基于ArcGIS的条带剖面提取方法在地貌分析中的应用   总被引：3，自引：0，他引：3  

邹斌文  马维峰  龙昱  侯圣山  张林 《地理与地理信息科学》2011,27(3):42-44

条带剖面提取方法是利用数理统计原理,获得垂直于剖面线方向上一定缓冲区范围的高程信息,计算最大、最小和平均高程以及地形起伏度,把地形剖面图对线状地形起伏特征的描述转化为对面状地形起伏特征的描述。该文基于ArcGIS 9.3对三峡地区SRTM-DEM数据进行了条带剖面提取方法研究,实现了基于ArcGIS的条带剖面提取技术流程。应用条带剖面对三峡地区地形地貌进行了定量分析,该方法可快速提取条带剖面,能准确获取高程属性的相关统计参数,对地形地貌信息提取和定量分析具有一定价值。  相似文献   

三维古地貌重建技术在中生代羌塘地体古地理演化分析中的应用     

于淼  陈建平  严琼  武瞾  王春女  于萍萍 《地质通报》2011,30(5):694-701

近年来,从古地貌-沉积组合与油藏关系的角度进行油气远景评价成为研究热点。针对古地貌的复原研究,提出一种建立三维古地貌模型的方法,将二维平面古地理图通过对资料的整理、挖掘与转换,并结合GIS技术生成了三维立体模型,补充了区域地形地貌的相关信息。利用该方法,建立了青藏高原油气资源潜力最大的区域——羌塘地体在三叠纪和侏罗纪的一系列三维古地貌模型,进而对其古环境和演化过程进行分析,这对于该区域的沉积矿产资源的预测与评价有重要的参考价值。  相似文献   

上海湖沼平原地貌分界线上地层分布特征研究   总被引：1，自引：0，他引：1  

孙莉 《上海国土资源》2011,32(4):68-72

上海湖沼平原和滨海平原地貌类型划分应遵从地貌特征,为工程应用方便,可划分地貌亚区。地貌分界线上典型的地质剖面,为湖沼平原第一硬土层与滨海平原暗绿色硬土层属于同一地质时代提供了直接证据。由于古河道、台地等古地貌特征,造就了不同地貌及地貌亚区之间地层差异。  相似文献   

江西信江盆地丹霞地貌形成机制分析   总被引：1，自引：1，他引：0  

姜勇彪  郭福生  刘林清  胡中华  吴志春  吴智勇 《热带地理》2011,31(2)

信江盆地是我国丹霞地貌发育最典型的区域之一。由于影响丹霞地貌演化的成景系统诸要素具有不同特征,信江盆地内不同部位丹霞地貌经历了不同的演化进程,不同发育阶段的丹霞地貌在盆地内成带状分布。盆地边缘由于受红层岩性、断裂构造及信江支流等因素影响,地表剥蚀速率快,丹霞地貌演化已步入壮年晚期至老年早期阶段,以丹霞石林、峰林、峰丛、崖壁以及各种类型的造型石为特征;盆地中部虽然断裂构造发育程度较弱,但受信江流水侵蚀,丹霞地貌演化也步入青年期至壮年早期阶段,以低矮的圆丘状丹霞石峰及岩洞为特征;而中部过渡地带,由于构造、水系发育均较弱,地貌演化速率慢,丹霞地貌演化处于幼年期至青年早期阶段,以石寨、巷谷、岩崖等景观为特征。  相似文献   

青藏高原腹地班戈—双湖一带晚新生代伸展构造 及动力学机制     

申添毅  王国灿 《地质通报》2013,32(1):75-85

在青藏高原腹地,晚新生代以来除发育南北向的伸展构造以外,还发现有一系列时代较新的近东西向正断层控制的伸展构造,空间上呈现出平行排列的宽缓凹槽及其间相对狭窄的山梁相互间隔的活动地貌结构特点,称这种地貌结构为"槽梁地貌"。数字高程模型(DEM)的研究表明,研究区近东西向的伸展构造在地貌上切割了近南北向的双湖盆地。结合断层运动学、年代学及盆地沉积作用的研究,认为近东西向的伸展构造的发育最早可能始于中新世,与近南北向的伸展构造交织发育,断裂的活动性在第四纪随着高原腹地海拔抬升得到了显著的增强。青藏高原隆升后重力作用导致了不同方向断陷盆地的发育。  相似文献   

安徽齐云山丹霞地貌成因   总被引：1，自引：0，他引：1  

马春梅  朱诚  彭华  ZHENG Chaogui  XIANG Fusheng  SUN Yufei  HU Jiyuan  ZHU Guanghui  LU Jianjun  CHENG Guanghua 《地理学报(英文版)》2006,16(1):45-56

According to the study of some local scholars (Peng Hua et al., 2000), over 400 sites of Danxia landform have been already discovered in China. Chen Guoda (1935), Zeng Zhaoxuan et al. (1978), Huang Jin et al. (1992; 1994; 1996) and Peng Hua et al. (1998; …  相似文献   

Quantifying sediment storage in a high alpine valley (Turtmanntal,Switzerland)     

Jan‐Christoph Otto  Lothar Schrott  Michel Jaboyedoff  Richard Dikau 《地球表面变化过程与地形》2009,34(13):1726-1742

The determination of sediment storage is a critical parameter in sediment budget analyses. But, in many sediment budget studies the quantification of magnitude and time‐scale of sediment storage is still the weakest part and often relies on crude estimations only, especially in large drainage basins (>100 km²). We present a new approach to storage quantification in a meso‐scale alpine catchment of the Swiss Alps (Turtmann Valley, 110 km²). The quantification of depositional volumes was performed by combining geophysical surveys and geographic information system (GIS) modelling techniques. Mean thickness values of each landform type calculated from these data was used to estimate the sediment volume in the hanging valleys and the trough slopes. Sediment volume of the remaining subsystems was determined by modelling an assumed parabolic bedrock surface using digital elevation model (DEM) data. A total sediment volume of 781·3×10⁶–1005·7×10⁶ m³ is deposited in the Turtmann Valley. Over 60% of this volume is stored in the 13 hanging valleys. Moraine landforms contain over 60% of the deposits in the hanging valleys followed by sediment stored on slopes (20%) and rock glaciers (15%). For the first time, a detailed quantification of different storage types was achieved in a catchment of this size. Sediment volumes have been used to calculate mean denudation rates for the different processes ranging from 0·1 to 2·6 mm/a based on a time span of 10 ka. As the quantification approach includes a number of assumptions and various sources of error the values given represent the order of magnitude of sediment storage that has to be expected in a catchment of this size. Copyright © 2009 John Wiley & Sons, Ltd.  相似文献   

汶川8.0级地震发震断层的累积地震位错研究   总被引：1，自引：0，他引：1  

王林  田勤俭  马保起  张世民  郝凯  余建强 《地震地质》2008,30(4):1012-1022

2008年5月12日,四川省汶川县内发生MS8.0地震。此次地震沿龙门山中央断裂产生1条长达200km的同震地表破裂带。文中选择位于地震地表破裂带北段的南坝镇、凤凰村以及南段的映秀镇这3个地点,以被断层错断的河流阶地为研究对象,对多级阶地面上的地震地表破裂及断层陡坎地貌进行了野外实测工作。经过测量数据的计算和分析,得到了各级阶地上断层陡坎的高度,该值即为该阶地记录的地震断层的累积垂直位错量。若以本次地震的垂直位错量作为古地震位错量的均值,则可计算得到每级阶地累积的地震次数。研究结果表明,各点T1阶地形成以来仅经历过1次事件,即本次地震事件;T2阶地形成以来约经历了5次事件;T3阶地形成以来约经历了9～11次事件;T4阶地形成以来约经历了20次事件。在本文研究的基础上,结合前人的阶地测年数据,则可获得古地震复发间隔的可靠数据  相似文献   

杭州湾南岸平原海蚀地貌的发现及意义     

李长安  王伟  侯红星  祝晓松  孙永辉 《地质论评》2022,68(1):287-292

杭州湾南岸是我国近代海岸线变化最大的海岸带之一.前人曾利用史料、遥感、土地利用等手段对这一带岸线的变化进行过大量的研究.最近,笔者等在慈溪市滨海平原中距海岸线2～3 km的二座孤山—伏龙山和海王山发现了海蚀崖、海蚀沟、海蚀穴等海蚀地貌,从而提供了对历史海岸线位置有明确指示意义的地质地貌证据.分析认为此乃20世纪60年代...  相似文献   

Influence of climate and tectonic movements on granite landforms in China     

CHEN Yixin  CUI Zhijiu  YANG Jianqiang 《地理学报》2009,19(5):587-599

Present granite landform characteristics and distribution are the integrated result of climate, tectonics and lithology. Various types of granite landforms in China signify climate zonality and differential vertical movement of earth surface, while published research results on Chinese granite landforms are very rare, especially in international journals. Based on the process analysis of chemical weathering and physical disintegration, four granite landform regions in China are classified according to the present climate regime. On the Tibetan Plateau, the cold and freezing climate induced periglacial landscapes; the northeast region is characterized by physical disintegration and low round mounds are widespread; in the northwest region controlled by arid climate, wind-carved minor landscapes are extremely prominent. The most spectacular granite landscapes in China are presented in southeast as a result of longtime chemical weathering under humid and warm conditions, as well as the differential uplift after Neogene. Correlating the weathering crust in southern China, Tibetan Plateau and India, a possible unified planation surface in Neogene is proposed. With corestones as indicators of original weathering front, the differential uplift extent of dissected planation surfaces can be estimated. At least three landforms implying uplift can be identified in southeastern China, with elevations of 300–400 m, 2000 m and 3600 m above the sea level respectively.  相似文献