Application of Digital Elevation Model in the geological mapping of the coastal plain of Tianjin
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摘要: 天津市滨海平原地区地势平坦,地貌类型不易划分,沉积物粒度较细,遥感解译精度及实地可识别性差,按照传统的地质调查方法开展填图,图面表达效果不佳。数字高程模型(Digital Elevation Model, DEM)是地形的数字化表达,具有一般地形图无法表达的三维可视化信息,能够真实反映地形地貌特征。在开展天津滨海平原地质填图过程中,通过建立研究区DEM,并结合路线地质调查、槽型浅钻施工、样品测试分析,进行了地貌单元划分,将浅地表沉积物划分为河流、海侵和三角洲3个沉积体系: 河流沉积体系包含边滩(曲流砂坝)、充填河槽(牛轭湖)、决口扇、天然堤、洪泛盆地和湖沼沉积微相; 海侵沉积体系包含海滩脊、越岸扇、高潮坪和残留潟湖沉积微相; 三角洲沉积体系主要为三角洲前缘沉积。通过与不同类型遥感解译结果进行对比分析可知,DEM可充分弥补遥感影像的不足,对浅地表沉积物进行详细的成因类型划分,提升对浅地表地质作用过程的认知程度,较好地指导野外地质填图。将高精度DEM数据应用于第四系覆盖区地质填图,可以大大提高填图精度及效率,为城市生态安全保障、国土空间规划、产业结构布局等提供基础地质依据。Abstract: Tianjin coastal plain is flat and its landform is not easy to be divided. The grain size of the sediments is fine, with poor remote sensing interpretation accuracy and field identification, which leads to weak geological map expression effect by the traditional geological survey method. Digital Elevation Model (DEM) is a digital representation of the topographic surface and it has 3D visual information that cannot be expressed by the general topographic map, which can truly reflect the features of the landform. The authors divided the geomorphic units of shallow sediments during the geological mapping process of Tianjin coastal plain based on DEM and the geological survey of the route, the construction of the shallow groove drilling and the sample testing. The shallow sediments can be divided into three sedimentary systems: fluvial sedimentary system, transgression sedimentary systm and deltaic sedimentary system. The fluvial sedimentary system includes several genetic types of point bar, oxbow lake, crevasse splay, natural levee, flood basin and lake marsh. And the transgression sedimentary system can be divided into beach ridge, overland fan, high tide flat, residual lagoon, while the deltaic sedimentary system includes the delta front. DEM can fully make up for the shortage of remote sensing images after the comparative analysis with the results of remote sensing interpretation of different types. Besides, DEM can also be used for the detailed genetic classification of the shallow sediments and improve the cognition about shallow geological process, which will guide the field mapping. The application of high-precision DEM data to the geological mapping on the covered areas of quaternary system can greatly improve the mapping accuracy and efficiency, and provide basic geological support for urban ecological security, territorial space planning and industrial structure layout.
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[1] 薛重生. 遥感技术在区域地质调查中的应用研究进展[J].地质科技情报,1997,16(增刊1):16-23. [2] 闫柏琨,董新丰,王喆,等.航空高光谱遥感矿物信息提取技术及其应用进展——以中国西部成矿带调查为例[J].中国地质调查,2016,3(4):55-62. [3] 杨清华,陈华,路云阁,等.全国边海防地区基础地质遥感调查[J].中国地质调查,2017,4(3):1-9. [4] 刘智,黄洁,孙小飞,等.基于GF-1影像的西藏亚东地区构造解译研究[J].中国地质调查,2017,4(3):17-23. [5] 侯德华,张立国,王硕,等.基于GF-2影像西藏桑耶地区岩性-构造遥感解译[J].中国地质调查,2018,5(5):66-73. [6] 黄帅堂,陈建波,阿里木江·亚力昆,等.基于数字高程模型的南天山地貌特征研究[J].高原地震,2018,30(3):17-24,6. [7] 胡昌龙,易燕.数字高程模型DEM及其显示[J].黑龙江科技学院学报,2007,14(4):233-236. [8] 刘少峰,王陶,张会平,等.数字高程模型在地表过程研究中的应用[J].地学前缘,2005,12(1):303-309. [9] 贾世真,赵伟亮.多角度卫星影像的DEM制作[J].测绘与空间地理信息,2016,39(6):145-147. [10] 谢飞,吴杰.Pleiades卫星立体像对提取数字高程模型的试验研究[J].城市地理,2017(22):132-133. [11] 陈隽敏. 资源三号正射影像和DEM制作及电力工程适用性分析[J].南方能源建设,2015,2(增刊1):207-211,229. [12] 李振洪,李鹏,丁咚,等.全球高分辨率数字高程模型研究进展与展望[J].武汉大学学报:信息科学版,2018,43(12):1927-1942. [13] 明国辉,委民正.SURF算法在无人机倾斜摄影测量三维建模中的应用[J].测绘工程,2017,26(9):41-45. [14] 张会,赵民.无人机影像数据提取大比例尺DEM的方法研究[J].测绘与空间地理信息,2018,41(5):195-197,201. [15] 戴伟琦,李欢,龚政,等.无人机技术在潮滩地貌演变研究中的应用[J].水科学进展,2019,30(3):359-372. [16] 常直杨,孙伟红,王建,等.数字高程模型在构造地貌形态分析中的应用现状及展望[J].南京师大学报:自然科学版,2015,38(4):129-136. [17] 许丽,李江海,刘持恒,等.基于数字高程模型(DEM)的可可西里地貌及区划研究[J].北京大学学报:自然科学版,2017,53(5):833-842. [18] 李美萍,春喜,胡和达来,等.基于数字高程模型的查干淖尔湖泊变迁研究[J].内蒙古师范大学学报:自然科学汉文版,2012,41(5):537-543. [19] Xu Q M,Yuan G B,Yang J L,et al.Plio-Pleistocene magnetostratigraphy of northern Bohai Bay and its implications for tectonic events since ca. 2.0 Ma[J].J Geodyn,2017,111:1-14. [20] 靳宝珍,杨云霄,邱京卫,等.天津市古潜山奥陶系岩溶裂隙发育规律研究[J].中国地质调查,2019,6(2):94-99. [21] 黄猛,李明辰,樊航宇,等.渤海湾西北岸QHJ01孔记录的晚新生代气候与沉积环境演化[J].地质学报,2019,93(4):899-914. [22] 王强,李凤林.渤海湾西岸第四纪海陆变迁[J].海洋地质与第四纪地质,1983,3(4):83-89. [23] 王宏,范昌福,李建芬,等.渤海湾西北岸全新世牡蛎礁研究概述[J].地质通报,2006,25(3):315-331. [24] 王强,袁桂邦,张熟,等.渤海湾西岸贝壳堤堆积与海陆相互作用[J].第四纪研究,2007,27(5):775-786. [25] 徐利淼. 天津滨海地区地貌特征与分类系统[J].天津师范大学学报:自然科学版,1995,15(4):54-59. [26] 张艳,孙杰,于长春,等.基于多源遥感数据的第四系覆盖物分类方法研究:以内蒙古旗杆甸子幅1:5万填图试点为例[J].地质科技情报,2019,38(2):281-290. [27] 陈星,贾晓青,张学斌.监督分类在第四纪堆积物遥感解译中的应用——以天津武清地区为例[J].电子制作,2013(4):54-55,69. -
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