.硅化木的鉴定特征、成因与分类评价研究.中山大学研究生学刊(自然科学与医学版), 35(1):8-13. http://www.cqvip.com/QK/83688X/201401/89748375504849524849484850.html