Terrace sequences and its evolution since the Late Pleistocene in Bier River of Daliang Mountain area
YIN Zhiqiang1, QU Tianyue2, PANG Mingfei1,3, SHAO Hai1, DING Yi1
1. China Institute of Geo-environment Monitoring, Beijing 100081, China; 2. Texas A&M University, College Station, Texas 77840, America; 3. China University of Geosciences (Wuhan), Hubei Wuhan 430074, China
摘要河流阶地详细记录了区域构造活动和地貌演化信息,可为第四纪地貌阶段性隆升提供证据。位于四川大凉山区的昭觉河流域及其支流地处青藏高原东南部,横断山脉与四川盆地西南缘的过渡带,发育了河流阶地等层状地貌。以昭觉河的支流比尔河为研究对象,通过野外河流阶地级序及阶地沉积物调查,结合14C测年结果,厘定了比尔河的3级河流阶地,其中T2和T3为基座阶地,T1为堆积阶地,形成时间为27.75 ka B.P.、12.20 ka B.P.以及6.65 ka B.P.,其中T3阶地与T2阶地的河流下切速率分别为0.59~1.29 mm/a和1.26~4.50 mm/a。认为川西大凉山地区30 000 a以来地貌至少经历了2次间歇性抬升,在整体隆升过程中,河流上游较中下游的地壳抬升速度更快,具有掀斜式抬升特征。T3、T2、T1阶地的形成与研究区气候变化有一定相关性,但新构造运动是比尔河河流阶地形成的主导因素,这对了解川西地区晚更新世以来河流阶地的级序展布及演化具有重要意义。
Abstract:The detailed information of regional active structures and geomorphic evolution were recorded by river terraces, which can provide evidence for the phased uplift of the Quaternary geomorphology. Zhaojue River Basin and its tributaries in Daliang Mountain of Sichuan Province are located in the transitional zone between Hengduan Mountains in the southeast of Qinghai-Tibet Plateau and the southwestern edge of Sichuan Basin, with the development of many river terraces and other layered landforms. The authors took a tributary of Zhaojue River- Bier River in the area as a case study to identify the three river terraces of Bier River, through the investigation of the terrace sequences, river alluvial sediments and 14C dating results. The T2 and T3 are the rock-seated terraces and T1 is a constructional terrace, with formation times of 27.75 ka B.P., 12.20 ka B.P., and 6.65 ka B.P.. The river incision rates of T3 and T2 are 0.59-1.29 mm/a and 1.26-4.50 mm/a respectively. The landform in the Daliangshan area of Western Sichuan has experienced at least two intermittent uplifts in the past 30 000 years, and the crustal uplift rate in the upper reaches of the river is faster than that in the middle and lower reaches of the river during the overall uplift process, with characteristics of tilting uplift. The terraces formation of T3, T2 and T1 has a certain correlation with the climate change in the study area, but the neotectonic activity is the dominant factor in the terraces formation of Bier River, which is of great significance for the river terraces sequence distribution and evolution in Western Sichuan since the Late Pleistocene.
殷志强, 屈天月, 庞明非, 邵海, 丁一. 大凉山区比尔河晚更新世以来阶地级序及其演化[J]. 中国地质调查, 2023, 10(2): 64-71.
YIN Zhiqiang, QU Tianyue, PANG Mingfei, SHAO Hai, DING Yi. Terrace sequences and its evolution since the Late Pleistocene in Bier River of Daliang Mountain area. , 2023, 10(2): 64-71.
[1] Gong Z J,Li S H,Li B.The evolution of a terrace sequence along the Manas River in the northern foreland basin of Tian Shan,China,as inferred from optical dating[J].Geomorphology,2014,213:201-212. [2] Vandenberghe J.River terraces as a response to climatic forcing:Formation processes,sedimentary characteristics and sites for human occupation[J].Quat Int,2015,370:3-11. [3] Zhang J F,Qiu W L,Wang X Q,et al.Optical dating of a hyperconcentrated flow deposit on a Yellow River terrace in Hukou,Shaanxi,China[J].Quat Geochronol,2010,5(2/3):194-199. [4] 吴环环,吴学文,李玥,等.黄河共和—贵德段河流阶地对青藏高原东北缘晚期隆升的指示[J].地质学报,2019,93(12):3239-3248. Wu H H,Wu X W,Li Y,et al.River terraces in the Gonghe-Guide section of the Yellow River:Implications for the late uplift of the northeastern margin of the Qinghai-Tibet Plateau[J].Acta Geol Sin,2019,93(12):3239-3248. [5] Erkens G,Dambeck R,Volleberg K P,et al.Fluvial terrace formation in the northern Upper Rhine Graben during the last 20 000 years as a result of allogenic controls and autogenic evolution[J].Geomorphology,2009,103(3):476-495. [6] 于航,步凡,胡道功,等.祁连山大通河河流阶地形成时代及地质意义[J].中国地质调查,2018,5(3):43-48. Yu H,Bu F,Hu D G,et al.Ages and geological significance of the river terrace of Datong River in Qilian Mountains[J].Geol Surv China,2018,5(3):43-48. [7] Stokes M,Cunha P P,Martins A A.Techniques for analysing Late Cenozoic river terrace sequences[J].Geomorphology,2012,165-166:1-6. [8] Wang X Z,Chun X,Zhou H J,et al.Application of standardised growth curves in quartz OSL dating of lacustrine sediments on the Mongolian Plateau[J].Quat Int,2021,592:51-59. [9] 张克旗,吴中海,吕同艳,等.光释光测年法——综述及进展[J].地质通报,2015,34(1):183-203. Zhang K Q,Wu Z H,Lv T Y,et al.Review and progress of OSL dating[J].Geol Bull China,2015,34(1):183-203. [10] Méndez-Quintas E,Santonja M,Pérez-González A,et al.A multidisciplinary overview of the lower Miño River terrace system (NW Iberian Peninsula)[J].Quat Int,2020,566-567:57-77. [11] Guo X H,Forman S L,Marin L,et al.Assessing tectonic and climatic controls for Late Quaternary fluvial terraces in Guide,Jianzha,and Xunhua Basins along the Yellow River on the northeastern Tibetan Plateau[J].Quat Sci Rev,2018,195:109-121. [12] Gao H S,Liu X F,Pan B T,et al.Stream response to Quaternary tectonic and climatic change:Evidence from the upper Weihe River,central China[J].Quat Int,2007,186(1):123-131. [13] Olszak J,Alexanderson H.Post-IR IRSL dating the oldest (?) river terrace sediments in the Polish Outer Carpathians:Insights into the landscape evolution[J].Geomorphology,2020,371:107436. [14] 王迎国,常宏,周卫健.渭河盆地河流阶地演化及其构造-气候意义[J].地质论评,2021,67(4):1033-1049. Wang Y G,Chang H,Zhou W J.Fluvial terrace evolution and its tectonic-climatic significance in the Weihe Basin[J].Geol Rev,2021,67(4):1033-1049. [15] Singh A K,Pattanaik J K,Gagan,et al.Late Quaternary evolution of Tista River terraces in Darjeeling-Sikkim-Tibet wedge:Implications to climate and tectonics[J].Quat Int,2017,443:132-142. [16] 刘海金,龚志军,罗明,等.沉积物含水量及误差变化对光释光测年精度的影响研究[J].第四纪研究,2021,41(1):123-135. Liu H J,Gong Z J,Luo M,et al.Study the effect of water content and its error on the precision of optical age results for sediments[J].Quat Sci,2021,41(1):123-135. [17] Singh A K,Pattanaik J K,Gagan,et al.Late Quaternary evolution of Tista River terraces in Darjeeling-Sikkim-Tibet wedge:Implications to climate and tectonics[J].Quat Int,2017,443:132-142. [18] Jia L Y,Hu D G,Wu H H,et al.Yellow River terrace sequences of the Gonghe-Guide section in the northeastern Qinghai-Tibet:Implications for plateau uplift[J].Geomorphology,2017,295:323-336. [19] He Z X,Zhang X J,Bao S Y,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. [20] 蒋玺,陈文奇,宁凡,等.贵州高原北部河流阶地发育与喀斯特地貌演化[J].地理研究,2021,40(1):81-92. Jiang X,Chen W Q,Ning F,et al.River terraces in the northern Guizhou Plateau and their implications for karst landform evolution[J].Geogr Res,2021,40(1):81-92. [21] 殷志强,孙东,张瑛,等.美姑河流域滑坡时空展布及成生机制研究[J].第四纪研究,2018,38(6):1358-1368. Yin Z Q,Sun D,Zhang Y,et al.Study on spatial-temporal distribution characteristics and forming mechanism of landslides in the Meigu River basin[J].Quat Sci,2018,38(6):1358-1368. [22] 殷志强,孙东,魏昌利,等.美姑河流域地质灾害与防灾减灾研究[M].北京:科学出版社,2018. Yin Z Q,Sun D,Wei C L,et al.Study on Geological Hazards and Disaster Prevention and Reduction in Meigu River Basin[M].Beijing:Science Press,2018. [23] 殷志强,邵海,马娟,等.金沙江支流美姑河流域地质灾害调查成果报告[R].北京:中国地质环境监测院,2017. Yin Z Q,Shao H,Ma J,et al.Report on geological hazard investigation results of Meigu River Basin,a tributary of Jinsha River[R].Beijing:China Institute of Geo-environment Monitoring,2017. [24] 胡云鹏,邵海,冯文凯,等.四川美姑洛高依达流域泥石流灾害分析[J].中国地质灾害与防治学报,2017,28(1):67-74. Hu Y P,Shao H,Feng W K,et al.Analysis on the debris flow ha-zard of Luogaoyida gully in Meigu county of Sichuan Pro-vince[J].Chin J Geol Hazard Control,2017,28(1):67-74. [25] 马吉福,殷志强,魏刚,等.黄河上游贵德盆地二连村泥流堆积扇发育过程分析[J].水文地质工程地质,2016,43(4):78-83. Ma J F,Yin Z Q,Wei G,et al.An analysis of the developmental process of the Erlian mud flow fans in the eastern Guide Basin in the upper reaches of the Yellow River[J].Hydrogeol Eng Geol,2016,43(4):78-83. [26] 赵希涛,张永双,曲永新,等.玉龙山西麓更新世冰川作用及其与金沙江河谷发育的关系[J].第四纪研究,2007,27(1):35-44. Zhao X T,Zhang Y S,Qu Y X,et al.Pleistocene glaciations along the Western foot of the Yulong Mountains and their relationship with the formation and development of the Jinsha River[J].Quat Sci,2007,27(1):35-44. [27] 唐川,黄润秋,黄达,等.金沙江美姑河牛牛坝水电站库区泥石流对工程影响分析[J].工程地质学报,2006,14(2):145-151. Tang C,Huang R Q,Huang D,et al.Impacts of debris flows on the reservoir of a Hydropower station in the Meigu River of Jinshajiang[J].J Eng Geol,2006,14(2):145-151. [28] Heaton T J,Köhler P,Butzin M,et al.Marine20-the marine radiocarbon age calibration curve (0~55,000 cal BP)[J].Radiocarbon,2020,62(4):779-820. [29] 崔杰. 美姑河坪头电站岸坡特殊地质现象与地下工程[D].成都:成都理工大学,2009:95-106. Cui J.Special Geological Environment of Bank Slope and Underground Engineering about Pingtou Hydroelectric Station of Meigu River[D].Chengdu:Chengdu University of Technology,2009:95-106. [30] Stinchcomb G E,Driese S G,Nordt L C,et al.A mid to late Holo-cene history of floodplain and terrace reworking along the middle Delaware River valley,USA[J].Geomorphology,2012,169-170:123-141. [31] Sridhar A,Chamyal L S,Bhattacharjee F,et al.Early Holocene fluvial activity from the sedimentology and palaeohydrology of gravel terrace in the semi arid Mahi River Basin,India[J].J Asian Earth Sci,2013,66:240-248. [32] 许刘兵,周尚哲.河流阶地形成过程及其驱动机制再研究[J].地理科学,2007,27(5):672-677. Xu L B,Zhou S Z.Formation process and driving mechanisms of fluvial terrace[J].Sci Geogr Sin,2007,27(5):672-677. [33] 姚檀栋,Thompson L G,施雅风,等.古里雅冰芯中末次间冰期以来气候变化记录研究[J].中国科学(D辑),1997,27(5):447-452. Yao T D,Thompson L G,Shi Y F,et al.Abrupt climatic changes on the Tibetan Plateau during the Last Ice Age[J].Sci China (Ser D),1997,27(5):447-452. [34] Starkel L.Climatically controlled terraces in uplifting mountain areas[J].Quat Sci Rev,2003,22(20):2189-2198.