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251.
湖南省地势图编制关键技术研究 总被引:1,自引:0,他引:1
地势图是一种着重表示地势起伏、植被分布、水系特征与分布规律的专题地图,强调表现地面的高低起伏、倾斜程度及与其他地理要素的对比关系,以及水系的分布特征和形态特征,并适当表示其地表的植被与土质。本文以湖南省为例,在基于DEM数据上,收集研究区域的资料并进行分析,采用分层设色法表示地势图,关键技术在于如何确定设色原则和建立色层表。 相似文献
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《Comptes Rendus Geoscience》2019,351(5):395-405
We aimed to determine variations in stress regimes during the youngest Variscan deformations in the northern part of the Bohemian Massif. For this purpose, we calculated the orientation of the principal stress and strain axes for kink folds observed in the metamorphic envelope of the Karkonosze Granite, using two methods: 1) the traditional method, incorporating structural diagrams (for conjugate kink folds only), and 2) butterfly diagram analysis. The use of both methods enabled us to determine the stress regime, based not only on conjugate but also on monoclinal kink bands. The obtained results prove that butterfly diagram analysis, when applied to monoclinal kink folds, yields reliable results, especially when calibrated using the internal friction angle (Ф) calculated for the conjugate structures.We identified two generations of kink folds: 1) an older one, developed under sublatitudinal shortening and most probably related to the Early Carboniferous terminal stages of the northwest-directed thrusting of the metamorphic units, and 2) a younger one; produced by north-south Variscan Carboniferous compression, and the emplacement and subsequent doming of the Karkonosze Granite. This is the first study on brittle-ductile structures observed commonly in the metamorphic units of the Bohemian Massif, showing their relation to the granitoid intrusion and complementing the tectonic models that usually omit kink folds. 相似文献
254.
济阳坳陷石炭二叠系暗色泥岩微量元素赋存特征及其地质意义 总被引:1,自引:0,他引:1
在对Sc、Co、Ni、Ga、Rb、Sr、Mo、Ba等微量元素进行电感耦合等离子体质谱(ICP-MS)测试和对泥岩粘土矿物进行x射线衍射相对定量分析的基础上,结合骨架砂岩岩石薄片镜下观察结果,采用Sr-Rb—Ba-Sc多元素标准化图解,分析了济阳坳陷石炭二叠系暗色泥岩微量元素赋存特征及其所指示的海陆沉积相变化、火山事件、物源等方面的地质意义。研究结果表明:(1)济阳坳陷暗色泥岩微量元素含量普遍比华北地台同时期沉积物高(Ba除外)。(2)济阳坳陷本溪组和太原组下部发育海相沉积以及上石盒子组曾发生数次规模较大的海侵,表现为在Sr-Rb-Ba-Sc标准化图解中sr上扬,或Rb-Ba—Sc近似呈直线;局限台地相沉积可能造成其上部相邻地层泥岩中Rb、Sr发生异常。(3)在济阳坳陷石炭二叠系骨架砂岩岩石薄片中观察到自形石英、港湾状石英、聚片双晶长石、保存较好的挠曲状云母,推测石炭二叠系受到多次火山作用影响;Sr-Rb—Ba-Sc标准化图解中Rb异常可能揭示火山作用的影响,而Rb异常的泥岩样品通常高岭石含量非常高(〉70%),且伊利石含量非常低(〈5%)。(4)Rb-Ba-Sc标准化图解显示济阳坳陷石炭二叠系物源区可能是华北地台北部的古老岩体,母岩岩浆来自上地壳。 相似文献
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针对以欧氏距离作为放大因子对电子地图进行放大裁剪引起的信息失衡问题,提出了采用地理多要素Voronoi图相邻关系的地图放大裁剪方法,可有效避免以欧氏距离作为地图放大因子的地图信息失衡问题。将电子地图中的地理要素分为点、线、面,对于点要素,构建它的Voronoi图;对于非点要素,即线和面要素,构建它们的近似Voronoi图,当用户对电子地图中感兴趣地理要素目标放大时,只需要提取该目标的多要素Voronoi图相邻要素的近似Voronoi图,并计算它们的最小外包矩形,将最小外包矩形区域用于最终的地图放大裁剪区域,则可较好地顾及用户感兴趣地理要素目标周围的地理要素信息,可提高地图的易读性。采用本文方法对某区域电子地图进行了试验,结果表明,地理多要素Voronoi图相邻关系的地图放大裁剪方法能够较好地顾及目标周边地理要素信息,避免了以欧氏距离为放大因子的地图信息失衡。 相似文献
258.
Changping Plain, located in the northwest of Beijing, has become an important groundwater recharge area for the Beijing Plain and an important source for the urban water supply. In this study, groundwater samples were collected during the dry and wet seasons in 2015 from 24 monitoring wells distributed in Changping Plain. A Piper-Tri-linear diagram, a Schoeller diagram, a Gibbs diagram, and the isotope technique were used to investigate the temporal and spatial variations in the concentrations of groundwater hydrochemicals and the sources of groundwater recharge. The results indicated: 1) seasonal variations in the concentrations of HCO3-, Ca2+, and Na+ were significant; the spatial variations of these ions were more dramatic in the dry season than in the wet season due to the dilution effect of precipitation; 2) Most groundwater samples had a HCO3-Ca-Mg based hydrochemical type and a few had a HCO3-Na-K based hydrochemical type; the hydrochemical type tended to evolve from HCO3-Ca-Mg based to HCO3-Na-K based in some monitoring wells that showed distinct seasonal variation; 3) the groundwater in the study area originated mainly from atmospheric precipitation, and it is affected by evaporation and concentration processes. 相似文献
259.
The hydrochemistry of alpine lakes reflects water characteristic and its response to climatic change. Over 300 water samples had been collected from 52 sites of 5 lakes and 7 inflowing rivers in the Yamzhog Yumco Basin, South Tibet, during 2009–2014, basing which the hydrochemical regime and its mechanism were analyzed along with the adoption of hydrological investigations in 1979 and 1984 as well. Results revealed that the waters were hard with weak alkalinity for the Yamzhog Yumco Basin. Most of them were fresh, and the rest were slightly saline. The hydrochemical types of 5 lakes (i.e., Lake Yamzhog Yum Co, Puma Yum Co, Bajiu Co, Kongmu Co, and Chen Co) were SO4 2––HCO3 ––Mg2+–Na+, HCO3 ––SO4 2––Mg2+–Ca2+, SO4 2––Mg2+–Na+, SO4 2––HCO3 ––Ca2+, and SO4 2––Na+–Mg2+–Ca2+, respectively. As for rivers, HCO3 – and SO4 2– were the major anions, and Ca2+ was the dominant cation. Lake Yamzhog Yum Co, the largest lake in the basin, exhibited remarkable spatial variations in hydrochemistry at its surface but irregular changes with depth. The weathering of evaporates and carbonates, together with evaporation and crystallization, were the major mechanisms controlling the hydrochemistry of waters in the Yamzhog Yumco Basin. Global warming also had significant impacts on hydrochemical variations. 相似文献
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