地球的“倾斜相机”式透视投影

引言空间图像提供了地球的壮观景色,它通常显示的是一个不同于空间背景的弯曲地平线,并且陆地和海洋形成鲜明对照。这些由地球轨道卫星拍摄的图像是一种形成于照相机聚焦平面上的透视投影。透视点或照相机的焦点是一个位于地表与无穷远之间某一空间位置上的点,照相机的聚焦平面通常倾斜于焦点与地球球心的连线。空间图像通常可以以一组经线、纬线和陆地轮廓线的透视投影来模拟,投影面就是位于透视点和地球之间的某个空间点上的倾斜平面。透视     

用专家系统技术确定地图要素的地图符号类型

地图要素与地图符号类型之间的关系长期被人们忽略。但它确是专题地图设计专家系统中不可缺少的重要环节,是地图符号设计的基础。本文给出了地图要素类型和地图符号类型的定义,详细阐述了两者之间的关系;作者用Turbo Prolog2.0语言在COMPAQ 386微机上建立的地图要素的地图符号类型确定专家系统模块,可以对一幅地图上各种类型的地图要素确定其地图符号类型,为下一步具体的符号设计工作打下了良好的基础。     

弹性椭球地球模型的海潮效应

本文推证了比较完整的弹性椭球地球模型的海潮负荷理论和计算公式,它对弹性球型地球模型海潮效应计算的发展起了一定的作用。     

Petrochemistry,Age and Petrogenesis of the Shexian Pluton in Southern Anhui

The Shexian gneissic granodiorite in southern Anhui trends NE 55° from Shexian in the west to Guitoujian in the east with a length of 22 km and an outcrop area of 32 km. It was considered formerly to be Caledonian on the basis of a biotite K-Ar age of 474 Ma (1982). However, new evidence indicates that it may be Early Jinning in age as shown by: (1) it is found intruding into the Mid-Proterozoic Shangxi Group and is unconformably overlain by the Sinian Xiuning Formation, and (2) a zircon U-Th-Pb age of 928 Ma is obtained for the pluton. The pluton is composed of plagioclase (An=27.37%), K-feldspar(14%), biotite(16%) and quartz(32%). Accessory minerals are ilmenite (150g/T), xenotime (15g/T). garnet(25g/T), monazite(10g/T), zircon (20g/T) and apatite (104g/T). Petrochemical characteristics of the intrusion are:(l) Al-enrichment (A/NKC=1.30); (2) H₂O enrichment (H₂O= 1.74%); and (3) low oxidation index (f ’=0.10). It belongs to the continental crust transformation type as evidenced by: (1) MF and Mg/Y values of biotite are 0.41 and 0.31 respectively; (2) (⁸⁷Sr/⁸⁶Sr)=0.71119; (3) δ Eu=0.52; and (4) A/NKC=130. The Shexian pluton is therefore considered as a product of melting of phyllite at depth in the light of similarities in trace element and REE contents with the phyllite of the Banxi Group. Calculations of REE batch partial melting indicate that it may have resulted from 75% melting of the Banxi phyllite.