Discussion on the eco-geo-environment effects of Neotectonic activities: A case study of Xichang City in western Yangtze block
LIU Hong1,2, HUANG Hanxiao1, OUYANG Yuan1, LI Wenchang1, ZHANG Jinghua1, ZHANG Tengjiao1
1. Chengdu Center, China Geological Survey, Sichuan Chengdu 610081, China; 2. College of Earth Sciences, Chengdu University of Technology, Sichuan Chengdu 610059, China
Abstract:The environmental changes and geological disasters in Xichang City of western Yangtze block are closely related to the Cenozoic tectonic activities. The Cenozoic tectonic movement in this area is divided into five stages. ① During the Qinghai-Tibet movement stage (N1-2, 11.6~1.0 Ma), the strata were strongly squeezed to the east to form a series of compound fold systems, and the fault zone was dominated by compressional strike-slip activity.② During the extensional fault depression stage (N2—Q1, 3.6~1.0Ma), the fault zone was dominated by oblique strike-slip activity and the activity intensity was weak, forming faulted basins such as Anning river Valley.③ During the Yuanmou movement stage (Q1-2, 1.0~0.6 Ma), the strata were further squeezed eastward to thicken the crust by thrusting, and the early fold mountain system accelerated uplift. ④ During the tectonic relaxation stage (Q2, 0.6~0.126 Ma), the fault subsidence occurred again in the Anning river valley and other areas. ⑤ During the Republican movement stage (Q3-4, 0.126 Ma to present), the left-lateral strike-slip activity was dominant, and the fold mountain system was slowly denudated and uplifted as a whole. The Neotectonic movement in Xichang City has characteristics of strong intensity, difference, oscillation, inheritance and neogenesis. And it led to the present geomorphological pattern in this area and controlled the distribution of mountains, rivers and lakes, which formed a unique local climate and had great impacts on soil, vegetation and other ecological environment. Besides, the Neotectonic movement also directly or indirectly controls the evolution of geological environment, and the development of geological disasters and earthquakes in this area.
刘洪, 黄瀚霄, 欧阳渊, 李文昌, 张景华, 张腾蛟. 新构造活动的生态地质环境效应讨论——以扬子西缘西昌市为例[J]. 中国地质调查, 2021, 8(6): 63-77.
LIU Hong, HUANG Hanxiao, OUYANG Yuan, LI Wenchang, ZHANG Jinghua, ZHANG Tengjiao. Discussion on the eco-geo-environment effects of Neotectonic activities: A case study of Xichang City in western Yangtze block. , 2021, 8(6): 63-77.
[1] 吴中海,张会平.新构造与环境[J].地质力学学报,2021,27(2):157-158. Wu Z H,Zhang H P.Neotectonics and environment[J].J Geomechan,2021,27(2):157-158. [2] 刘洪,黄瀚霄,欧阳渊,等.基于地质建造的土壤地质调查及应用前景分析——以大凉山区西昌市为例[J].沉积与特提斯地质,2020,40(1):91-105. Liu H,Huang H X,Ouyang Y,et al.Soil's geologic investigation in Daliangshan,Xichang,Sichuan[J].Sediment Geol Tethyan Geol,2020,40(1):91-105. [3] 王京彬,卫晓锋,张会琼,等.基于地质建造的生态地质调查方法——以河北省承德市国家生态文明示范区综合地质调查为例[J].中国地质,2020,47(6):1611-1624. Wang J B,Wei X F,Zhang H Q,et al.The eco-geological survey based on geological Formation,exemplified by integrated geological survey of National Ecological Civilization Demonstration area in Chengde City,Hebei Province[J].Geol China,2020,47(6):1611-1624. [4] 卫晓锋,樊刘洋,孙紫坚,等.河北承德柴白河流域地质建造对植物群落组成的影响[J].中国地质,2020,47(6):1869-1880. Wei X F,Fan L Y,Sun Z J,et al.The influence of geological formation on plant community composition in Chaibai River Basin,Chengde,Hebei province[J].Geol China,2020,47(6):1869-1880. [5] 殷志强,卫晓锋,刘文波,等.承德自然资源综合地质调查工程进展与主要成果[J].中国地质调查,2020,7(3):1-12. Yin Z Q,Wei X F,Liu W B,et al.Progresses and main achievements of comprehensive geological survey project of natural resources in Chengde[J].Geol Surv China,2020,7(3):1-12. [6] 何泽新,樊刘洋,卫晓锋,等.基于地质建造和流域地貌的河北省承德蟠龙湖地区大比例尺地质遗迹调查[J].中国地质,2020,47(6):1881-1893. He Z X,Fan L Y,Wei X F,et al.Large-scale survey of geological heritage in the Panlong Lake area of Chengde,Hebei province:based on geological formations and watershed landforms[J].Geol China,2020,47(6):1881-1893. [7] 聂洪峰,肖春蕾,戴蒙,等.生态地质调查工程进展与主要成果[J].中国地质调查,2021,8(1):1-12. Nie H F,Xiao C L,Dai M,et al.Progresses and main achievements of ecogeological survey project[J].Geol Surv China,2021,8(1):1-12. [8] 何登发,李德生,王成善,等.活动论构造古地理的研究现状、思路与方法[J].古地理学报,2020,22(1):1-28. He D F,Li D S,Wang C S,et al.Status,thinking,and methodology of studying on the mobile tectono-palaeogeography[J].J Palaeogeogr,2020,22(1):1-28. [9] 莫宣学,赵志丹,周肃,等.印度-亚洲大陆碰撞的时限[J].地质通报,2007,26(10):1240-1244. Mo X X,Zhao Z D,Zhou S,et al.On the timing of India-Asia continental collision[J].Geol Bull China,2007,26(10):1240-1244. [10] 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 G T,Xiao Q H,Lu S N,et al.Subdivision of tectonic units in China[J].Geol China,2009,36(1):1-28. [11] Zhu Z M,Sun Y L.Direct Re-Os dating of chalcopyrite from the Lala IOCG deposit in the Kangdian Copper Belt,China[J].Econ Geol,2013,108(4):871-882. [12] 李文昌,江小均.扬子西缘陆内构造转换系统与构造岩浆成矿效应[J].地学前缘,2020,27(2):151-164. Li W C,Jiang X J.The Cenozoic tectono-magmatism-mineralization effect of the intracontinental tectonic transformation system in the western margin of Yangtze Block[J].Earth Sci Front,2020,27(2):151-164. [13] 张永双,刘筱怡,吴瑞安,等.青藏高原东缘深切河谷区古滑坡:判识、特征、时代与演化[J].地学前缘,2021,28(2):94-105. Zhang Y S,Liu X Y,Wu R A,et al.Cognization, characteristics,age and evolution of the ancient landslides along the deep-cut valleys on the eastern Tibetan Plateau,China[J].Earth Sci Front,2021,28(2):94-105. [14] 张岳桥,杨农,孟晖,等.四川攀西地区晚新生代构造变形历史与隆升过程初步研究[J].中国地质,2004,31(1):23-33. Zhang Y Q,Yang N,Meng H,et al.Late Cenozoic tectonic deformation history and uplift process of the Panxi region,western Sichuan[J].Geol China,2004,31(1):23-33. [15] 冯希杰. 再探中国大陆第四纪地壳运动时程[J].地震地质,1999,21(1):83-87. Feng X J.Another study on the time and process of Quaternary crustal movement of the Chinese continent[J].Seismol Geol,1999,21(1):83-87. [16] 葛肖虹,王敏沛,刘俊来.重新厘定”四川运动”与青藏高原初始隆升的时代、背景:黄陵背斜构造形成的启示[J].地学前缘,2010,17(4):206-217. Ge X H,Wang M P,Liu J L.Redefining the Sichuan Movement and the age and background of Qingzang Plateau’s first uplift:The implication of Huangling anticline and its enlightenment[J].Earth Sci Front,2010,17(4):206-217. [17] Li J J,Zhou S Z,Zhao Z J,et al.The Qingzang Movement:The major uplift of the Qinghai-Tibetan Plateau[J].Sci China Earth Sci,2015,58(11):2113-2122. [18] 张岳桥,李海龙.青藏高原东部晚新生代重大构造事件与挤出造山构造体系[J].中国地质,2016,43(6):1829-1852. Zhang Y Q,Li H L.Late Cenozoic tectonic events in east Tibetan Plateau and extrusion-related orogenic system[J].Geol China,2016,43(6):1829-1852. [19] 卞爽,于志泉,龚俊峰,等.青藏高原近南北向裂谷的时空分布特征及动力学机制[J].地质力学学报,2021,27(2):178-194. Bian S,Yu Z Q,Gong J F,et al.Spatiotemporal distribution and geodynamic mechanism of the nearly NS-trending rifts in the Tibetan Plateau[J].J Geomechan,2021,27(2):178-194. [20] Ahmed S.青藏高原东缘的隆升及其对河流演化和地貌形成的影响[D].杭州:浙江大学,2019:1-115. Ahmed S.Uplift of the Eastern Margin of Tibetan Plateau and Its Impact on River Network Pattern and Landscape Formation[D].Hangzhou:Zhejiang University,2019:1-115. [21] 张森琦,李永国,尚小刚,等.黄河源区新构造运动对生态环境恶化的影响[J].地质通报,2006,25(1):213-220. Zhang S Q,Li Y G,Shang X G,et al.Effects of neotectonic movement in the source area of the Yellow River,China on eco-environmental deterioration[J].Geol Bull China,2006,25(1):213-220. [22] 冯嘉辉,陈立春,王虎,等.大凉山断裂带北段石棉断裂的古地震[J].地震地质,2021,43(1):53-71. Feng J H,Chen L C,Wang H,et al.Paleoseismologic study on the Shimian fault in the northern section of the Daliangshan fault zone[J].Seismol Geol,2021,43(1):53-71. [23] 徐杰,李祥根,虢顺民.安宁河断裂带新构造运动的初步研究[J].地质科学,1978,13(3):235-246. Xu J,Li X G,Guo S M.A preliminary study of Neotectonic movement along the Anninghe faulting belt[J].Chin J Geol,1978,13(3):235-246. [24] 高萌萌,李瑞敏,徐慧珍,等.基于MapGIS建立的中国地质环境图系数据库[J].中国地质,2019,46(S2):130-140. Gao M M,Li R M,Xu H Z,et al.Database of geological environmental map system of China based on MapGIS[J].Geology in China,2019,46(S2):130-140. [25] 张腾蛟,刘洪,欧阳渊,等.中高山区土壤成土母质理化特征及主控因素初探——以西昌市为例[J].沉积与特提斯地质,2020,40(1):106-114. Zhang T J,Liu H,Ouyang Y,et al.A preliminary discussion on the physical and chemical characteristics and main controlling factors of soil and parent material in the Middle and high mountain area——take Xichang as an example[J].Sediment Geol Tethyan Geol,2020,40(1):106-114. [26] 张景华,欧阳渊,陈远智,等.基于无人机遥感的四川省昭觉县农业产业园土地适宜性评价[J/OL].中国地质.[2020-08-06].https://kns.cnki.net/kcms/detail/11.1167.P.20200806.1013.002.html. Zhang J H,Ouyang Y,Chen Y Z,et al.Land suitability evaluation of agricultural industrial park based on unmanned aerial vehicle's remote sensing in Zhaojue County of Sichuan province[J/OL].Geol China.[2020-08-06].https://kns.cnki.net/kcms/detail/11.1167.P.20200806.1013.002.html. [27] 李樋,刘小念,刘洪,等.西昌普诗地区中-下白垩统小坝组岩石-紫色土剖面稀土元素地球化学特征分析[J/OL].沉积与特提斯地质.[2021-06-08].https://doi.org/10.19826/j.cnki.1009-3850.2021.06002. Li T,Liu X N,Liu H,et al.Geochemistry of rare earth elements of purple soil layers in the Middle-Lower Cretaceous Xiaoba Formation,Pushi area,Xichang[J/OL].Sediment Geol Tethyan Geol.[2021-06-08].https://doi.org/10.19826/j.cnki.1009-3850.2021.06002. [28] 张慈,赵银兵,欧阳渊,等.青藏高原东缘地质环境对植被覆盖度的影响研究:以冕宁县为例[J/OL].沉积与特提斯地质.[2021-03-15].https://doi.org/10.19826/j.cnki.1009-3850.2021.03010. Zhang C,Zhao Y B,Ouyang Y,et al.Influence of geological environment on vegetation coverage in the eastern edge of Qinghai-Tibet Plateau:a case study of Mianning[J/OL].Sediment Geol Tethyan Geol.[2021-03-15].https://doi.org/10.19826/j.cnki.1009-3850.2021.03010. [29] 从柏林,赵大升,张雯华,等.西昌地区岩浆活动特征及其与构造地质的关系[J].地质科学,1973,8(3):175-195. Cong B L,Zhao D S,Zhang W H,et al.Characteristics of magmatic activity in the Xichang area and its bearing on the tectonic geological development[J].Chin J Geol,1973,8(3):175-195. [30] 尹福光,王冬兵,王保弟,等.西南三江造山带地层区划[J].沉积与特提斯地质,2017,37(4):1-8. Yin F G,Wang D B,Wang B D,et al.Stratigraphic classification in the Nujiang-Lancangjiang-Jinshajiang orogenic zone in southwestern China[J].Sediment Geol Tethyan Geol,2017,37(4):1-8. [31] 任飞,潘桂棠,尹福光,等.西南三江地区洋板块地层特征及构造演化[J].沉积与特提斯地质,2017,37(4):9-16. Ren F,Pan G T,Yin F G,et al.Oceanic plate stratigraphy and tectonic evolution of the Nujiang-Lancangjiang-Jinshajiang ar-ea in southwestern China[J].Sediment Geol Tethyan Geol,2017,37(4):9-16. [32] 高慧,吴文贤,张建龙.西南山区遥感蚀变异常信息提取综合研究——以云南酒房地区为例[J].沉积与特提斯地质,2017,37(4):107-112. Gao H,Wu W X,Zhang J L.Remote sensing information extraction of alteration anomalies in the Jiufang region,Yunnan,southwestern China:A case study[J].Sediment Geol Tethyan Geol,2017,37(4):107-112. [33] 闻学泽. 则木河断裂的第四纪构造活动模式[J].地震研究,1983,6(1):41-50. Wen X Z.Model of active tectonic of the Quaternary Period of Zemu River Fault[J].J Seismol Res,1983,6(1):41-50. [34] 谢吉尊,冯文凯,杨少帅,等.则木河断裂带活动特征和地质灾害对地貌演化的影响——以鹅掌河流域为例[J].工程地质学报,2017,25(3):772-783. Xie J Z,Feng W K,Yang S S,et al.Active characteristics and Geohazard of Zemuhe fault and their influence on morphological evolution in Ezhang River[J].J Eng Geol,2017,25(3):772-783. [35] 黄祖智,唐荣昌.则木河断裂与地震[J].地震研究,1983,6(2):167-177. Huang Z Z,Tang R C.The Zemuhe fault and earthquakes[J].J Seismol Res,1983,6(2):167-177. [36] 刘辛中,刘志广,朱爽,等.安宁河—则木河断裂带断层活动特征及其与地震活动的关系[J].震灾防御技术,2015,10(2):253-261. Liu X Z,Liu Z G,Zhu S,et al.Research on seismic activity feature of Anninghe-Zemuhe fault[J].Technol Earthq Disaster Prev,2015,10(2):253-261. [37] 何宏林,池田安隆.安宁河断裂带晚第四纪运动特征及模式的讨论[J].地震学报,2007,29(5):537-548. He H L,Ikeda Y.Faulting on the Anninghe fault zone,Southwest China in Late Quaternary and its movement model[J].Acta Seismol Sin,2007,29(5):537-548. [38] 冉勇康,程建武,宫会玲,等.安宁河断裂紫马跨一带晚第四纪地貌变形与断层位移速率[J].地震地质,2008,30(1):86-98. Ran Y K,Cheng J W,Gong H L,et al.Late Quaternary geomorphic deformation and displacement rates of the Anninghe fault around Zimakua[J].Seismol Geol,2008,30(1):86-98. [39] 程建武,郭桂红,岳志军.安宁河断裂带晚第四纪活动的基本特征及强震危险性分析[J].地震研究,2010,33(3):265-272. Cheng J W,Guo G H,Yue Z J.Basic characteristics and earthquake risk analysis of the Anning River fault zone in the West of Sichuan province[J].J Seismol Res,2010,33(3):265-272. [40] 范柱国,李峰,谈树成,等.丽江—大理地区新构造运动特征及环境效应[J].大地构造与成矿学,2002,26(1):6-9. Fan Z G,Li F,Tan S C,et al.The characteristics and environmental effecs of Neotectonic Movement in Lijiang-Dali region[J].Geotecton Metall,2002,26(1):6-9. [41] 蒋实. 攀枝花青龙山昔格达组剖面地球化学特征及其古气候环境演变[D].成都:成都理工大学,2010:1-100. Jiang S.Geochemical Characteristics and Paleoclimate Evolution of Qinglongshan Xigeda Formation in Panzhihua[D].Chengdu:Chengdu University of Technology,2010:1-100. [42] 程建武,宫会玲,郭雪莲.川西安宁河Ⅰ~Ⅲ级阶地孢粉记录反映晚更新世以来古气候变化[J].西北地震学报,2010,32(4):349-356. Cheng J W,Gong H L,Guo X L.Pollen records reflecting paleoclimate change since Late-Pleistocene in the terraces Ⅰ~Ⅲ of Anning river in western Sichuan province[J].Northwestern Seismol J,2010,32(4):349-356. [43] 张建平,王道杰,王玉宽,等.元谋干热河谷区生态环境变迁探讨[J].地理科学,2000,20(2):148-152. Zhang J P,Wang D J,Wang Y K,et al.Discusses on Eco-environment changes in dry-hot valley of Yuanmou[J].Sci Geograph Sin,2000,20(2):148-152. [44] 明庆忠,潘保田,苏怀,等.山区河谷-水系演化及环境效应研究——以金沙江为例[J].云南师范大学学报:自然科学版,2013,33(2):1-10. Ming Q Z,Pan B T,Su H,et al.Study on the valley & drainage evolution and its effects on environment:A case study of Jinsha River[J].J Yunan Normal Univ2013,33(2):1-10. [45] 魏晓玥,黄晓荣,潘荦,等.金沙江上游近60年径流变化对气候的响应[J].水力发电,2019,45(8):12-17. Wei X Y,Huang X R,Pan L,et al.Response of runoff change to climate in the upper reaches of Jinsha River in past 60 years[J].Water Power,2019,45(8):12-17. [46] 金德生,乔云峰,杨丽虎,等.新构造运动对冲积河流影响研究的回顾与展望[J].地理研究,2015,34(3):437-454. Jin D S,Qiao Y F,Yang L H,et al.A research of influence of neo-tectonic movement on alluvial rivers:Review and prospect[J].Geograph Res,2015,34(3):437-454. [47] 安艳芬,韩竹军,万景林.川南马边地区新生代抬升过程的裂变径迹年代学研究[J].中国科学(D辑):地球科学,2008,38(5):555-563. An Y F,Han Z J,Wan J L.Fission track dating of the Cenozoic uplift in Mabian area,southern Sichuan Province,China[J].Sci China Ser D:Earth Sci,2008,51(9):1238-1247. [48] 何宏林,池田安隆,何玉林,等.新生的大凉山断裂带—鲜水河—小江断裂系中段的裁弯取直[J].中国科学(D辑):地球科学,2008,38(5):564-574. He H L,Ikeda Y,He Y L,et al.Newly-generated Daliangshan fault zone-shortcutting on the central section of Xianshuihe-Xiaojiang fault system[J].Sci China Ser D:Earth Sci,2008,51(9):1248-1258. [49] 郑义加,孙丽娟,李敏刚.安宁河河谷平原地下水资源分布的初步分析[J].中国农资,2014(4):184-186. Zheng Y J,Sun L J,Li M G.Preliminary analysis of groundwater resources distribution in Anninghe valley plain[J].China agri-production news,2014(4):184-186. [50] 袁建飞,邓国仕,徐芬,等.西昌市尔乌泉域泉水水文地球化学特征及成因[J].水文地质工程地质,2017,44(4):15-22. Yuan J F,Deng G S,Xu F,et al.Hydrogeochemical characteristics and genesis of springs in the catchment area of the Erwu spring of Xichang[J].Hydrogeol Eng Geol,2017,44(4):15-22. [51] 张永双,郭长宝,姚鑫,等.青藏高原东缘活动断裂地质灾害效应研究[J].地球学报,2016,37(3):277-286. Zhang Y S,Guo C B,Yao X,et al.Research on the geohazard effect of active fault on the eastern Margin of the Tibetan Pla-teau[J].Acta Geosci Sin,2016,37(3):277-286. [52] 曹楠,申太丽,罗水莲,等.西昌市地质灾害发育分布规律及防灾建议[J].中国地质灾害与防治学报,2010,21(1):127-132. Cao N,Shen T L,Luo S L,et al.Development and distribution patterns of geologic hazards in Xichang City and prevention suggestion[J].Chin J Geol Hazard Control,2010,21(1):127-132. [53] 铁永波,徐如阁,刘洪,等.西昌市泸山地区典型火后泥石流特征与成因机制研究——以响水沟左岸3#支沟为例[J].中国地质调查,2020,7(3):82-88. Tie Y B,Xu R G,Liu H,et al.Study on the characteristics and Formation mechanism of the typical post-fire debris flow in Lu-shan area of Xichang City:A case study of 3# branch on the left bank of Xiangshuigou[J].Geol Surv China,2020,7(3):82-88. [54] 王帅,王深法,俞建强.构造活动与地质灾害的相关性——浙西南山地滑坡、崩塌、泥石流的分布规律[J].山地学报,2002,20(1):47-52. Wang S,Wang S F,Yu J Q.Study on the relationships between Neotectonism and Geological Hazards[J].J Mt Sci,2002,20(1):47-52.