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31.
大别山北麓钼矿找矿重大进展及其矿床地质特征研究 总被引：5，自引：0，他引：5
在总结近年来钼矿勘查成果的基础上,综合论述了大别山钼矿床的基本特征和成矿规律.钼矿带呈北西向狭长带状展布,钼矿床的形成与燕山期中酸性浅成-超浅成小花岗岩斑岩体有关,钼矿床直接产于岩体内外接触带及其附近;矿床类型主要为斑岩型,少量矽卡岩型、热液脉型.结合Re-Os同位素精测年龄数据,确定了大别山钼矿床的成矿时代主要集中在... 相似文献
32.
Crossing Honghe fracture in Yunnan Province two measuring profiles were set up, each measuring profile consisted of 8 observing
sites. Three component geomagnetic variation observations were carried out continuously and simultaneously along each profile.
Induction arrows were calculated for the periods from 8 min to 60 min. There exists a reversal axis of induction arrow between
Eryuan, Xiaguan, Weishan, Mejiang and Yongping, Yunxian, Lincang, Simao. The real arrows reverse from one side of the axis
to another side and the magnitude of the real induction arrows attenuates with increase in distance from the axis, the attenuation
in northeast side of the axis is slightly less than that in southwest side. The real induction arrows of shorter periods are
greater than those of longer periods at most of the observing sites. According to the features of the real induction arrows
and by use of numerical calculation we tried to look for the restriction which was to be attached to the possible high conductivity
zone in the area under investigation. It shows that there is a high conductivity belt west of Honghe fracture which tilts
northeastward and there is a high conductor cover over the high conductivity belt beneath most of the observing sites
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,14, 201–210, 1992. 相似文献
33.
详细介绍榆树地震台地电场观测系统的运行状况,从数据完整率、静日、扰日变化形态以及相关系数、差值等方面对观测系统运行进行综合评价,结果表明:榆树地震台地电场观测系统运行稳定可靠,能够记录到震前地电场异常变化,可以为地震预测预报研究提供一定依据。 相似文献
34.
面对日益增长的空间数据,网络环境较差的地图、地理信息应用服务系统面临着存储容量有限、地理空间数据格式不开放的挑战。而现有的许多地理空间数据存储依赖于平台,还需要克服跨平台带来的问题,亟需研究设计统一的数据存储标准来解决空间数据格式不一致、不同GIS平台数据转换过程复杂等问题。考虑到不同系统GIS平台、GIS应用程序间数据格式的差异,本研究基于GeoPackage（GPKG）数据容器存储标准,采用Qt 5.2.0+VS2010开发平台,C++编程语言,通过三层架构编程模式研发了GIS数据存储格式的检查软件,以解决数据格式不统一的问题。该软件利用批量数据库查询,快速地实现了核心功能项、可选功能项、注册扩展功能三大类等超过百项功能文件格式的检查,并输出详细的检查结果,为GIS数据格式存储标准化提供支持和帮助,可有效解决不同GIS平台、不同GIS应用程序数据共享时面临的格式不一致问题,简化了数据转换的步骤。 相似文献
35.
针对GIS数据的多维、海量、动态性等特点,本文设计了基于四叉树和双缓存机制的GIS动态数据可视化模型,并详细地介绍并阐述该模型的数据存储规格和数据可视化方法及其特点。基于四叉树索引结构和多线程双缓存机制,构建GIS动态数据可视化模型,探讨多线程分层绘制动态对象方法和GIS空间数据库实时更新方法,实现GIS海量数据的动态化、序列化、实时可视化表达。并测试对比了常见可视化算法与本算法之间的显示效率,发现本研究算法针对多种GIS图形类型、大数据量GIS数据显示,均有较高的效率提升,实验证明该方法稳定可行,可为其他GIS动态数据的可视化提供参考。 相似文献
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37.
Gravity Anomalies of Arbitrary 3D Polyhedral Bodies with Horizontal and Vertical Mass Contrasts 总被引：10，自引：2，他引：8
Zhengyong Ren Chaojian Chen Kejia Pan Thomas Kalscheuer Hansruedi Maurer Jingtian Tang 《Surveys in Geophysics》2017,38(2):479-502
During the last 15 years, more attention has been paid to derive analytic formulae for the gravitational potential and field of polyhedral mass bodies with complicated polynomial density contrasts, because such formulae can be more suitable to approximate the true mass density variations of the earth (e.g., sedimentary basins and bedrock topography) than methods that use finer volume discretization and constant density contrasts. In this study, we derive analytic formulae for gravity anomalies of arbitrary polyhedral bodies with complicated polynomial density contrasts in 3D space. The anomalous mass density is allowed to vary in both horizontal and vertical directions in a polynomial form of \(\lambda =ax^m+by^n+cz^t\), where m, n, t are nonnegative integers and a, b, c are coefficients of mass density. First, the singular volume integrals of the gravity anomalies are transformed to regular or weakly singular surface integrals over each polygon of the polyhedral body. Then, in terms of the derived singularity-free analytic formulae of these surface integrals, singularity-free analytic formulae for gravity anomalies of arbitrary polyhedral bodies with horizontal and vertical polynomial density contrasts are obtained. For an arbitrary polyhedron, we successfully derived analytic formulae of the gravity potential and the gravity field in the case of \(m\le 1\), \(n\le 1\), \(t\le 1\), and an analytic formula of the gravity potential in the case of \(m=n=t=2\). For a rectangular prism, we derive an analytic formula of the gravity potential for \(m\le 3\), \(n\le 3\) and \(t\le 3\) and closed forms of the gravity field are presented for \(m\le 1\), \(n\le 1\) and \(t\le 4\). Besides generalizing previously published closed-form solutions for cases of constant and linear mass density contrasts to higher polynomial order, to our best knowledge, this is the first time that closed-form solutions are presented for the gravitational potential of a general polyhedral body with quadratic density contrast in all spatial directions and for the vertical gravitational field of a prismatic body with quartic density contrast along the vertical direction. To verify our new analytic formulae, a prismatic model with depth-dependent polynomial density contrast and a polyhedral body in the form of a triangular prism with constant contrast are tested. Excellent agreements between results of published analytic formulae and our results are achieved. Our new analytic formulae are useful tools to compute gravity anomalies of complicated mass density contrasts in the earth, when the observation sites are close to the surface or within mass bodies. 相似文献