淮南舜耕山奥陶系古岩溶发育特征及古地貌恢复??     

杨婷婷  许光泉  张著  李浩  章晋升  贺彪 《地质论评》2024,(1):2024010024-2024010024

研究古岩溶发育特征及古地貌恢复对于华北煤田岩溶水害防治具有重要指导意义。以华北板块南缘淮南舜耕山奥陶系古岩溶为对象，采用野外地质踏勘、分段剖面测量以及残余厚度法等工作方法，揭露了古岩溶发育特征和恢复基岩面剖面起伏形态，并结合现代岩溶理论，从形成条件的角度剖析不同岩溶带的空间变化规律。本文认为马家沟组主要发育大型岩溶缝洞，内部充填物少，而萧县组沿层面发育层间岩溶，充填岩溶角砾，且内部充填方解石由东向西逐渐增多。舜耕山奥陶系古岩溶发育程度自东向西、自上至下逐步减弱。该地区奥陶系古地貌呈东高西低，可划分为残丘、缓坡、陡坡和洼地等4个三级岩溶地貌单元。通过对古岩溶地质条件、古水流径流方式以及古岩溶发育特征等因素的考察与分析，古岩溶地貌从上至下可分为表层岩溶带、垂向渗流带、水平潜流带和深部缓流带。其中，残丘和缓坡的表层岩溶带和垂向渗流带岩溶最为发育，在沉积层面间常发育成大型岩溶缝洞，且在地下水流发生改变时，易形成岩溶塌陷。  相似文献   

一种遥感数据自适应剖分分块渐进传输方法     

吴尚竹  程承旗 《地理信息世界》2016,(2):1-8

针对当前遥感影像数据量巨大的特点,如何利用相对有限的带宽来保障遥感数据高效、灵活的传输与服务是遥感数据应用的一个关键问题。本文基于Geo SOT全球剖分与编码体系提出了一种对网络带宽、用户请求和元数据信息自适应的遥感数据剖分分块方法,并设计了基于优先级函数的面片渐进传输方法,实现根据目标的变化量信息和导航路径偏移信息估计面片对用户的重要性,从而渐进传输感兴趣数据的功能。通过模拟实验证明该方法可以满足遥感数据自适应剖分、灵活传输应用的需求。  相似文献   

冀北侏罗纪地层划分与《中国地层表》的对应关系     

张路锁  杨森丛  范和平  张树胜  谢明忠  唐锦秀  孙跃民  尚洪田 《地质论评》2016,62(4):840-848

中国地层委员会2014年发布的《中国地层表》,在年代地层和岩石地层划分等方面和原地层表相比都有很大变化,作者在对该表进行初步解读的基础上,将冀北侏罗系与其做了对比,以期引起广大同行的关注和重视。作者认为:河北省北部的下花园组时代应由早—中侏罗世改为中侏罗世,层位与西山窑组一致;南大岭组与八道湾组层位相当;九龙山组和髫髻山组的层位相当于头屯河组;后城组时代为晚侏罗世,同层位地层是土城子组;张家口组划归下白垩统。  相似文献   

GIS岛多边形三角剖分算法     

芦军军  田正华 《测绘与空间地理信息》2016,(11)

结合Delaunay三角剖分原理,在多边形顶点关系的基础上,通过对多边形从外向内间隔相邻级环间的三角剖分,来实现岛多边形的剖分算法。算法涉及图形相交、相邻、相离、包含等几何关系分析,以及Delaunay三角形构建等过程。对图形几何关系判断和三角形构建等过程进行了优化处理,提高了岛内三角剖分的精度和速度,解决了GIS制图中存在的"岛中岛"等复杂几何图形的剖分问题,可以对任意凹凸多边形实现快速三角剖分。首先获取并存储shape文件中多边形的空间坐标数据,然后基于该算法在VC++开发环境中完成岛多边形的三角剖分和显示。通过对不同形状的岛多边形反复测试表明,该算法的三角剖分结果均可达到最优,且效率较高。  相似文献   

Sequence subdivision and development characteristics of low-accommodation non-marine basins: a case study of the Yanchang Formation in the Ordos Basin     

S. Fu  Y.-Z. Li  Y.-R. Guo  X.-M. Xu  J.-J. Liu 《Australian Journal of Earth Sciences》2018,65(6):823-850

The third-order sequences of the Yanchang Formation in the Ordos Basin were determined by a comprehensive analysis of surface outcrops, core, logging and seismic data. Natural gamma curves were studied by the band-pass method. The hidden stratigraphic sequence and six lithological cycles were extracted. By examining sequence boundaries and lithological cycles, we identified six third-order (including SQ1, SQ2, SQ3, SQ4, SQ5 and SQ6) and three second-order sequences in the Yanchang Formation. The sequence stratigraphy of the Ordos Basin was found to have the following special development characteristics: (1) the third-order sequence growths were totally stable, and the thickness of the Ordos Basin was relatively stable; (2) thick sand bodies did not form in lowstand systems because of underdeveloped slope breaks; (3) the third-order sequences had diverse features at different sedimentary periods; (4) the distribution of the depositional systems had various characteristics in different tectonic belts, and the entire sequence had the filling characteristics of multiprovenances and multicycles. The low-accommodation Ordos Basin in the Upper Triassic was limited by slow subsidence, gentle basement paleorelief, stable tectonic settings and sufficient sediment supply. The characteristics of the basin included stable developed sequences, limited preserved lowstand systems tracts, multiple depocentres and subsiding centres, development of many delta systems in the north and south of the basin controlled by the gradient of the basement paleorelief, and laterally stretching sediments. Results further indicated that the controlling factors of the third-order stratigraphic sequences of Yanchang Formation in the low-accommodation lacustrine Ordos Basin included sediment supply (provenance), climate and lake-level fluctuation. Overall, our case study indicated that the development characteristics and controlling factors of sequence stratigraphy in a low-accommodation lake basin provided a comprehensive method of establishing the sequence stratigraphic framework of a low-accommodation non-marine basin. Our results also predicted that the SQ3, SQ4 and SQ5 of the Qiaochuan and Zhidan areas favoured oil and gas prospecting of the Yanchang Formation.  相似文献   

A model of submarine channel-levee evolution based on channel trajectories: Implications for stratigraphic architecture   总被引：3，自引：0，他引：3  

Zoltán SylvesterAlessandro Cantelli 《Marine and Petroleum Geology》2011,28(3):716-727

Channel-levee systems are frequently interpreted as having a long history of cut-and-fill by channel-shaped features of different scales. Results from a simple geometric model based on a centerline migration algorithm combined with a vertical channel trajectory show that an incising-to-aggrading trajectory of a single channel can produce realistic morphologies similar to systems observed on the seafloor and subsurface, including features such as a basal erosional surface, coeval inner and outer levees, internal erosional boundaries, and terraces draped by inner levee deposits. Channel migration results in composite erosional surfaces that are distinct from topographic surfaces, and their formation does not require larger than usual erosional flows. Many submarine channels interpreted as underfit were probably carved by flows similar to the ones that eroded and deposited the entire channel system. We suggest that the features of most submarine channel-levee systems do not require large temporal variations in flow magnitude but can be explained by a simpler model whereby incision, migration and aggradation of a single channel form over time results in an apparently complex system.  相似文献   

山东地区山西组地层特征研究     

殷天涛  李守军  赵秀丽 《山东国土资源》2014,30(12)

山东山西组是煤和煤成气的重要富集层位。以综合地层学理论为核心,以岩石地层学、生物地层学、层序地层学等方法,将山东地区二叠系典型剖面淄博与鲁西(彭庄)、济阳坳陷山西组,进行对比研究,建立地层对比格架。经综合分析研究,得出山东地区山西组在纵向与横向上的变化趋势。造成这些变化的主要原因可能是晚石炭世鲁西是由东南向西北海侵。太原组上部灰岩的顶界,山西组泥岩的底部形成于突发性海侵向海退转化时。  相似文献   

位置主导的空时记录体系架构设计     

关丽  吕雪锋 《测绘科学》2012,(1):104-108

针对传统空间数据记录体系在全球尺度空间数据管理中存在的弊端,如数据图幅范围缺乏大范围或全球统一标准管理、数据跨图幅接边处理复杂等问题,本文构建了一套以空间位置记录为核心、时间为属性、计算机集群为存储模式的空时记录体系。在剖析了传统空间数据记录模式基础上,探讨了空时记录体系的内涵与优势,并基于全球剖分模型及其编码(GeoID编码)着重设计了空时记录体系架构和结构功能,为全球海量空间数据的管理与组织提供了技术参考。  相似文献   

西南地区气候季节划分及特征分析     

徐晓  肖天贵  麻素红 《四川气象》2010,(1):35-40

本文运用聚类分析方法对西南地区进行分区讨论,研究了各区域的气候季节及其变化特征。我国西南地区5个区域夏季和秋季的分配基本一致,而冬春两季差异明显;而降水场和温度场四季划分也有一定相关和相异性,均按照云南区-川西高原区-贵州区-四川盆地区-川东区的顺序逐级递减。  相似文献   

The Quaternary is here to stay     

D. Q. Bowen  Philip L. Gibbard 《第四纪科学杂志》2007,22(1):3-8

The proposals to drop the name Quaternary, to extend the Neogene Period to the present day, and to confirm the base of the Pleistocene at 1.8 Ma are reviewed. It is concluded that there is no scientific case for dropping the name Quaternary and that an overwhelming volume of evidence points to 2.6 Ma as the most appropriate base for the Quaternary/Pleistocene, when extensive Northern Hemisphere mid‐latitude glaciation occurred under what were essentially similar physical boundary conditions of continents, oceans, seaways and mountain ranges that characterise, and are unique to, the Quaternary. It is desirable that all stratigraphical and geochronological evidence is tied rigorously into the Global Stratigraphic Timescale. Copyright © 2007 John Wiley & Sons, Ltd.  相似文献