必须声明标量变量 "@Script_ID"。 宁夏红寺堡盆地隐伏古隆起成因机制及其对区域沙漠化的影响-《地球科学与环境学报》
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[1]董晓朋,李振宏,黄 婷,等.宁夏红寺堡盆地隐伏古隆起成因机制及其对区域沙漠化的影响[J].地球科学与环境学报,2020,42(05):688-700.[doi:10.19814/j.jese.2020.05005]
 DONG Xiao-peng,LI Zhen-hong,HUANG Ting,et al.Origin of the Latent Palaeohigh in Hongsibu Basin of Ningxia, China and Its Effect on the Regional Desertification[J].Journal of Earth Sciences and Environment,2020,42(05):688-700.[doi:10.19814/j.jese.2020.05005]
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宁夏红寺堡盆地隐伏古隆起成因机制及其对区域沙漠化的影响(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第42卷
期数:
2020年第05期
页码:
688-700
栏目:
水资源与环境
出版日期:
2020-09-15

文章信息/Info

Title:
Origin of the Latent Palaeohigh in Hongsibu Basin of Ningxia, China and Its Effect on the Regional Desertification
文章编号:
1672-6561(2020)05-0688-13
作者:
董晓朋12李振宏12黄 婷12姜博宇3崔加伟12
1. 中国地质科学院地质力学研究所,北京 100081; 2. 自然资源部古地磁与古构造重建重点实验室,北京 100081; 3. 中国石油物资有限公司西安分公司,陕西 西安 710018
Author(s):
DONG Xiao-peng12 LI Zhen-hong12 HUANG Ting12 JIANG Bo-yu3 CUI Jia-wei12
1. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China; 2. Key Laboratory of Paleomagnetism and Tectonic Reconstruction of Ministry of Natural Resources, Beijing 100081, China; 3. Xi’an Branch of China Petroleum Materials Company Limited, Xi’an 710018, Shaanxi, China
关键词:
隐伏古隆起 盆山一体化 沙漠化 烟筒山断裂 剩余重力异常 音频大地电磁测深 二维地震勘探 宁夏
Keywords:
latent paleohigh coupling system between basin and range desertification Yantong-shan fault residual gravity anomaly AMT 2D seismic prospecting Ningxia
分类号:
P546
DOI:
10.19814/j.jese.2020.05005
文献标志码:
A
摘要:
目前对于青藏高原东北缘活动构造研究多集中于活动断裂带的活动性,而对夹持于其间的沉积盆地构造格架及活动性研究甚少。以夹持于烟筒山断裂与牛首山—罗山断裂之间的宁夏红寺堡盆地为研究对象,采用重力资料重处理解译、音频大地电磁测深(AMT)和地震勘探相结合,揭示红寺堡盆地隐伏构造特征,并进一步采用盆山一体化思路分析隐伏构造的成因机制及其对区域沙漠化的控制作用。结果表明:青藏高原在中新世末发生强烈的NE向推挤、扩展和隆升,红寺堡盆地由坳陷盆地转变为挠曲盆地; 在青藏高原NE向扩展的影响下,烟筒山断裂发生强烈的逆冲作用,古生代—中生代基底逆冲于古近系—新近系之上,受构造变形影响的最新地层为中新统彰恩堡组; 红寺堡盆地内的隐伏古隆起呈NW—SE向,与烟筒山构造带具有相同的构造动力学背景,受青藏高原NE向扩展影响形成于中新世末,并且至今仍具有活动性; 隐伏古隆起周缘断裂的活动破坏了地表稳定性、蓄水能力和地表植被,导致区域沙漠化呈现有规律的NW—SE向带状展布。该研究成果对于宁夏红寺堡盆地区域稳定性评价及沙漠化的综合治理具有现实指导意义。
Abstract:
Arc-shaped tectonic belt in the northeastern margin of Qinghai-Tibet Plateau consists of Haiyuan fault, Xiangshan-Tianjingshan fault, Yantongshan fault, Niushoushan-L uoshan fault and intermontane basins between these faults. Former’s researches about the active tectonic in the northeastern margin of Qinghai-Tibet Plateau mainly focus on the active activities of fault zones while the tectonic framework and activities in the intermontane basins are rarely known. Gravity anomalies interpretation, AMT and seismic prospecting in Hongsibu Basin of Ningxia between Yantongshan fault and Niushoushan-Luoshan fault were carried out, and the structural characteristics of the latent palaeohigh in this basin were revealed. Moreover, the origin of the latent palaeohigh and controlling factors of the desertification in Hongsibu Basin were discussed based on the theory of the coupling system between basin and range. The results show that the intense northeastward pushing, extension and uplift in the northeastern margin of Qinghai-Tibet Plateau occur at the end of Miocene; as a result, Hongsibu Basin is transformed from depression basin to flex basin; besides that, Paleozoic-Mesozoic basement thrust above Eogene-Neogene sedimentary stratum, and the latest strata which involve in the tectonic deformation is Miocene Zhang’enbao Formation; NW-SE trending latent paleohigh in Hongsibu Basin has the same tectonic background with Yantongshan tectonic zone; under the effect of the northeastern extention of Qinghai-Tibet Plateau, the latent paleohigh develops at the end of Miocene and is still active until now; the active movements of faults around the latent paleohigh destroy the stability, water storage capacity and surface vegetation, and the regional desertification around the latent paleohigh distributes in bands with NW-SE trending.The research is of great significance to the evaluation of the regional stability and comprehensive treatment of the desertification in Hongsibu Basin of Ningxia.

参考文献/References:

[1] 邓起东,程绍平,闵 伟,等.鄂尔多斯块体新生代构造活动和动力学的讨论[J].地质力学学报,1999,5(3):13-21.
DENG Qi-dong,CHENG Shao-ping,MIN Wei,et al.Discussion on Cenozoic Tectonics and Dynamics of Ordos Block[J].Journal of Geomechanics,1999,5(3):13-21.
[2] 邓起东,张培震,冉勇康,等.中国活动构造基本特征[J].中国科学:D辑,地球科学,2002,32(12):1020-1030.
DENG Qi-dong,ZHANG Pei-zhen,RAN Yong-kang,et al.Basic Characteristics of Active Structures in China[J].Science in China:Series D,Earth Sciences,2002,32(12):1020-1030.
[3] DENG Q D,SUNG F M,ZHU S L,et al.Active Faulting and Tectonics of the Ningxia Hui Autonomous Region,China[J].Journal of Geophysical Research:Solid Earth,1984,89(6):4427-4445.
[4] ZHANG W Q,JIAO D C,ZHANG P Z,et al.Displacement Along the Haiyuan Fault Associated with the Great 1920 Haiyuan Earthquake,China[J].Bulletin of the Seismological Society of America,1987,77(1):117-131.
[5] ZHANG P Z,MOLNAR P,BURCHFIEL B C,et al.Bounds on the Holocene Slip Rate of the Haiyuan Fault,North-central China[J].Quaternary Research,1988,30(2):151-164.
[6] ZHANG P Z,BURCHFIEL B C,MOLNAR P,et al.Later Cenozoic Tectonic Evolution of the Ningxia Hui Autonomous Region,China[J].Geological Society of America Bulletin,1990,102(11):1484-1498.
[7] BURCHEFIEL B C,ZHANG P Z,WANG Y P,et al.Geology of the Haiyuan Fault Zone,Ningxia Hui Autonomous Region,China,and Its Relation to the Evolution of the Northeastern Margin of the Qinghai-Tibet Plateau[J].Tectonics,1991,10(6):1091-1110.
[8] 柴炽章,张维歧,焦德成.天景山断裂带晚第四纪水平活动强度的分时、分段研究[J].中国地震,1997,13(1):35-42.
CHAI Chi-zhang,ZHANG Wei-qi,JIAO De-cheng.Discussion of the Level Active Severity in Different Time Intervals and Segments on Late Quaternary Along Tianjingshan Fault Zone[J].Earthquake Research in China,1997,13(1):35-42.
[9] 冉永康,段瑞涛,邓起东,等.海原断裂高湾子地点三维探槽的开挖与古地震研究[J].地震地质,1997,19(2):97-107.
RAN Yong-kang,DUAN Rui-tao,DENG Qi-dong,et al.3-D Trench Excavation and Paleoseismology at Gaowanzi of the Haiyuan Fault[J].Seismology and Geology,1997,19(2):97-107.
[10] DING Z L,XIONG S F,SUN J M,et al.Pedostratigraphy and Paleomagnetism of a ~7.0 Ma Eolian Loess-red Clay Sequence at Lingtai,Loess Plateau,North-central China and the Implications for Paleomonsoon Evolution[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1999,152(1/2):49-66.
[11] 刘 静,徐锡伟,李岩峰,等.以海原断裂甘肃老虎山段为例浅析走滑断裂古地震记录的完整性:兼论古地震研究中的若干问题[J].地质通报,2007,26(6):650-660.
LIU Jing,XU Xi-wei,LI Yan-feng,et al.On the Completeness of Paleoseismic Records of Strike-slip Faults:An Example from the Laohushan Segment of the Haiyuan Fault in Gansu,China,with a Discussion of Several Problems in the Paleoearthquake Study[J].Geological Bulletin of China,2007,26(6):650-660.
[12] 施 炜,刘 源,刘 洋,等.青藏高原东北缘海原断裂带新生代构造演化[J].地学前缘,2013,20(4):1-17.
SHI Wei,LIU Yuan,LIU Yang,et al.Cenozoic Tectonic Evolution of Haiyuan Fault Zone in the Northeast Margin of the Tibetan Plateau[J].Earth Science Frontiers,2013,20(4):1-17.
[13] CHEN H,HU J M,GONG W B,et al.Characteristics and Transition Mechanism of Late Cenozoic Structural Deformation Within the Niushoushan-Luoshan Fault Zone at the Northeastern Margin of the Qinghai-Tibet Plateau[J].Journal of Asian Earth Sciences,2015,114:73-88.
[14] 袁道阳,张培震,刘百篪,等.青藏高原东北缘晚第四纪活动构造的几何图像与构造转换[J].地质学报,2004,78(2):270-278.
YUAN Dao-yang,ZHANG Pei-zhen,LIU Bai-chi,et al.Geometrical Imagery and Tectonic Transformation of Late Quaternary Active Tectonics in Northeastern Margin of Qinghai-Xizang Plateau[J].Acta Geologica Sinica,2004,78(2):270-278.
[15] 宋友桂,方小敏,李吉均,等.晚新生代六盘山隆升过程初探[J].中国科学:D辑,地球科学,2001,31(增):142-148.
SONG You-gui,FANG Xiao-min,LI Ji-jun,et al.Exploration About the Uplift of the Liupan Shan During the Late Cenozoic[J].Science in China:Series D,Earth Sciences,2001,31(S):142-148.
[16] ZHENG D W,ZHANG P Z,WAN J L,et al.Rapid Exhumation at ~8 Ma on the Liupan Shan Thrust Fault from Apatite Fission-track Thermochronology:Implications for Growth of the Northeastern Qinghai-Tibet Plateau Margin[J].Earth and Planetary Science Letters,2006,248(1/2):198-208.
[17] WANG W T,KIRBY E,ZHANG P Z,et al.Tertiary Basin Evolution Along the Northeastern Margin of the Qinghai-Tibet Plateau:Evidence for Basin Formation During Oligocene Transtension[J].Geological Society of American Bulletin,2013,125(3/4):377-400.
[18] AN K X,LIN X B,WU L,et al.An Immediate Response to the Indian-Eurasian Collision Along the Northeastern Qinghai-Tibet Plateau:Evidence from Apatite Fission Track Analysis in the Kuantan Shan-Hei Shan[J].Tectonophysics,2020,774:228278.
[19] DING G Y,CHEN J,TIAN Q J,et al.Active Faults and Magnitudes of Left-lateral Displacement Along the Northern Margin of the Qinghai-Tibet Plateau[J].Tectonophysics,2004,380:243-260.
[20] 王伟涛,张培震,郑德文,等.青藏高原东北缘海原断裂带晚新生代构造变形[J].地学前缘,2014,21(4):266-274.
WANG Wei-tao,ZHANG Pei-zhen,ZHENG De-wen,et al.Late Cenozoic Tectonic Deformation of the Haiyuan Fault Zone in the Northeastern Margin of the Tibetan Plateau[J].Earth Science Frontiers,2014,21(4):266-274.
[21] TIAN J X,LI M T,LIANG Z R,et al.Tectonic Evolution of the Qingshuihe Basin Since the Late Miocene:Relationship with North-eastward Expansion of the Tibetan Plateau[J].Geological Journal,2019,DOI:10.1002/gj.3650.
[22] LI X N,FENG X J,LI X N,et al.Geological and Geomorphological Evidence for Active Faulting of the Southern Liupanshan Fault Zone,NE Tibetan Plateau[J].Geomorphology,2019,345:106849.
[23] 汪一鹏,宋方敏,李志义,等.宁夏香山—天景山断裂带晚第四纪强震重复间隔的研究[J].中国地震,1990,6(2):15-24.
WANG Yi-peng,SONG Fang-min,LI Zhi-yi,et al.Study on Recurrence Intervals of Great Earthquakes in the Late Quateranary of Xiangshan-Tianjingshan Fault Zone in Ningxia[J].Earthquake Research in China,1990,6(2):15-24.
[24] 张 珂,刘开瑜,吴加敏,等.宁夏中卫盆地的沉积特征及其所反映的新构造运动[J].沉积学报,2004,22(3):465-473.
ZHANG Ke,LIU Kai-yu,WU Jia-min,et al.Depositional Features of the Zhongwei Basin,Ningxia and Its Implications for Neotectonic Movements[J].Acta Sedimentologica Sinica,2004,22(3):465-473.
[25] 李传友.青藏高原东北部几条主要断裂带的定量研究[D].北京:中国地震局地质研究所,2005.
LI Chuan-you.Quantitative Studies on Major Active Fault Zones in Northeastern Qinghai-Tibet Plateau[D].Beijing:Institute of Geology,China Earthquake Adiministration,2005.
[26] 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 Jian-bo.Preliminary Result of the Dating by TCN Technique of the Highest Terrace of the Heishanxia Gorge Mouth,Northeast Margin of Qinghai-Tibet Plateau and Its Expression of Neotectonic Movement in That Area[J].Quaternary Sciences,2006,26(1):85-91.
[27] 李新男.香山—天景山断裂带西段晚第四纪运动学特征与古地震研究[D].北京:中国地震局地质研究所,2014.
LI Xin-nan.Late Quaternary Kinematic Characteristics and Paleoearthquakes Along the Western Segment of the Xiangshan-Tianjingshan Fault[D].Beijing:Institute of Geology,China Earthquake Adiministration,2014.
[28] 李新男,李传友,张培震,等.香山—天景山断裂带西段的运动性质变化及其成因机制[J].地震地质,2016,38(3):732-746.
LI Xin-nan,LI Chuan-you,ZHANG Pei-zhen,et al.Changes in Fault Movement Property and Genetic Mechanism on the Western Segment of the Xiang-shan-Tianjingshan Fault Zone[J].Seismology and Geology,2016,38(3):732-746.
[29] 王伟涛,张培震,雷启云.牛首山—罗山断裂带的变形特征及其构造意义[J].地震地质,2013,35(2):195-207.
WANG Wei-tao,ZHANG Pei-zhen,LEI Qi-yun.Deformation Characteristics of the Niushoushan-Luo-shan Fault Zone and Its Tectonic Implications[J].Seismology and Geology,2013,35(2):195-207.
[30] 国家地震局地质研究所,宁夏回族自治区地震局.海原活动断裂带[M].北京:地震出版社,1990.
Institute of Geology of State Seismological Bureau,Earthquake Agency of Ningxia Hui Autonomous Region.Haiyuan Active Fault Zone[M].Beijing:Seismological Press,1990.
[31] 陈 虹,胡健民,公王斌,等.青藏高原东北缘牛首山—罗山断裂带新生代构造变形与演化[J].地学前缘,2013,20(4):18-35.
CHEN Hong,HU Jian-min,GONG Wang-bin,et al.Cenozoic Deformation and Evolution of the Niushoushan-Luoshan Fault Zone in the Northeast Margin of Tibet Plateau[J].Earth Science Frontiers,2013,20(4):18-35.
[32] 马寅生,廖椿庭,张业成,等.黄河上游新构造活动与地质灾害风险评价[M].北京:地质出版社,2003.
MA Yin-sheng,LIAO Chun-ting,ZHANG Ye-cheng,et al.The Neotectonic Activity and the Evaluation of Geological Hazards Risk in the Upper Reaches of the Yellow River[M].Beijing:Geological Publishing House,2003.
[33] 赵红格,刘池洋,姚亚明,等.鄂尔多斯盆地西缘差异抬升的裂变径迹证据[J].西北大学学报(自然科学版),2007,37(3):470-474.
ZHAO Hong-ge,LIU Chi-yang,YAO Ya-ming,et al.Differential Uplift in Western Margin of Ordos Basin Since Mesozoic from the Fission Track Evidence[J].Journal of Northwest University(Natural Science Edition),2007,37(3):470-474.
[34] 赵 杨.宁南盆地丁家二沟剖面古近纪—新近纪沉积特征及其构造意义[D].北京:中国地质大学,2019.
ZHAO Yang.Sedimentary Characteristics and Tectonic Significance of Paleogene-Neogene in Dingjiaer-gou Profile of the Southern Ningxia Basin[D].Beijing:China Unverisity of Geosiences,2019.
[35] 崔加伟,李振宏,刘 锋,等.宁夏红寺堡盆地萨拉乌苏组地层时代重新厘定及意义[J].地质力学学报,2018,24(2):283-292.
CUI Jia-wei,LI Zhen-hong,LIU Feng,et al.Redefinition of the Sedimentary Time of Salawusu Formation in Hongsibu Basin,Ningxia and Its Significance[J].Journal of Geomechanics,2018,24(2):283-292.
[36] 黄 婷,李振宏,刘 锋,等.宁夏红寺堡盆地地表沙漠化现状及其地质主控因素[J].地质力学学报,2018,24(4):505-514.
HUANG Ting,LI Zhen-hong,LIU Feng,et al.The Current Situation of Desertification in the Hongsibu Basin,Ningxia,and Its Main Geological Controlling Factors[J].Journal of Geomechanics,2018,24(4):505-514.
[37] CALASSOU S,LARROQUE C,MALAVIEILLE J.Transfer Zones of Deformation in Thrust Wedges:An Experimental Study[J].Tectonophysics,1993,221(3/4):325-344.
[38] RAVAGLIA A,TURRINI C,SENO S.Mechanical Stratigraphy as a Factor Controlling the Development of a Sandbox Transfer Zone:A Three-dimensional Analysis[J].Journal of Structural Geology,2004,26(12):2269-2283.
[39] 王伟涛.宁夏南部新生代盆地沉积演化及其对青藏高原东北角构造变形的响应[D].北京:中国地震局地质研究所,2011.
WANG Wei-tao.Sedimentary Responses to the Cenozoic Tectonic Evolution of the Northeastern Corner of the Qinghai-Tibet Plateau[D].Beijing:Institute of Geology,China Earthquake Adiministration,2011.
[40] 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 Wei-tao,ZHENG De-wen,PANG Jian-zhang.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.
[41] WANG W T,ZHENG W J,ZHANG P Z,et al.Expansion of the Qinghai-Tibet Plateau During the Neogene[J].Nature Communications,2017,8(1):1-12.
[42] 黄桂华,黄立峰.生态移民地区跨越式发展的思考:以宁夏吴忠市红寺堡区为例[J].贵州民族研究,2010,31(2):101-105.
HUANG Gui-hua,HUANG Li-feng.Ecology Immigration Area Leap Frog Development Ponder:Take the Ningxia Wuzhong Hongsibu Area as the Example[J].Guizhou Ethnic Studies,2010,31(2):101-105.
[43] 郭慧秀,贾科利.基于GIS的生态脆弱移民区土地资源承载力评价:以红寺堡区为例[J].宁夏工程技术,2015,14(4):375-379.
GUO Hui-xiu,JIA Ke-li.Bearing Capacity of Land Resources Evaluation on GIS in the Ecological Fragile Area:Take Hongsibu as an Example[J].Ningxia Engineering Technology,2015,14(4):375-379.
[44] 张森琦,石维栋,朱 桦,等.黄河源区生态环境恶化的地质原因及发展演化趋势[J].西北地质,2004,37(2):101-106.
ZHANG Sen-qi,SHI Wei-dong,ZHU Hua,et al.The Reason for Degeneration of the Eco-environment Advance Trend in the Headwater Area of the Yellow River[J].Northwestern Geology,2004,37(2):101-106.
[45] 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(1/2):213-220.
ZHANG Sen-qi,LI Yong-guo,SHANG Xiao-gang,et al.Effects of Neotectonic Movement in the Source Area of the Yellow River,China on Eco-environmental Deterioration[J].Geological Bulletin of China,2006,25(1/2):213-220.
[46] 康相武,吴绍洪,刘雪华.浑善达克沙地土地沙漠化时空演变规律研究[J].水土保持学报,2009,23(1):1-6.
KANG Xiang-wu,WU Shao-hong,LIU Xue-hua.Research on Spatio-temporal Change of Sandy Desertification in Hunshandake[J].Journal of Soil and Water Conservation,2009,23(1):1-6.
[47] 花 婷,王训明,次 珍,等.中国干旱、半干旱区近千年来沙漠化对气候变化的响应[J].中国沙漠,2012,32(3):618-624.
HUA Ting,WANG Xun-ming,CI Zhen,et al.Responses of Desertification to Climate Change in Arid and Semiarid Regions of China over the Past Millennium[J].Journal of Desert Research,2012,32(3):618-624.
[48] 罗 君,许端阳,任红艳.2000~2010年鄂尔多斯地区沙漠化动态及其气候变化和人类活动驱动影响的辨识[J].冰川冻土,2013,35(1):48-56.
LUO Jun,XU Duan-yang,REN Hong-yan.The Desertification Dynamics in Ordos from 2000 to 2010 and Their Relationship with Climate Change and Human Activities[J].Journal of Glaciology and Geocryology,2013,35(1):48-56.

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备注/Memo:
收稿日期:2020-05-05; 修回日期:2020-07-01; 网络首发日期:2020-08-26投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41972119); 中国地质调查局地质调查项目(DD20190018,DD20160060)
作者简介:董晓朋(1989-),男,山东潍坊人,中国地质科学院地质力学研究所助理研究员,理学博士,E-mail:dongxiaopeng_geo@163.com。
更新日期/Last Update: 2020-09-20