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汶川地震驱动的隆升、剥蚀作用与龙门山地貌生长——以映秀红椿沟为例

ISSN号：1671-9727
期刊名称：成都理工大学学报(自然科学版)
时间：2015
页码：5-17
分类：P534.63[天文地球—第四纪地质学;天文地球—古生物学与地层学;天文地球—地质学]
作者机构：[1]油气藏地质及开发工程国家重点实验室(成都理工大学),成都610059, [2]四川省地震局工程地震研究院,成都610041, [3]中国地质科学院地质研究所,北京100037
相关基金：国家自然科学基金资助项目（40841010,40972083,41172162,41372114,41340005）; 国土资源部地质调查工作项目（1212011121268）; 油气藏地质及开发工程国家重点实验室自主研究课题（SK-0801）
相关项目：汶川地震驱动的崩塌、滑坡和泥石流的河流响应过程研究

关键词：汶川地震, 构造抬升, 同震滑坡, 震后泥石流, 沉积通量, 山脉生长, 红椿沟, 岷江, 龙门山, 青藏高原东缘, Wenchuan earthquake, landslide, debris flow, erosion, sediment flux, mountain growth, Hongchun gully, Minjiang River, Longmen Mountains, eastern margin, Tibetan Plateau

中文摘要：

汶川（Ms 8.0）地震驱动的构造抬升作用和滑坡、泥石流剥蚀作用如何影响龙门山的地貌生长是目前争论的焦点。作者以位于汶川地震震中位置的映秀红椿沟泥石流为例,利用野外实测资料、航片和数字高程资料,开展了红椿沟流域汶川地震驱动的构造抬升与滑坡、泥石流的表面侵蚀过程及其对龙门山地貌生长约束方面的定量研究,获得以下初步认识：（1）红椿沟位于汶川地震震中区的高山峡谷,发震断裂——北川断裂从该沟切过。（2）汶川地震触发的同震滑坡体积达3.800 1×10^6 m^3,是震前滑坡量的3倍。（3）2010-08-13和2010-08-18强降雨形成的震后泥石流体积为0.705×10^6 m^3,表明震后强降雨使同震滑坡量的20%转化为泥石流。（4）红椿沟泥石流将0.485×10^6 m^3固体物质输入岷江河道（主河）,导致河道变窄、河床升高、河床比降增大。（5）冲入河道量与同震滑坡量之间的转化率约为13%,冲入河道量与泥石流量之间的转化率为70%。（6）在红椿沟流域同震的滑坡体积（3.800 1×10^6 m^3）小于同震的构造抬升体积（6.67×10^6 m^3）,仅有约57%的构造抬升量转化为滑坡量,表明以逆冲-走滑作用为特征的汶川地震所导致的构造抬升量大于滑坡量,将使龙门山地貌产生新的抬升和生长。

英文摘要：

How the tectonic uplift,landslides,and debris flow erosion driven by the Wenchuan（Ms 8.0）earthquake affect the geomorphic growth of Mt.Longmen is the focus of the debate at present.The aim of this study is to make clear how the mass wasting triggered by the Wenchuan earthquake affect the growth of the Mt.Longmen.Field data,aerial photographs,and digital elevation data are used to conduct quantitative analyses of the tectonic uplift driven by the Wenchuan earthquake and of landslide and debris flow erosion processes,along with their effects on the geomorphic growth of Mt.Longmen.The preliminary insights obtained are as follows.（1）The Hongchun gully is located in alpine valleys within the earthquake epicenter area.The seismogenic fault- the Beichuan fault cuts through the gully.（2）The Wenchuan earthquake triggered the coseismic landslides of 3.800 1×10^6 m^3,being three times the volume before the earthquake.（3）The volume of the debris flow resulting from heavy rainfalls on August 13 and 18,2010 after the earthquake was 0.705×10^6 m^3,indicating that 20% of the volume of the coseismic landslides after the earthquake was changed into debris flows because of heavy rainfalls.（4）The Hongchun gully debris flow discharged solid materials of 0.485×10^6 m^3 into the Minjiang River（the main river）,leading the watercourse to be narrowed,the riverbed elevated,and the riverbed gradient increased.（5）The conversion ratio between the sediments input into the watercourse and the coseismic landslide sediments was about 13%.The conversion ratio between the sediments input into the watercourse and the debris flow sediments was 70%.（6）The volume（3.800 1×10^6 m^3）of the coseismic landslides in the Hongchun gully was less than that of the coseismic uplift（6.67×10^6 m^3）.Only about 57% of the uplift volume was converted into the landslide volume,indicating agreater volume of the tectonic uplift compared to the volume of the landslides resulting from the Wenchuan earthquake characterized by thr

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