[1] Lu H Y, Wang X Y, Wang Y, et al. Chinese loess and the Asian monsoon: What we know and what remains unknown[J]. Quaternary International, 2022, 620: 85-97.
[2] 邵可涵,鹿化煜,陈久毅,等. 郑州邙山黄土碳酸盐和白云石含量记录的80 ka以来季风降水变化及驱动机制[J]. 第四纪研究,2020,40(6):1622-1630.

Shao Kehan, Lu Huayu, Chen Jiuyi, et al. East Asian monsoon precipitation variations over the past 80 ka revealed by carbonate and dolomite content in loess deposit at Zhengzhou (central China) and forcing mechanism[J]. Quaternary Sciences, 2020, 40(6): 1622-1630.
[3] 蒋复初,吴锡浩,肖华国,等. 郑州邙山桃花峪高分辨率晚更新世黄土地层[J]. 地质力学学报,1997,3(2):11-17.

Jiang Fuchu, Wu Xihao, Xiao Huaguo, et al. The high resolution Late Pleistocene loess stratigraphy in Taohuayu, Mangshan, Zhengzhou[J]. Journal of Geomechanics, 1997, 3(2): 11-17.
[4] Qiu F Y, Zhou L P. A new luminescence chronology for the Mangshan loess-palaeosol sequence on the southern bank of the Yellow River in Henan, central China[J]. Quaternary Geochronology, 2015, 30: 24-33.
[5] 蒋复初,吴锡浩,孙东怀,等. 中原邙山黄土地层[J]. 地质力学学报,1998,4(4):12-18.

Jiang Fuchu, Wu Xihao, Sun Donghuai, et al. On Mangshan loess stratigraphy in China central plains[J]. Journal of Geomechanics, 1998, 4(4): 12-18.
[6] 王喜生,杨振宇,王书兵,等. 中原邙山黄土下部地层的古地磁初步结果[C]//中国地球物理学会第二十四届年会论文集. 北京:中国大地出版社,2008:599.

Wang Xisheng, Yang Zhenyu, Wang Shubing,et al. Preliminary Paleomagnetic Results of the Lower Strata of the Mangshan Loess in the Central Plains [C]//Proceedings of the 24th Annual Meeting of the Chinese Geophysical Society. Beijing: China Land Press,2008:599.
[7] 杨革联,赵希涛,朱日祥,等. 河南荥阳孤柏嘴黄土剖面磁性地层学初步研究[J]. 现代地质,2001,15(1):35-39.

Yang Gelian, Zhao Xitao, Zhu Rixiang, et al. A preliminary study in magnetostratigraphy of Gubaizui loess section in Xingyang, Henan province[J]. Geoscience, 2001, 15(1): 35-39.
[8] 杨州,王书兵,蒋复初,等. 中原邙山黄土地层划分的讨论[J]. 地质力学学报,2018,24(2):274-282.

Yang Zhou, Wang Shu-bing, Jiang Fuchu, et al. Discussion on Mangshan loess stratigraphic divison in China central plains[J]. Journal of Geomechanics, 2018, 24(2): 274-282.
[9] 季军良,郑洪波,刘锐,等. 邙山黄土地层再研究[J]. 海洋地质与第四纪地质,2004,24(4):101-108.

Ji Junliang, Zheng Hongbo, Liu Rui, et al. Restudy on the stratigraphy of Mangshan loess[J]. Marine Geology & Quaternary Geology, 2004, 24(4): 101-108.
[10] Jin C S, Liu Q S. Revisiting the stratigraphic position of the Matuyama-Brunhes geomagnetic polarity boundary in Chinese loess[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 299(1/2): 309-317.
[11] Peterse F, Martínez-García A, Zhou B, et al. Molecular records of continental air temperature and monsoon precipitation variability in East Asia spanning the past 130, 000 years[J]. Quaternary Science Reviews, 2014, 83: 76-82.
[12] Zhang H Z, Lu H Y, He J, et al. Large-number detrital zircon U-Pb ages reveal global cooling caused the formation of the Chinese Loess Plateau during Late Miocene[J]. Science Advances, 2022, 8(41): eabq2007.
[13] Bird A, Stevens T, Rittner M, et al. Quaternary dust source variation across the Chinese Loess Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2015, 435: 254-264.
[14] Stevens T, Carter A, Watson T P, et al. Genetic linkage between the Yellow River, the Mu Us desert and the Chinese Loess Plateau[J]. Quaternary Science Reviews, 2013, 78: 355-368.
[15] Pullen A, Kapp P, McCallister A T, et al. Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications[J]. Geology, 2011, 39(11): 1031-1034.
[16] 曾方明,向树元,刘向军,等. 黄土高原风尘堆积物源研究进展[J]. 地球科学:中国地质大学学报,2014,39(2):125-140.

Zeng Fangming, Xiang Shuyuan, Liu Xiangjun, et al. Progress in tracing provenance of eolian deposits in Chinese Loess Plateau[J]. Earth Science: Journal of China University of Geosciences, 2014, 39(2): 125-140.
[17] Xiao G Q, Zong K Q, Li G J, et al. Spatial and glacial‐interglacial variations in provenance of the Chinese Loess Plateau[J]. Geophysical Research Letters, 2012, 39(20): L20715.
[18] Shang Y, Prince M A, Beets C J, et al. Aeolian dust supply from the Yellow River floodplain to the Pleistocene loess deposits of the Mangshan plateau, central China: Evidence from zircon U-Pb age spectra[J]. Quaternary Science Reviews, 2018, 182: 131-143.
[19] 蒋复初,吴锡浩,肖华国,等. 中原邙山黄土及构造与气候耦合作用[J]. 海洋地质与第四纪地质,1999,19(1):45-51.

Jiang Fuchu, Wu Xihao, Xiao Huaguo, et al. Mangshan loess in China central plains and the coupling effect between tectonics and climate[J]. Marine Geology & Quaternary Geology, 1999, 19(1): 45-51.
[20] 蒋复初,王书兵,傅建利,等. 河南邙山晚更新世黄土的环境记录[J]. 第四纪研究,2003,23(6):702.

Jiang Fuchu, Wang Shubing, Fu Jianli, et al. Palaeoenvironmental records preserved in the Late Pleistocene loess in the Mangshan plateau, Henan, China[J]. Quaternary Sciences, 2003, 23(6): 702.
[21] 蒋复初,王书兵,赵志中,等. 中原邙山黄土与末次间冰期以来古季风特征[J]. 地质论评,2004,50(5):554-560.

Jiang Fuchu, Wang Shubing, Zhao Zhizhong, et al. The Mangshan loess in central China and paleomonsoon characteristic since the last interglacial stage[J]. Geological Review, 2004, 50(5): 554-560.
[22] Zheng H B, Huang X T, Ji J L, et al. Ultra-high rates of loess sedimentation at Zhengzhou since Stage 7: Implication for the Yellow River erosion of the Sanmen Gorge[J]. Geomorphology, 2007, 85(3/4): 131-142.
[23] 吴锡浩,蒋复初,王苏民,等. 关于黄河贯通三门峡东流入海问题[J]. 第四纪研究,1998(2):188.

Wu Xihao, Jiang Fuchu, Wang Sumin, et al. On problem of the Yellow River passing through the Sanmen Gorge and flowing east into sea[J]. Quaternary Sciences, 1998(2): 188.
[24] 陈立业,张珂,傅建利,等. 邙山黄土古土壤S2沉积以来的微量和稀土元素地球化学特征及其物源指示意义[J]. 中山大学学报(自然科学版),2018,57(3):14-23.

Chen Liye, Zhang Ke, Fu Jianli, et al. The trace and rare earth element characteristics of Mangshan loess since deposit of paleosol S2 and its implications for provenance[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2018, 57(3): 14-23.
[25] 陈立业,张珂,傅建利,等. 邙山黄土L5以来的常量元素地球化学特征及其对物源的指示意义[J]. 第四纪研究,2017,37(6):1293-1308.

Chen Liye, Zhang Ke, Fu Jianli, et al. Major element geochemical characteristics of Mangshan loess since L5 and its implications for provenance[J]. Quaternary Sciences, 2017, 37(6): 1293-1308.
[26] 蒋复初,傅建利,王书兵,等. 关于黄河贯通三门峡的时代[J]. 地质力学学报,2005,11(4):293-301.

Jiang Fuchu, Fu Jianli, Wang Shubing, et al. The age of the Yellow River passing through the Sanmen Gorge[J]. Journal of Geomechanics, 2005, 11(4): 293-301.
[27] Wu X H, Jiang F C, Xiao H G, et al. Mangshan loess on China's Central Plain and its response to tectonic movement and climate[J]. Science China (Seri. D): Earth Sciences, 1999, 42(5): 465-473.
[28] Chen Q, Liu X M, Zhao G Y, et al. 0.2 Ma or 1.2 Ma? Timing of the linking of the middle and lower reaches of the Yellow River inferred from loess-palaeosol sequences[J]. Geophysical Research Letters, 2022, 49(6): e2021GL097510.
[29] 王苏民,吴锡浩,张振克,等. 三门古湖沉积记录的环境变迁与黄河贯通东流研究[J]. 中国科学:地球科学,2001,31(9):760-768.

Wang Sumin, Wu Xihao, Zhang Zhenke, et al. Sedimentary records of environmental evolution in the Sanmen lake basin and the Yellow River running through the Sanmenxia Gorge eastward into the sea[J]. Science China: Earth Sciences, 2001, 31(9): 760-768.
[30] Zhang H Z, Lu H Y, Zhou Y L, et al. Heavy mineral assemblages and U-Pb detrital zircon geochronology of sediments from the Weihe and Sanmen basins: New insights into the Pliocene-Pleistocene evolution of the Yellow River[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2021, 562: 110072.
[31] Wang X, Hu G, Saito Y, et al. Did the modern Yellow River form at the Mid-Pleistocene transition?[J]. Science Bulletin, 2022, 67(15): 1603-1610.
[32] 潘桂棠,肖庆辉,陆松年,等. 中国大地构造单元划分[J]. 中国地质,2009,36(1):1-28.

Pan Guitang, Xiao Qinghui, Lu Songnian, et al. Subdivision of tectonic units in China[J]. Geology in China, 2009, 36(1): 1-28.
[33] 胡健民,孟庆任,石玉若,等. 松潘—甘孜地体内花岗岩锆石SHRIMP U-Pb定年及其构造意义[J]. 岩石学报,2005,21(3):867-880.

Hu Jianmin, Meng Qingren, Shi Yuruo, et al. SHRIMP U-Pb dating of zircons from granitoid bodies in the Songpan-Ganzi terrane and its implications[J]. Acta Petrologica Sinica, 2005, 21(3): 867-880.
[34] 封铿,李瑞保,裴先治,等. 东昆仑造山带东段大格勒花岗岩锆石U-Pb年代学、地球化学特征及其构造意义[J]. 地球科学与环境学报,2020,42(4):442-463.

Feng Keng, Li Ruibao, Pei Xianzhi, et al. Zircon U-Pb dating and geochemical characteristics of Dagele granite in the eastern margin of east Kunlun orogenic belt, China and their tectonic implications[J]. Journal of Earth Sciences and Environment, 2020, 42(4): 442-463.
[35] 张传林,陆松年,于海锋,等. 青藏高原北缘西昆仑造山带构造演化:来自锆石SHRIMP及LA-ICP-MS测年的证据[J]. 中国科学:地球科学,2007,37(2):145-154.

Zhang Chuanlin, Lu Songnian, Yu Haifeng, et al. Tectonic evolution of the West Kunlun orogenic belt on the northern margin of the Qinghai-Tibet Plateau: Evidence from zircon SHRIMP and LA-ICP-MS dating[J]. Science China: Earth Sciences, 2007, 37(2): 145-154.
[36] 吴才来,徐学义,高前明,等. 北祁连早古生代花岗质岩浆作用及构造演化[J]. 岩石学报,2010,26(4):1027-1044.

Wu Cailai, Xu Xueyi, Gao Qianming, et al. Early Palaezoic grranitoid magmatism and tectonic evolution in North Qilian, NW China[J]. Acta Petrologica Sinica, 2010, 26(4): 1027-1044.
[37] 李江海,钱祥麟,黄雄南,等. 华北陆块基底构造格局及早期大陆克拉通化过程[J]. 岩石学报,2000,16(1):1-10.

Li Jianghai, Qian Xianglin, Huang Xiongnan, et al. Tectonic framework of North China Block and its cratonization in the early Precambrian[J]. Acta Petrologica Sinica, 2000, 16(1): 1-10.
[38] 朱日祥,徐义刚,朱光,等. 华北克拉通破坏[J]. 中国科学:地球科学,2012,42(8):1135-1159.

Zhu Rixiang, Xu Yigang, Zhu Guang, et al. Destruction of the North China Craton[J]. Science China: Earth Sciences, 2012, 42(8): 1135-1159.
[39] 翟明国. 克拉通化与华北陆块的形成[J]. 中国科学:地球科学,2011,41(8):1037-1046.

Zhai Mingguo. Cratonization and the Ancient North China continent: A summary and review[J]. Science China: Earth Sciences, 2011, 41(8): 1037-1046.
[40] 沈其韩,耿元生,宋彪,等. 华北和扬子陆块及秦岭—大别造山带地表和深部太古宙基底的新信息[J]. 地质学报,2005,79(5):616-627.

Shen Qihan, Geng Yuansheng, Song Biao, et al. New information from the surface outcrops and deep crust of Archean rocks of the North China and Yangtze Blocks, and Qinling-Dabie orogenic belt[J]. Acta Geologica Sinica, 2005, 79(5): 616-627.
[41] 翟明国,胡波,彭澎,等. 华北中—新元古代的岩浆作用与多期裂谷事件[J]. 地学前缘,2014,21(1):100-119.

Zhai Mingguo, Hu Bo, Peng Peng, et al. Meso-Neoproterozoic magmatic events and multi-stage rifting in the NCC[J]. Earth Science Frontiers, 2014, 21(1): 100-119.
[42] Nie J S, Stevens T, Rittner M, et al. Loess Plateau storage of northeastern Tibetan Plateau-derived Yellow River sediment[J]. Nature Communications, 2015, 6(1): 8511.
[43] Yang J, Gao S, Chen C, et al. Episodic crustal growth of North China as revealed by U-Pb age and Hf isotopes of detrital zircons from modern rivers[J]. Geochimica et Cosmochimica Acta, 2009, 73(9): 2660-2673.
[44] 王海然,赵红格,乔建新,等. 锆石U-Pb同位素测年原理及应用[J]. 地质与资源,2013,22(3):229-232,242.

Wang Hairan, Zhao Hongge, Qiao Jianxin, et al. Theory and application of zircon U-Pb isotope dating technique[J]. Geology and Resources, 2013, 22(3): 229-232, 242.
[45] Zhang H Z, Lu H Y, Xu X S, et al. Quantitative estimation of the contribution of dust sources to Chinese loess using detrital zircon U-Pb age patterns[J]. Journal of Geophysical Research: Earth Surface, 2016, 121(11): 2085-2099.
[46] Zhang H Z, Lu H Y, Stevens T, et al. Expansion of dust provenance and aridification of Asia Since~7.2 Ma revealed by detrital zircon U-Pb dating[J]. Geophysical Research Letters, 2018, 45(24): 13437-13448.
[47] Wiedenbeck M, Allé P, Corfu F, et al. Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses[J]. Geostandards and Geoanalytical Research, 1995, 19(1): 1-23.
[48] Watling R J, Herbert H K, Abell I D. The application of laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) to the analysis of selected sulphide minerals[J]. Chemical Geology, 1995, 124(1/2): 67-81.
[49] Pearce N J G, Perkins W T, Westgate J A, et al. A compilation of new and published major and trace element data for NIST SRM 610 and NIST SRM 612 glass reference materials[J]. Geostandards and Geoanalytical Research, 1997, 21(1): 115-144.
[50] Anderson T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192(1/2): 59-79.
[51] 李云,宋友桂,聂军胜,等. 基于U-Pb定年和单颗粒锆石粒径分析示踪中国黄土高原黄土和红粘土物源[J]. 地质论评,2014,60(2):380-388.

Li Yun, Song Yougui, Nie Junsheng, et al. Tracing the provenance of loess and red clay on the Chinese Loess Plateau using the U-Pb dating and single-size zircon size[J]. Geological Review, 2014, 60(2): 380-388.
[52] 何梦颖,郑洪波,贾军涛. 长江现代沉积物碎屑锆石U-Pb年龄及Hf同位素组成与物源示踪研究[J]. 第四纪研究,2013,33(4):656-670.

He Mengying, Zheng Hongbo, Jia Juntao. Detrital zircon U-Pb dating and Hf isotope of modern sediments in the Yangtze River: Implications for the sediment provenance[J]. Quaternary Sciences, 2013, 33(4): 656-670.
[53] 王伟涛,郑德文,庞建章. 青藏高原东北缘寺口子剖面碎屑锆石示踪及其构造意义[J]. 地质学报,2013,87(10):1551-1569.

Wang Weitao, Zheng Dewen, Pang Jianzhang. Provenancial tracing for the Cenozoic Sikouzi section in the northeastern margin of the Tibetan Plateau and its tectonic implications[J]. Acta Geologica Sinica, 2013, 87(10): 1551-1569.
[54] 丁振举,文成雄,国阿千,等. 西秦岭吴家山群地层时代及物源特征:来自碎屑锆石U-Pb年龄证据[J]. 地球科学与环境学报,2018,40(2):111-132.

Ding Zhenju, Wen Chengxiong, Guo Aqian, et al. Stratigraphic ages and provenance characteristics of Wujiashan Group in west Qinling, China: Evidences from detrital zircon U-Pb age[J]. Journal of Earth Sciences and Environment, 2018, 40(2): 111-132.
[55] 翟明国,彭澎. 华北克拉通古元古代构造事件[J]. 岩石学报,2007,23(11):2665-2682.

Zhai Mingguo, Peng Peng. Paleoproterozoic events in the North China Craton[J]. Acta Petrologica Sinica, 2007, 23(11): 2665-2682.
[56] Sundell K E, Saylor J E. Unmixing detrital geochronology age distributions[J]. Geochemistry, Geophysics, Geosystems, 2017, 18(8): 2872-2886.
[57] Lu Huayu, Yi Shuangwen, Xu Zhiwei, et al. Chinese deserts and sand fields in Last Glacial Maximum and Holocene Optimum[J]. Chinese Science Bulletin, 2013, 58: 2775-2783.
[58] 鹿化煜,安芷生. 黄土高原红黏土与黄土古土壤粒度特征对比:红黏土风成成因的新证据[J]. 沉积学报,1999,17(2):226-232.

Lu Huayu, An Zhisheng. Comparison of grain-size distribution of red clay and loess-paleosol deposits in Chinese Loess Plateau[J]. Acta Sedimentologica Sinica, 1999, 17(2): 226-232.
[59] Gallet S, Jahn B M, Torii M. Geochemical characterization of the Luochuan loess-paleosol sequence, China, and paleoclimatic implications[J]. Chemical Geology, 1996, 133(1/2/3/4): 67-88.
[60] Jiang F C, Fu J L, Wang S B, et al. Formation of the Yellow River, inferred from loess-palaeosol sequence in Mangshan and lacustrine sediments in Sanmen Gorge, China[J]. Quaternary International, 2007, 175(1): 62-70.
[61] Prins M A, Zheng H B, Beets K, et al. Dust supply from river floodplains: The case of the lower Huang He (Yellow River) recorded in a loess-palaeosol sequence from the Mangshan plateau[J]. Journal of Quaternary Science, 2009, 24(1): 75-84.