网络环境下分区统计地图制图子系统的设计与实现

分析了网络环境下分区统计地图表达信息的特点,根据其可视化地理统计信息的需要,运用Java Ap-plet技术,设计和开发了网络环境下交互式分区统计地图制图子系统。     

线与面之间基本拓扑关系类型在抽象过程中的等价转换

以空间拓扑关系组合推理所描述的线与面之间的拓扑关系为基础，研究了抽象过程中基本拓扑关系类型等价转换所涉及的问题；提出了成分抽象的等价转换方法，并将其运用于线与面之间基本拓扑关系类型的抽象过程中；绘制了线与面之间基本拓扑关系类型的等价转换图。     

地图自动综合知识的分类及其形式化描述

在分析了已有地图综合知识的分类和表示方法的基础上 ,提出了一种新的地图综合知识的分类方法和形式化方法 ,这种分类方法易于系统开发 ,其形式化方法便于同地图综合模型和空间数据管理相结合。     

线状要素图形综合的渐进方法研究

提出了“渐进式”线状要素的２种图形综合方法：基于三角形的纯几何渐进方法和基于图形基本单元“弯曲”的渐进方法。该方法明显优于Ｄｏｕｇｌａｓ综合方法,可以控制线的自交,使地图比例尺从离散式变成连续式,适用于地理信息系统。在兼顾特征点的情况下,其效果更佳。     

Magnetic structure of Archean Kongling Group from Yangtze craton,South China

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REE Geochemistry of VMS and SEDEX Ores in China

REE ratios and patterns for massive pyrite ore and massive cuprous pyrite ore ofthe Baiyinchang orefield are quite similar to those for quartz keratophyritic tuff and quartzalbitophyre of the same orefield. However, massive cuprous pyrite ore of the Ashele Cu-Zn de-posit is similar to basalt-diabase of the same district in REE geochemistry. Comparison of theChinese VMS ores with those from Rio Tinto, Spain and Que River, Australia, in REEgeochemistry has been made. REE ratios and patterns of bedded-massive and massive ores ofthe Changba-Lijiagou Zn-Pb deposit, the second largest SEDEX deposit in China are similarto those of their host rocks, the Qinling shales of Devonian age and the Changba adamellite.The three types of ore and their host rocks of the Dongshengmiao pyrite (pyrrhotite)-Zn-Pbdeposit have parallel REE ratios and patterns.     

微细浸染型（卡林型）金矿成矿过程中碳和有机质的作用

在众多关于黔滇桂微细浸染型（卡林型）金矿研究成果的基础上，本文通过本类型金矿含碳及有机质的特征；金能形成金属有机化合物及原子簇化合物的特征的研究。提出金以金属有机化合物形式在本区上二叠统富含生物成因有机质的煤系地层中形成预富集；在区域热变质作用中，金以气相金属有机化合物方式向上运移，蓄积在上二叠统至中三叠统各层位的背斜和穹隆部位；动力变质带的断裂活动引起物理化学突变，使金的气相金属有机化合物在构造断裂带解体、裂化从而形成了含细分散碳质的微细浸染型含金硫化物原生矿化；并探讨了主成矿期后与有机质解体有关的叠加热液活动和表生氧化作用对原生矿化的改造。从而从有机质演化角度初步建立了此类型的成矿模式     

明暗等高线自动绘制方法

从Tanaka手工绘制明暗等高线图的方法入手,分析比较了已有的几种改进方法,以Arc/Info软件为平台实现了明暗等高线的自动绘制,并对输出的几种结果进行了理论分析。     

相邻比例尺地形图之间居民地要素匹配方法研究

在研究相邻比例尺的居民地要素变化规律的基础上,提出了居民地要素匹配的新方法;以国家基本比例尺矢量地形图为实验数据,建立了街区等居民地空间目标的匹配关系.     

Investigation of Curie Point Depth in Sulu Ultrahigh-Pressure Metamorphic Belt,Eastern China

The Curie point depth of continental crust can reflect the regional tectonic pattern and geothermal structures. Analysis of magnetism is an efficient way to obtain the Curie point depth on a regional scale. This study systematically investigated the Curie point depth of Sulu (苏鲁) ultrahigh pressure (UHP) metamorphic belt (33°40'N to 36°20'N and 118°E to 120°E, ca. 60 000 km2), eastern China using aeromagnetic data. The results show that the Curie point depth of the Sniu region varies from 18.5 to 27 kin. The shallowest Curie point depth (ca. 18.5 km) is located in Subei (苏北) subsidence, where the estimated temperature gradient value is about 31.35℃/kin, which is comparable with the measured value of 30℃/krn. In addition, a two-dimensional numerical solution of the heat conduction was used to calculate the temperature field to a depth of 30 km along the profile from Tancheng (郯城) to Lianshui (涟水) with a length of 139 km. The steady state model solved using the finite element method shows that the temperature around the Curie point depth is about 585.36℃, which is close to the Curie temperature (580 ℃) of magnetite at atmospheric pressure. These results provide new insights into the tectonic and continuous thermal structures of the Sulu UHP metamorphic belt.