[1]张信宝,代 彬.碎屑锆石U-Pb年龄谱物源示踪技术确定黄河贯通时间的质疑[J].山地学报,2022,(5):637-647.[doi:10.16089/j.cnki.1008-2786.000699]
　ZHANG Xinbao,DAI Bin,et al.A Query on the Determination of the Cutting-Through Period of the Yellow River of China by the Tracing Technique of U-Pb Age Spectrum of Detrital Zircons[J].Mountain Research,2022,(5):637-647.[doi:10.16089/j.cnki.1008-2786.000699]
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碎屑锆石U-Pb年龄谱物源示踪技术确定黄河贯通时间的质疑
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2022年第5期
页码:
637-647
栏目:
专家观点
出版日期:
2022-11-20

文章信息/Info

Title:
A Query on the Determination of the Cutting-Through Period of the Yellow River of China by the Tracing Technique of U-Pb Age Spectrum of Detrital Zircons
文章编号:
1008-2786-(2022)5-637-11
作者:
张信宝1; 3; 代 彬2; 3
(1. 中国科学院、水利部成都山地灾害与环境研究所 山地环境演变与调控重点实验室,成都 610041; 2. 中国科学院地球化学研究所 环境地球化学国家重点实验室,贵阳 550081; 3. 中国科学院普定喀斯特生态系统观测研究站,贵州 普定 562100)
Author(s):
ZHANG Xinbao1;  3;  DAI Bin2;  3
(1. Key Laboratory of Mountain Environment Evolution and Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China; 2. State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China; 3. Puding Karst Ecosystem Observation Research Station, Chinese Academy of Sciences, Puding 562100, Guizhou, China)
关键词:
碎屑锆石U-Pb年龄谱;  物源示踪技术;  黄河
Keywords:
U-Pb detrital zircon geochronology;  tracing technology;  the Yellow River
分类号:
K928.42
DOI:
10.16089/j.cnki.1008-2786.000699
文献标志码:
A
摘要:
黄河贯通时间一直是地学研究者关注的热点问题,但未能形成共识。本文在阐明新近纪以来黄河中游及邻区古湖消亡及水系贯通过程的基础上,剖析了运用碎屑锆石U-Pb年龄谱物源示踪技术约束黄河贯通时间4个案例研究所存在的问题。三门湖泥岩中的钙结核和钙质层表明,0.3 Ma前该湖为咸水-半咸水内流湖,三门峡一带的黄河沿岸阶地是古湖的湖滨或河流阶地,三门湖沉积物源于当地河流,黄河上游与中游贯通发生于1.3 Ma～1.5 Ma,和～5 Ma前的结论不能成立。华北平原现黄河入海口附近钻孔沉积物源于燕山和太行山的河流,根据碎屑锆石U-Pb年龄谱得出的1.5 Ma～1.6 Ma黄河贯通的结论不成立。黄土是黄河泥沙的主要来源,黄土中碎屑锆石U-Pb年龄谱比较复杂,增加了运用这一技术约束黄河贯通时间的不确定性。
Abstract:
Although the cutting-through period of the Yellow River of China has always been a hot issue for geoscience researchers, no consensus had been reached. In this study, we elucidated the extinction of ancient lakes and the penetrating process of the middle reaches of the Yellow River and its adjacent areas since Neogene; then the issues in four case studies was picked up for examination of the use of tracing technology of U-Pb detrital zircon geochronology, which were used in four case studies for rebuilding the cutting-through period of the Yellow River in the middle reach. As reported in the referred case studies, there were calcium nodules and calcareous layers to be formed in the mudstone of the Sanmen Lake, indicating it is an endorheic lake of saltwater-brackish water before 0.3 Ma; the terraces along the Yellow River in the Sanmen Gorges were lakeside of the ancient lake or river terraces. Therefore, the sediments of the Sanmen lake originated from local rivers other than the later Yellow River. The conclusion that the Yellow River united the upper reaches with the middle reaches occurred at 1.3 Ma～1.5 Ma or ～5 Ma cannot be established. Also as justified in the aforesaid cases, the borehole sediments near the present mouth of the Yellow River in the North China Plain originated from the rivers of the Yanshan Mountains as well as the Taihang Mountains; consequently, the advocated conclusion that the Yellow River run through in the upper and middle reach at 1.5 Ma～1.6 Ma in terms of the U-Pb age spectrum of detrital zircons is not convincing.In conclusion, loess is primary source of sediments in the Yellow River. The age spectrum of U-Pb detrital zircon in loess is too complicated for application, which increases the uncertainty about using U-Pb detrital zircon age spectrum to determine the period of channel connection of the Yellow River.

参考文献/References:

[1] 潘保田, 胡振波,胡小飞,等. 晋陕峡谷北段晚新生代河流演化初步研究[J]. 第四纪研究,2012, 32(1):111-121. [PAN Baotian,HU Zhenbo,Hu Xiaofei,et al. Time-slice of the fluvial evolution in the northern Jinshaan Gorge during Late Cenozoic [J]. Quaternary Sciences, 2012, 32(1):111-121] DOI: 10.3969/j.issn.1001-7410.2012.01.12
[2] 张抗. 黄河中游水系形成史初探[J]. 第四纪研究, 1989(8):185-193. [ZHANG Kang. Liminary study on the formation of hydrographic net along the middle reaches of the Huanghe(Yellow)River [J]. Quaternary Sciences, 1989(8):185-193]
[3] 王书兵,蒋复初,傅建利,等. 关于黄河形成时代的一些认识[J]. 第四纪研究,2013,33(4):705-714. [WANG Shubing, JIANG Fuchu, FU Jianli, et al. Some knowledge of the formation of the Yellow River [J]. Quaternary Sciences, 2013,33(4):705-714] DOI: 10.3969/j.issn.1001-7410.2013.04.08
[4] 赵希涛,贾丽云,胡道功. 内蒙河套地区黄河阶地与新近纪砾石层的发现及其对黄河发育、中国河流古老性与河湖并存论的意义[J]. 地质学报,2018, 92(4):845-886. [ZHAO Xitao, JIA Liyun, HU Daogong. Discoveries of fluvial terraces and Neogene gravels in the Hetao area, Inner Mongolia: Implications for the development of the Yellow River, the antiquity of Chinese rivers, and coexistence theory of rivers and lakes [J]. Acta Geologica Sinica, 2018,92(4):845-886] DOI: 10.3969/j.issn.0001-5717.2018.04.013
[5] 袁宝印,汤国安,周力平,等. 新生代构造运动对黄土高原地貌分异与黄河形成的控制作用[J]. 第四纪研究,2012,32(5):829-838. [YUAN Baoyin, TANG Guoan, ZHOU Liping, et al. Control action on the geomorphic differentiation in Loess Plateau and the formation of Yellow River by Cenozoic tectogenesis [J]. Quaternary Sciences, 2012,32(5):829-838] DOI: 10.3969/j.issn.1001-7410.2012.05.01
[6] 程绍平,邓起东,闵伟,等. 黄河晋陕峡谷河流阶地和鄂尔多斯高原第四纪构造活动[J]. 第四纪研究,1998(3):238-248. [CHENG Shaoping, DENG Qidong, MIN Wei, et al. Yellow River and Quaternary tectonic movements of the Ordos Plateau [J]. Quaternary Sciences, 1998(3):238-248] DOI: 10.1088/0256-307X/16/9/027
[7] 王小燕, 邱维理, 张家富, 等. 晋陕峡谷北段保德—府谷地区唐县面上冲积物的特征及其地貌意义[J]. 第四纪研究, 2013, 33(4):715-722. [WANG Xiaoyan, QIU Weili, ZHANG Jiafu, et al. Features of the alluvium on Tangxian surface near Baode-Fugu and its geomorphologic implications in the northern Jinshaan gorge, Yellow River [J]. Quaternary Sciences, 2013, 33(4):715-722] DOI: 10.3969/j.issn.1001-7410.2013.04.09
[8] 张珂. 河流的竞争——以汾河与晋陕黄河形成演化为例[J]. 第四纪研究, 2012,32(5): 859-865. [ZHANG Ke. Fluvial competition: Exemplified by formation and evolution of the Fen River and JinshanYellow River [J]. Quaternary Sciences, 2012,32(5):859-865] DOI: 10.3969/j.issn.1001-7410.2012.05.04
[9] 聂宗笙. 内蒙古河套盆地晚更新世地层划分、环境演变及黄河的贯通[J]. 地学前缘, 2019,26(4):259-272. [NIE Zongsheng. Stratigraphic division of the Upper Pleistocene, environmental change and formation of the Yellow River in the Hetao Basin, Inner Mongolia [J]. Earth Science Frontiers, 2019, 26(4):259-272] DOI: 10.13745/j.esf.sf.2019.5.7
[10] HU Zhenbo, LI Menghao, DONG Zijuan, et al. Fluvial entrenchment and integration of the Sanmen Gorge, the Lower Yellow River [J]. Global and Planetary Change, 2019, 178:129-138. DOI: 10.1016/j.gloplacha.2019.04.010
[11] 傅建利, 张珂, 马占武,等. 中更新世晚期以来高阶地发育与中游黄河贯通[J]. 地学前缘, 2013, 20(4):166-181. [FU Jianli,ZHANG Ke,MA Zhanwu, et al. The terrace(T5 and T4)formation since the late Middle Pleistocene and its implication in the through cutting of the middle reach of Yellow River [J]. Earth Science Frontiers, 2013,20(4):166-181]
[12] 张信宝,刘彧,王世杰, 等. 黄河、长江的形成演化及贯通时间[J]. 山地学报,2018,36(5):661-668. [ZHANG Xinbao,LIU Yu,WANG Shijie, et al. On the chronology of the Yellow Rivers and the Yangtze Rivers [J]. Mountain Research,2018,36(5):661-668] DOI: 10.16089/j.cnki.1008-2786.000362
[13] 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(D辑),2001,31(9):760-768. [WANG Sumin,WU Xihao,ZHANG Zhengke,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 in China(Series D),2001,31(9):760-768] DOI: 10.3969/j.issn.1674-7240.2001.09.008
[14] 戴英生. 黄河的形成与发育简史[J].人民黄河,1983(2):1-7. [DAI Yingsheng. Brief history of formation and evolution of Yellow River [J]. Yellow River,1983(2): 1-7]
[15] 潘保田,王均平,高红山,等. 河南扣马黄河最高级阶地古地磁年代及其对黄河贯通时代的指示[J].科学通报,2005,50(3):255-261. [PAN Baotian,WANG Junping,GAO Hongshan, et al. Paleomagnetic dating of the topmost terrace in Kouma,Henan and its indication to the Yellow River’s running through Sanmen Gorges [J]. Chinese Science Bulletin,2005,50(3):255-261] DOI: 10.3321/j.issn:0023-074X.2005.03.010
[16] 刘书丹,李广坤,李玉信,等. 从河南东部平原第四纪沉积物特征探讨黄河的形成与演变[J].河南地质,1988,6(2):20-24. [LIU Shudan,LI Guangkun,LI Yuxin,et al. The formation and evolution of the Yellow River from Quaternary sediments in the eastern plain of Henan province [J]. Henan Geology,1988,6(2):20-24]
[17] HU Zhenbo, PAN Baotian, BRIDGLAND D, et al. The linking of the upper-middle and lower reaches of the Yellow River as a result of fluvial entrenchment [J]. 2017,166(2):324-338. DOI: 10.1016/j.quascirev.2017.02.026
[18] 魏荣珠, 王权, 庄其天, 等. 黄河中游及邻区晚新生代地层特征及地表过程讨论[J]. 第四纪研究, 2022, 42(3):823-842. [WEI Rongzhu, WANG Quan, ZHUANG Qitian, et al. Discussion on Late Cenozoic stratigraphic features and earth surface processes in the middle reaches of the Yellow River and its adjacent regions [J]. Quaternary Sciences, 2022, 42(3): 823-842] DOI: 10.11928/j.issn.1001-7410.2022.03.16
[19] KONG Ping, JIA Jun, ZHENG Yong. Time constraints for the Yellow River traversing the Sanmen Gorge [J]. Geochemistry Geophysics Geosystems, 2014,15(2):395-407. DOI: 10.1002/2013GC004912
[20] ZHANG Hanzhi, LU Huayu, ZHOU Yali,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(15):110072. DOI: 10.1016/j.palaeo.2020.110072
[21] XIAO Guoqiao, SUN Yuqi, YANG Jilong,et al. Early Pleistocene integration of the Yellow River I: Detrital-zircon evidence from the North China Plain [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2020, 546:109691. DOI: 10.1016/j.palaeo.2020.109691
[22] YANG Jilong, YUAN Haifan, HU Yunzhuang, et al. Significance of sedimentary provenance reconstruction based on borehole records of the North China Plain for the evolution of the Yellow River [J]. Geomorphology, 2022, 401:108077. DOI: 10.1016/j.geomorph.2021.108077
[23] WANG Xin, HU Gang, SAITO Y, et al. Did the modern Yellow River form at the Mid-Pleistocene transition? [J]. Science Bulletin, 2022,67:1603-1610. DOI: 10.1016/j.scib.2022.06.003
[24] NIE Junsheng, STEVENS T, RITTNER M, et al. Loess Plateau storage of Northeastern Tibetan Plateau-derived Yellow River sediment [J]. Nature Communication, 2015,6:8511. DOI: 10.1038/ncomms9511(2015)
[25] 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. DOI: 10.1130/G32296.1
[26] 马丽芳. 中国地质图集[M]. 北京: 地质出版社, 2007. [MA Lifang. Geological atlas of China [M]. Beijing: Geology Press, 2007]
[27] XIONG Jianguo, LIU Yunming, ZHANG Peizhen, et al. Entrenchment of the Yellow River since the late Miocene under changing tectonics and climate [J]. Geomorphology, 2022, 416:108428. DOI: 10.1016/j.geomorph.2022.108428

备注/Memo

备注/Memo:
收稿日期(Received date):2022-09-20; 改回日期(Accepted date):2022-10-20
基金项目(Foundation item): 国家自然科学基金(91747207)。[National Natural Science Foundation of China(91747207)]
作者简介(Biography): 张信宝(1946-),男,二级研究员,主要研究方向:土壤侵蚀与水土保持。[ZHANG Xinbao(1946-), professor, male, research on soil erosion, soil and water conservation] E-mail:zxbao@imde.ac.cn
更新日期/Last Update: 2022-10-30