排序方式： 共有14条查询结果，搜索用时 15 毫秒
1.
2.
3.
4.
三维模型产品的验收方法及问题浅析 总被引：1，自引：1，他引：0
目前,城市三维模型在全国许多地区逐步建设起来,针对基于基础测绘资料加工的三维模型产品、生产流程,总结检查经验,探讨产品的验收方法和影响产品的因素。 相似文献
6.
The Hengshan area in Shaanxi Province is located at the transitional junction of the Loess Plateau and the Mu Us sandy land in China. It is sensitive to environmental changes and has formed a unique paleoaeolian sand loess paleosol sequence. In this study, the L3 and S3 loess paleosol strata of the Liushumao section in Hengshan were selected for the analysis of the element content and related geochemical parameters in soil samples, to systematically explain the chemical weathering intensity and environmental evolution information recorded by the element geochemical index parameters during the L3 loess accumulation and S3 paleosol development in the Hengshan area. The results show that the major elements in the Liushumao section are mainly SiO2, Al2O3 and CaO. There are differences in the content of major elements in loess layers (L3-1, L3-2), paleosol layers (S3-1, S3-2), and aeolian sand layers (L3F, S3F). The contents of Al2O3 and Fe2O3 are the highest in the paleosol layer of the section, the content of CaO is the highest in the loess layer, and the content of Na2O is the highest in the aeolian sand layer. The CIA and Na/K values of the section samples reveal that the loess-paleosol layer are in the stage of primary chemical weathering, and the aeolian sand layer has not entered the stage of chemical weathering. The high values of CIA, Rb/Sr ratio, and magnetic susceptibility in the Liushumao section indicate the strengthening of weathering and pedogenesis, the relatively warm and humid climate in this period, the increasingly strong summer monsoon, and the fixed contraction of the Mu Us sandy land. The high values of the ratio of silicon and aluminium (Sa) and > 63 μm particle content indicate the occurrence of strong winter monsoon, which led to the activation and expansion of the sandy land under the effect of dry and cold climate. One extremely cold period, two cold periods, and a relatively warm period occurred in the L3 loess accumulation period, while two warm periods and one cold period occurred in the S3 paleosol development period. The change of element geochemical indicators in the Liushumao section revealed that the climate change in the Hengshan area was mainly affected by the change of strength of the East Asian winter and summer monsoon, which is generally consistent with other climate change records in North China. The study results provide more evidence for exploring the climate and environmental changes in the transitional area of the Loess Plateau and Mu Us sandy land in China. © 2023, Editorial office of PROGRESS IN GEOGRAPHY. All rights reserved. 相似文献
7.
多山地区SAR数据的预处理是实践应用中的关键。基于GAMMA平台,研究微波遥感数据的辐射定标、多视处理、滤波、正射校正和辐射校正等预处理方法和流程,为有关研究的进一步开展提供基础数据。辐射定标使SAR图像真实地反映地面目标后向散射特性;Gamma-map滤波既能很好地平滑图像去除斑点噪声,又能很好地保持边缘和纹理细节,目视效果较好;基于DEM模拟影像的正射校正方法原理清晰,效果较好;辐射校正可以消除因地形引起的辐射畸变。 相似文献
8.
靖边波浪谷丹霞地貌区是近年来国内外地学界的新发现和持续关注点。论文通过野外地质调查、粒度分析,岩石地球化学分析等研究,探讨红色砂岩地球化学特征、沉积环境、物源性质等相关问题。研究表明：红色砂岩以中—细砂为主,SiO2和Al2O3含量之和在85%以上,沉积环境为河湖相,为水动力中等,水面较浅的河流入湖三角洲河口区地带,而不具有目前一些学者通过宏观观察提出的该砂岩为沙漠相沉积特征。沉积阶段气温较高,存在暖干与暖湿的多次变化。地球化学分析表明红色砂岩地球化学类型为长石砂岩和亚长石砂岩,物源可能来自于盆地内部隆起或再旋回造山带所提供的富石英质沉积岩。 相似文献
9.
鄂西高坪龙骨洞地层形成环境的研究 总被引：5，自引：0，他引：5
鄂西龙骨洞保存有早更新世早期的地层,并产早期人类化石和巨猿化石以及石器。通过对这套地层的形成环境的研究表明:沉积物形成于水动力条件较弱的暗河环境,期间发生过几次水体干涸事件,形成钙板层。根据沉积环境的特点,龙骨洞的地层可划分为4部分:第一部分是剖面的底部,在洞穴沉积物的形成初期,沉积物粒度较粗,形成水动力较强的暗河环境;第二部分是钙板层或强钙质胶结层的形成,表明洞穴处于干涸或水很少的环境;第三部分是地层的主体部分,以粘土和亚粘土为主,形成于弱水流的暗河环境,化石主要产自这部分;第四部分是剖面的顶部,为钙板层,洞穴干涸。洞中的化石和石器部分是被水流带入洞中沉积形成的,部分为人类和巨猿在洞中生存时留下的。 相似文献
10.
通过对观测结构的研究探讨了观测的基本机理;提出了观测结构的6种形态,从根本上分析了病态性存在的原因.利用观测矩阵的QR分解结果,将对观测结构的分析过渡到对上三角矩阵的分析与计算.由此对观测结构进行了深入分析与度量,能够对观测结构的各种形态进行推断,进而对系统的Ⅰ类及Ⅱ类病态性作出推断与估计. 相似文献