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Episodic Orogeny Deduced from Coeval Sedimentary Sequences in the Foreland Basin and Its Implication for Uplift Process of longmen Mountain,China

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Journal of Mountain Science 2013年第1期10卷 29-42页

作者： lI Yong SU De-chen ZHOU Rong-jun lI Hai-bing alexander l.densmore YAN liang YAN Zhao-kun State Key laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu University of Technology Institute of Geology Chinese Academy of Geological Science Institute of Earthquake Engineering Seismological Bureau of Sichuan Province Institute of Hazard and Risk Research and Department of Geography Durham University

longmen Mountain located at the boundary between the Sichuan Basin and Tibetan Plateau,representing the steepest gradient of any edges of the *** endmember models of uplift process and mechanism have been proposed,including crustal thickening,crustal flow,and crustal isostatic *** we use coeval sedimentary sequences in the foreland basin to restraint uplift process and mechanism in the longmen *** more than 10,000 m thick late TriassicQuaternary strata filled in this foreland basin and can be divided into six megasequences that are distinguished as two distinct *** first type is the wedge-shaped megasequences which are sedimentary response of strong active thrust loading events,characterized by a high rate of subsidence and sediment accumulation,coarsening-upward succession and a dual-sourced sediment *** type includes late Triassic,late Jurassic to Early Cretaceous and late Cretaceous to Paleogene *** second type is the tabular megasequences,characterized by the low rate of subsidence and sediment accumulation,finingupward succession,and a single-sourced sediment supply,which is sedimentary response of isostatic rebound and erosion *** type includes the Early to Middle Jurassic,Middle Cretaceous and Neogene to Quaternary *** on sedimentary,active tectonic,geomorphic evidence,we infer that the direction has been reversed from SSWdirected sinistral strike-slip to NNE-directed dextral strike-slip during 40-3.6 Ma,and since 3.6 Ma,the longmen Mountain thrust belt belong to times of isostatic rebound and erosional unloading with NNEdirected dextral *** suggests that crustal isostatic rebound is a primary driver for uplift and topography of the present longmen *** Wenchuan(Ms8.0) earthquake,which ruptured a large thrust fault with NNE-directed dextral strikeslip along the range front,is an active manifestation of this crustal isostatic rebound process with dextral st

关键词： Wedge-shaped megasequence Tabular megasequence Orogenic loading Erosional unloading Uplift process longmen Mountain Foreland basin

Active Tectonics and Erosional Unloading at the Eastern Margin of the Tibetan Plateau

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Journal of Mountain Science 2005年第2期2卷 146-154页

作者： alexander l. densmore lI Yong Michael A. Ellis ZHOU Rongjun Institute of Geology Department of Earth Sciences ETH Zentrum CH-8092 Zürich Switzerland National Key laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu University of Technology Chengdu 610059 China Center for Earthquake Research and Information University of Memphis 3890 Central Avenue Memphis TN 38152 USA Institute of Earthquake Engineering Seismological Bureau of Sichuan Province Chengdu 610041 China

The eastern margin of the Tibetan Plateau is marked by an extremely steep mountain front with relief of over 5 km. This topography,coupled with abundant Mesozoic thrusts within the margin,explains why tectonic maps of the India-Asia collision typically show the eastern margin as a major thrust zone. Actually,it does not like that. Field observations suggest that the margin is better characterized as a zone of NNE-directed dextral shear with extensive strike-slip faulting and secondary thrusting. The high relief and steep gradients are partially explained by erosional unloading of an elastic lithosphere;the pre-erosion inherited topography may be the inherited Mesozoic thrust belt landscape modified by a component of Cenozoic tectonic shortening.

关键词： Tibetan Plateau tectonic erosional unloading faulting

利用水系流域偏转研究走滑断层的运动模式--以南汀河断裂带为例

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地震地质 2018年第4期40卷 773-783页

作者：石峰何宏林 alexander l densmore 魏占玉孙浩越中国地震局地质研究所活动构造与火山重点实验室北京100029 英国杜伦大学地理系英国杜伦DLI3LE

构造地貌能够记录构造运动的长期积累,并能通过相关参数定量表达。水系是对构造作用反映最敏感的地貌之一,长期以来许多研究者利用水系来反映和研究构造。但是过去的研究大都集中在垂直运动的构造作用区域上,尤其是正断层区域上,而对走... 详细信息

构造地貌能够记录构造运动的长期积累,并能通过相关参数定量表达。水系是对构造作用反映最敏感的地貌之一,长期以来许多研究者利用水系来反映和研究构造。但是过去的研究大都集中在垂直运动的构造作用区域上,尤其是正断层区域上,而对走滑作用区域的研究非常少。文中以南汀河断裂带为研究区域,利用高精度DEM数据提取水系。通过研究断层附近水系流域的偏转来研究南汀河断裂带的运动模式。通过分析流水地貌对断层活动的响应特征,对断裂带的空间展布和活动性进行了分析,为探讨活动断层与地貌响应之间的关系提供良好范例。

关键词：水系偏转角构造地貌南汀河断裂带

二维分形参数与构造活动关系研究--以滇西南块体为例

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地震地质 2016年第4期38卷 862-873页

作者：石峰何宏林 alexander l densmore 毕丽思魏占玉中国地震局地质研究所活动构造与火山重点实验室北京100029 Department of Geography Durham UniversityDurhamUK 广东省地震局广州510070

构造地貌能够记录构造运动的长期积累,并能通过相关参数定量表达。但是,由于地貌还受到气候和岩性等因素的影响,所以如何利用相关参数来表达地貌与构造之间的关系是一个研究热点。文中利用水平分辨率为90m的SRTM数据,采用元分维模型,通... 详细信息

构造地貌能够记录构造运动的长期积累,并能通过相关参数定量表达。但是,由于地貌还受到气候和岩性等因素的影响,所以如何利用相关参数来表达地貌与构造之间的关系是一个研究热点。文中利用水平分辨率为90m的SRTM数据,采用元分维模型,通过变差函数法计算了滇西南地区的二维分形参数。并对比了在不同岩性不同气候条件下分形参数的分布特征。结果显示,二维分形参数与岩性、气候因素相关性不强。而分维值与构造活动因素相关性很好,在构造活动强烈区域分维值较低,在构造活动不强烈区域分维值较高。这说明分维值能在一定程度上反映构造活动的强弱,为研究区域构造活动提供了一种新的手段。

关键词：分形参数构造活动滇西南块体

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青藏高原东缘活动构造

矿物岩石 2006年第2期26卷 40-51页

作者：周荣军李勇 alexander l densmore Michael A Ellis 何玉林王凤林黎小刚四川省地震局工程地震研究所成都理工大学油气藏地质及开发工程国家重点实验室 Institute of Geology Department of Earth SciencesETH Zentrum CH-8092 ZürichSwitzerland Center for Earthquake Research and Information University of Memphis 3890 Central AvenueMemphisTN 38152USA

青藏高原东缘由岷山断块和龙门山构造带构成。以活动构造地貌学为主线,在解析该地区主干断裂晚第四纪以来活动的地质地貌表现的基础上,对一批断裂运动学和史前强震活动的定量数据进行分析研究,结果表明:在岷山断块中,虎牙断裂的平均左... 详细信息

青藏高原东缘由岷山断块和龙门山构造带构成。以活动构造地貌学为主线,在解析该地区主干断裂晚第四纪以来活动的地质地貌表现的基础上,对一批断裂运动学和史前强震活动的定量数据进行分析研究,结果表明:在岷山断块中,虎牙断裂的平均左旋滑动速率为1.4 mm/a,垂直滑动速率为0.3 mm/a。岷江断裂的平均垂直滑动速率介于0.37 mm/a^0.53 mm/a之间,左旋位错量与垂直位错量大致相当;在龙门山构造带中,茂汶-汶川断裂、北川-映秀断裂和彭县-灌县断裂的平均垂直滑动速率均在1 mm/a左右,且几条主干断裂的右旋位错量与垂直位错量相当。结合震源机制解结果和GPS测量资料,建立晚新生代以来青藏高原东缘向南东方向逸出的构造变形模式。

关键词：构造地貌滑动速率强震复发青藏高原东缘

Surface Rupture and Hazard of Wenchuan Ms 8.0 Earthquake, Sichuan, China

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International Journal of Geosciences 2010年第1期1卷 21-31页

作者： Yong li Runqiu Huang liang Yan alexander l. densmore Rongjun Zhou 不详

longmen Shan is located the special joint between the Qinghai-Tibetan Plateau in the west and the Yangtze craton in the east. Consisting of a series of parallel imbricated thrust, it develops, from the west to the east, the Maoxian-Wenchuan, Yingxiu-Beichuan and Pengxian-Guanxian faults. Wenchuan Ms 8.0 earthquake is a thrust with strike-slip type, and surface ruptures are located in Yingxiu-Beichuan fault zone and Peng- xian-Guanxian fault zone. Based on the geological background, tectonic setting, the active tectonics of long- men Shan and surface ruptures of the Wenchuan earthquake, a dynamical model to illustrate possible links between surface processes and upward extrusion of lower crustal flow channel at the eastern margin of the Tibetan plateau have been studied, and the results is the material in lower crust in the longmen Shan moving as nearly-vertical extrusion and uplift, resulting in the surface rate of tectonic movement differing according to depth rate as well as the occurrence of large shallow Wenchuan earthquake.

关键词： Wenchuan Earthquake longmen Shan Surface Rupture Hazard Sichuan China

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映秀-北川断裂的地表破裂与变形特征

地质学报 2008年第12期82卷 1688-1706页

作者：李勇周荣军 alexander l.densmore 闫亮 Nicholas RICHARDSON 董顺利 Michael A.EllIS 张毅何玉林陈浩乔宝成马博琳成都理工大学油气藏地质及开发工程国家重点实验室 610059 四川省地震局工程地震研究院成都610041 Institute of Hazard and Risk Research and Department of Geography Durham UniversityDurhamUK Department of Earth Science Swiss Federal Institute of TechnologyZurichSwitzerland Center for Earthquake Research and Information University of MemphisMemphisTennesseeUSA

2008年5月12日在龙门山映秀-北川断裂带发生的8.0级特大地震,属于逆冲—走滑型地震。本文以地表破裂为切入点,在映秀-北川断裂的关键部位开展了详细的野外地貌测量,标定了映秀-北川断裂带的垂向断距和水平断距,结果表明映秀-北川断裂的... 详细信息

2008年5月12日在龙门山映秀-北川断裂带发生的8.0级特大地震,属于逆冲—走滑型地震。本文以地表破裂为切入点,在映秀-北川断裂的关键部位开展了详细的野外地貌测量,标定了映秀-北川断裂带的垂向断距和水平断距,结果表明映秀-北川断裂的地表破裂带从映秀向北东延伸达180～190km,走向介于NE30°～50°之间,倾向北西,地表平均垂向断距为2.9m,平均水平断距为3.1m;地表最大错动量的地点位于北川县擂鼓镇,垂直断错为6.2±0.1m,水平断错为6.8±0.2m,逆冲分量与右行走滑分量的比值为3∶1～1∶1,表明该断裂以逆冲—右行走滑为特点,逆冲运动分量略大于或等于右行走滑运动分量。根据近南北向的分段断裂可将映秀-北川断层的地表破裂带划分为两个高值区和两个低值区,其中两个高值区分别位于南段的映秀—虹口一带和中北段的擂鼓—北川县城—邓家坝一带。基于保存于破裂面上的擦痕,我们将该地震破裂过程划分为两个阶段,早期为逆冲作用,晚期为斜向走滑作用。

关键词：汶川地震地表破裂映秀-北川断裂走滑-逆冲作用龙门山

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汶川(M_s8.0)地震的河流地貌响应

第四纪研究 2013年第4期33卷 785-801页

作者：李勇周荣军苏德辰 alexander l.densmore 丁海容陈浩闫亮颜照坤乔宝成马博琳云琨赵国华马超成都理工大学油气藏地质及开发工程国家重点实验室成都610059 四川省地震局工程地震研究院成都610041 中国地质科学院地质研究所北京100037 Institute of Hazard and Risk Research and Department of Geography Durham University

2008年5月12日龙门山汶川(M_S8.0)地震导致了北川断裂、彭灌断裂和小鱼洞断裂发生了地表破裂,显示为两条近于平行的北东向逆冲-走滑型断层。同震变形在瞬间就改变了地形坡度,并产生了巨量的滑坡和泥石流,导致河流地貌产生相应的变化和... 详细信息

2008年5月12日龙门山汶川(M_S8.0)地震导致了北川断裂、彭灌断裂和小鱼洞断裂发生了地表破裂,显示为两条近于平行的北东向逆冲-走滑型断层。同震变形在瞬间就改变了地形坡度,并产生了巨量的滑坡和泥石流,导致河流地貌产生相应的变化和响应。本文在整合汶川地震所导致的地表破裂、地形和水系变化相关数据的基础上,标定了汶川地震驱动的逆冲-走滑型构造作用对河流坡折点、河流转折点、河道走向的控制作用,刻画了平行的走滑-逆冲断层对河流地貌与不规则水系样式的控制作用,讨论了汶川地震驱动的隆升作用对河床梯度剖面的影响,探讨了汶川地震和暴雨驱动滑坡、泥石流和洪水及其剥蚀卸载作用对河道地貌和龙门山地形演化的影响。研究结果表明:1)汶川地震驱动的右行走滑作用导致水平位错和偏转,使水系产生新的河流流向的转折点;2)汶川地震驱动的逆冲作用导致的垂向位错使水系产生新的河流坡折点;3)汶川地震驱动的活动断层走向对河道走向具有控制作用;4)汶川地震驱动抬升作用导致河床梯度平衡剖面和剥蚀基准面的变化;5)汶川地震驱动的滑坡使得该地区剥蚀作用加强,同震滑坡量远大于同震岩石隆升增加的山脉体积,导致了龙门山造山带的物质亏损;6)龙门山地形雨的"雨影区"产生的强降雨带与汶川地震驱动的地表破裂带和滑坡带的空间分布位置一致,暴雨季节来临时容易出现滑坡、泥石流和洪水,这是未来几十年所面临的地质灾害。因此认为,在龙门山地震活动频繁的地区,河流地貌和水系样式主要受地震构造活动控制。

关键词：汶川地震地表破裂河流地貌水系响应河道走向河道坡折带河道转折带河床剖面滑坡泥石流构造负载剥蚀卸载龙门山青藏高原东缘

Parasites of the liver:A global problem?

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World Journal of Gastroenterology 2024年第30期30卷 3554-3559页

作者： Vladislav V Tsukanov alexander V Vasyutin Julia l Tonkikh Clinical Department of the Digestive System Pathology of Adults and Children Federal Research Center“Krasnoyarsk Science Center”of the Siberian Branch of the Russian Academy of SciencesScientific Research Institute of Medical Problems of the NorthKrasnoyarsk 660022Russia

Parasitic liver diseases can be caused by trematodes,cestodes,nematodes,and *** pathology is significant because millions of people in different parts of the world have liver parasites,which can manifest themselves in the development of inflammation,liver cysts,cholecystitis,cholelithiasis,pancreatitis and liver cirrhosis that are often threatening their *** International Agency for Research on Cancer considers three species of trematodes,Schistosoma haematobium,Opisthorchis viverrini and Clonorchis sinensis,to be *** modern examination methods,in some cases including extensive screening of large populations,are required for diagnosing liver *** of parasitic liver diseases is differentiated and can involve a combination of surgical and therapeutic *** is no doubt that the clinical and epidemiological scale allows one to regard parasitic liver diseases as a global healthcare problem.

关键词： liver Parasites Epidemiology Diagnosis Clinics Treatment Echinococcosis Opisthorchiasis Fascioliasis Schistosomiasis