[1]王 营,高红山*,赵珂梓,等.渭河三阳川盆地最高级阶地的年代厘定及其对河谷发育的指示意义[J].山地学报,2020,(01):1-8.[doi:10.16089/j.cnki.1008-2786.000485]
 WANG Ying,GAO Hongshan*,ZHAO Kezi,et al.Dating of the Highest Terrace of the Weihe River in the Sanyangchuan Basin and Its Implications to Valley Evolution[J].Mountain Research,2020,(01):1-8.[doi:10.16089/j.cnki.1008-2786.000485]
点击复制

渭河三阳川盆地最高级阶地的年代厘定及其对河谷发育的指示意义()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2020年01期
页码:
1-8
栏目:
山地环境
出版日期:
2020-01-30

文章信息/Info

Title:
Dating of the Highest Terrace of the Weihe River in the Sanyangchuan Basin and Its Implications to Valley Evolution
文章编号:
1008-2786-(2020)1-001-08
作者:
王 营1高红山1*赵珂梓1李宗盟2刘芬良3潘保田1
1.兰州大学 资源环境学院 西部环境教育部重点实验室, 甘肃 兰州 730000; 2.信阳师范学院 地理科学学院, 河南 信阳 464000; 3.湖南城市学院 市政与测绘工程学院, 湖南 益阳 413000
Author(s):
WANG Ying1 GAO Hongshan1* ZHAO Kezi1 LI Zongmeng2 LIU Fenliang3 PAN Baotian1
1. Key Laboratory of Western China's Environmental Systems, Ministry of Education, Lanzhou University, Lanzhou 730000, China; 2. School of Geographic Sciences, Xinyang Normal University, Xinyang 464000, Hunan China; 3. School of Municipal and Geomatics Engineering, Hunan City University, Yiyang 413000, Hunan China
关键词:
ESR 26Al/10Be埋藏测年 阶地 河谷发育 三阳川盆地
分类号:
P931.1
DOI:
10.16089/j.cnki.1008-2786.000485
文献标志码:
A
摘要:
青藏高原东缘水系的演化历史长期存在着重大争议,鉴于任一水系的形成演化都是通过主要河谷的发育及其不断延展与整合完成的,因此确定河谷发育的起始时代是研究水系演化的关键。本文针对渭河上游三阳川盆地最高级阶地形成时代的研究,发现李家小湾河流阶地砾石层的ESR年代为1.26±0.15 Ma和1.32±0.19 Ma,26Al/10Be埋藏年代为1.45±0.70 Ma和1.04±0.43 Ma,说明该段河谷形成于早更新世晚期。综合青藏高原东缘夷平面、剥蚀面与河流阶地的研究成果,推断该区现代河谷系列主要形成于1.2 Ma以后,河流平均下切速率较高,为0.1~0.32 m/ka,指示了中更新世以来该区快速的地表抬升与河谷发育过程; 而其前少数地段的先成河谷下切速率介于0.04~0.29 m/ka之间,说明区域地势总体低平,地表过程以剥蚀夷平为主,即高原东缘的现今水系格局主要是第四纪期间构造和气候共同作用下河流侵蚀的产物。

参考文献/References:

[1] WANG Pinxian. Late Cenozoic environmental evolution in China: Marine factors and records[C]//JABLONSKI N G, ed. The changing face of East Asia during the Tertiary and Quaternary. Proceeding of the fourth conference on the evolution of the East Asian environment. Hong Kong: The University of Hong Kong, 1997:263-274.
[2] GLOCK W S. The development of drainage systems:A synoptic view[J]. Geographical Review, 1931, 21(3): 475-482.
[3] CLIFT P D, BLUSZTAJN J. Reorganization of the western Himalayan river system after five million years ago[J]. Nature, 2005, 438:1001-1003.
[4] ZHENG Hongbo, CLIFT P D, WANG Ping, et al. Pre-Miocene birth of the Yangtze river[J]. Proceedings of the National Academy of Sciences of the United States of America, 2013, 110:7556-7561.
[5] 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 Science, 2013, 33(4): 715-722]
[6] LI Jijun. Uplift of Qinghai-Xizang(Tibet)plateau and global change[M]. Lanzhou: Lanzhou University Press, 1995: 191-207.
[7] HU Zhenbo, PAN Baotian, GUO Lianyong, et al. Rapid fluvial incision and headward erosion by the Yellow River along the Jinshaan gorge during the past 1.2 Ma as a result of tectonic extension[J]. Quaternary Science Reviews, 2016, 133:1-14.
[8] 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]
[9] 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]
[10] 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共存论的意义[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,antiquity of Chinese rivers,and coexistence theory of rivers and lakes[J]. Acta Geologica Sinica, 2018, 92(4): 845-886]
[11] CLAPP F G. The hwang Ho,Yellow River[J]. Geographical Review, 1922, 12(1): 1-18.
[12] LIN Aiming, YANG Zhenyu, SUN Zhiming, et al. How and when did the Yellow River develop its square Bend?[J]. Geology, 2001, 29(10): 951-954.
[13] SUN Jimin. Long-term fluvial archives in the Fen Wei Graben,central China,and their bearing on the tectonic history of the India-Asia collision system during the Quaternary[J]. Quaternary Science Reviews, 2005, 24(10/11): 1279-1286.
[14] GAO Hongshan, LI Zongmeng, JI Yapeng, et al. Climatic and tectonic controls on strath terraces along the upper Weihe River in central China[J]. Quaternary Research, 2016, 86(3): 326-334.
[15] 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(7): 657-664.
[16] 陈云,童国榜,曹家栋,等.渭河宝鸡段河谷地貌的构造气候响应[J].地质力学学报,1999,5(4): 51-58.[CHEN Yun, TONG Guobang, CAO Jiadong, et al. Tectonic climate response in the geomorphology of the Weihe River valley around Baoji,Shaanxi Province[J]. Journal of Geomechanics, 1999, 5(4):51-58]
[17] GAO Hongshan, LI Zongmeng, LIU Xiaofeng, et al. Fluvial terraces and their implications for Weihe River valley evolution in the Sanyangchuan Basin[J]. Science China Earth Sciences, 2017, 60(3): 413-427.
[18] 王志才,张培震,张广良,等.西秦岭北缘构造带的新生代构造活动——兼论对青藏高原东北缘形成过程的指示意义[J].地学前缘,2006,13(4):119-135.[WANG Zhicai, ZHANG Peizhen, ZHANG Guangliang, et al. Tertiary tectonic activities of the North frontal fault zone of the West Qinling mountains:implications for the growth of the northeastern margin of the Qinghai-Tibetan Plateau[J]. Earth Science Frontiers, 2006, 13(4): 119-135]
[19] 薛祥煦,张云翔.从生物化石的性质和分布分析秦岭上升的阶段性与幅度[J].地质论评,1996,42(1):30-36.[XUE Xiangxu, ZHANG Yunxiang. The uplift stages and amplitudes of the Qinling Mountains by analying the distribution and character of the fossils found in the mountains[J]. Geological Review, 1996, 42(1): 30-36]
[20] 王营.渭河三阳川盆地阶地序列的ESR和宇生核素~(26)Al/~(10)Be埋藏年代学研究[D].兰州:兰州大学,2019:22-29.[WANG Ying. ESR and cosmogenic nuclides 26Al/10Be burial dating of terrace sequence in the Sanyangchuan Basin of the Weihe River[D]. Lanzhou: Lanzhou University, 2019: 22-29]
[21] YOKOYAMA Y, FALGURES C, QUAEGEBEUR J P. ESR dating of quartz from quaternary sediments:First attempt[J]. Nuclear Tracks&Radiation Measurements, 1985, 10(4/6): 921-928.
[22] GRANGER D E, MUZIKAR P F. Dating sediment burial with in situ-produced cosmogenic nuclides:theory, techniques, and limitations[J]. Earth and Planetary Science Letters, 2001, 188(1): 269-281.
[23] SCHUMM S A, ETHRIDGE F G. Origin, evolution, and morphology of fluvial valleys[C]//DALRYMPLE R W, BOYD R, ZAITLIN B A, ed. Incised-valley systems: origin and sedimentary sequences. Society of Economic Paleontologists and Mineralogists, Special Publication, Tulsa,Oklahoma, 1994,51:11-27.
[24] PAN Baotian, GAO Hongshan, WU Guangjian, et al. Dating of erosion surface and terraces in the eastern Qilian Shan,northwest China[J]. Earth Surface Processes and Landforms, 2007, 32(1): 143-154
[25] 潘保田,高红山,李炳元,等.青藏高原层状地貌与高原隆升[J].第四纪研究,2004,24(1): 50-57+133.[PAN Baotian, GAO Hongshan, LI Bingyuan, et al. Step-like landforms and uplift of the Qinghai-Xizang Plateau[J]. Quaternary Science, 2004, 24(1): 50-57+133]
[26] BUCHER W H. "Strath"as a geomorphic term[J]. Science, 1932, 75(1935): 130-131.
[27] 李吉均,方小敏,潘保田,等.新生代晚期青藏高原强烈隆起及其对周边环境的影响[J].第四纪研究,2001,21(5):381-391.[LI Jijun, FANG Xiaomin, PAN Baotian, et al. Late cenozoic intensive uplift of Qinghai-Xizang plateau and its impacts on environments in surrounding area[J]. Quaternary Science, 2001, 21(5): 381-391]
[28] 齐矗华,甘枝茂,惠振德.陕西东秦岭构造地貌基本特征[J].陕西师范大学学报(自然科学版),1982,10(0): 180-193.[QI Chuhua, GAN Zhimao, XI Zhende. The main characteristics of the structure geomorphology of East Qinling in Shaanxi[J]. Journal of Shaanxi Normal University(Natural Science Edition), 1982, 10(0): 180-193]
[29] 吴忱,张秀清,王然,等.华北山地夷平面研究[J].地理与地理信息科学,2017,33(1): 124-127.[WU Chen, ZHANG Xiuqing, WANG Ran, et al. Study on planation surface in North China[J]. Geography and Geo-Information Science, 2017, 33(1): 124-127]
[30] LI Jijun, MA Zhenhua, LI Xiaomiao, et al. Late Miocene-Pliocene geomorphological evolution of the xiaoshuizi peneplain in the maxian mountains and its tectonic significance for the northeastern tibetan plateau[J]. Geomorphology, 2017, 295:393-405.
[31] XIONG Jiangou, LI Youli, ZHONG Yuezhi, et al. Paleomagnetic age of the Tangxian planation surface,northwestern Zhongtiao Shan of the Shanxi Graben System,North China[J]. Geomorphology, 2017, 283:17-31.
[32] LIU Fenliang, GAO Hongshan, PAN Baotian, et al. Quantitative analysis of planation surfaces of the upper Yangtze River in the Sichuan-Yunnan Region,Southwest China[J]. Frontiers of Earth Science, 2019, 13(1): 55-74.
[33] LI Jijun, XIE Siyou, KUANG Mingsheng. Geomorphic evolution of the Yangtze Gorges and the time of their formation[J]. Geomorphology, 2001, 41(2/3): 125-135.
[34] 朱俊杰,钟巍,李吉均,等.陇西盆地最老的风成黄土沉积——兰州烟洞沟剖面[J].地理科学,1996,16(4):365-369.[ZHU Junjie, ZHONG Wei, LI Jijun, et al. The oldest eolian loess deposition in Longxi Basin-Yandonggou profile in Lanzhou[J]. Scientia Geographica Sinica, 1996, 16(4): 365-369]
[35] YANG Dong, FANG Xiaomin, LU Lianqing, et al. Development of a pediment on western slopes of Liupan Mountain related to the Neotectonic Uplift[J]. Chinese Science Bulletin, 2001, 46(1): 11-15.
[36] 邢成起,尹功明,丁国瑜,等.黄河黑山峡阶地的砾石Ca膜厚度与粗碎屑沉积地貌面形成年代的测定[J].科学通报,2002,47(3):167-172.[XING Chengqi, YIN Gongming, DING Guoyu, et al. Thickness of Calcium carbonate coats on stones of the Heishanxia terraces of the Yellow River and dating of coarse clastic sedimentary geomorphic surfaces[J]. Chinese Science Bulletin, 2002, 47(3): 167-172]
[37] 张珂,蔡剑波.黄河黑山峡口最高阶地宇宙核素的初步年龄及所反映的新构造运动[J].第四纪研究,2006,26(1):85-91.[ZHANG Ke, CAI Jianbo. Preliminary result of the dating by TCN technique of the highest terrace of the Heishanxia gorge mouth,Northeast margin of Tinetan Plateau and its expression of neotectonic movement in that area[J]. Quaternary Science, 2006, 26(1): 85-91]
[38] 国家地震局.鄂尔多斯周缘活动断裂系[M].北京:地震出版社,1988:114-142.[GUO Jiadezhenju. Active fault system around ordos massif[M]. Beijing: Earthquake Press, 1988: 114-142]
[39] 高红山,潘保田,李吉均,等.祁连山东段金塔河流域层状地貌时代与成因探讨[J].山地学报,2005,23(2):129-135.[GAO Hongshan, PAN Baotian, LI Jijun, et al. Age and Genesis of the stepped geomorphic surfaces in jinta river basin of the eastern qilian mountains[J]. Mountain Research, 2005, 23(2): 129-135]
[40] ZHANG Huiping, ZHANG Peizhen, CHAMPAGNAC J D, et al. Pleistocene drainage reorganization driven by the isostatic response to deep incision into the northeastern Tibetan Plateau[J]. Geology, 2014, 42(4): 303-306.
[41] 鹿化煜,安芷生,王晓勇,等.最近14Ma青藏高原东北缘阶段性隆升的地貌证据[J].中国科学D辑:地球科学,2004,34(9): 855-857+856.[LU Huayu, AN Zhisheng, WANG Xiaoyong, et al. Geomorphologic evidence of phased uplift of the northeastern Qinghai-Tibet Plateau since 14 million years ago[J]. Science China Earth Sciences, 2004, 34(9): 855-857+856]
[42] 刘芬良.晚新生代金沙江下游段地貌演化与河谷发育研究[D].兰州:兰州大学,2018:76-90.[LIU Fenliang. Geomorphological evolution and Valley development of the Lower Jinsha River during Late Cenozoic[D]. Lanzhou: Lanzhou University, 2018:76-90]
[43] 赵志军,刘勇,陈晔,等.基于ESR年代的川西高原河流下切速率[J].兰州大学学报(自然科学版),2013,49(2): 160-165+172.[ZHAO Zhijun, LIU Yong, CHEN Ye, et al. Quaternary fluvial incision rates of the Western Sichuan Plateau inferred from ESR chronology[J]. Journal of Lanzhou University(Natural Sciences), 2013, 49(2): 160-165+172]
[44] HE Zexin, ZHANG Xujiao, BAO Shuyan, et al. Multiple climatic cycles imprinted on regional uplift-controlled fluvial terraces in the lower Yalong River and Anning River,SE Tibetan Plateau[J]. Geomorphology, 2015, 250:95-112.
[45] LI Jijun, FANG Xiaomin, ROB V D, et al. Magnetostratigraphic dating of river terraces:Rapid and intermittent incision by the Yellow River of the northeastern margin of the Tibetan Plateau during the Quaternary[J]. Journal of Geophysical Research-Solid Earth, 1997, 1021(B5): 10121-10132.
[46] PAN Baotian, SU Huai, HU Zhenbo, et al. Evaluating the role of climate and tectonics during non-steady incision of the Yellow River:evidence from a 1.24 Ma terrace record near Lanzhou,China[J]. Quaternary Science Reviews, 2009, 28(27): 3281-3290.

备注/Memo

备注/Memo:
收稿日期(Received date):2018-11-14; 改回日期(Accepted date):2019-11-25
基金项目(Foundation item):国家自然科学基金面上项目(41471008); 国家自然科学基金重点项目(41730637)。[National Natural Science Foundation of China(41471008, 41730637)]
作者简介(Biography):王营(1992-),女,河南三门峡人,硕士,主要研究方向:流域地貌演化。[WANG Ying(1992-), female, born in Sanmenxia, Henan province, M.Sc., research on drainage basin geomorphic evolvement] E-mail: 1347026637@qq.com
*通讯作者(Corresponding author):高红山(1977-),男,博士,教授,主要研究方向:流域地貌演化与河流过程。[GAO Hongshan(1977-), male, Ph.D., professor, research on drainage basin geomorphic evolvement and river process] E-mail: gaohsh@lzu.edu.cn
更新日期/Last Update: 2020-01-30