袖珍矿物晶体结构模型的制作

所谓晶体结构,即晶体内部原子的排列形式}o晶体结构的表示方法有两种,即图示和模型。虽然所有的物理学、化学、矿物学和材料科学的教科书中都有晶体结构图,但是要使学生乃至专家建立结构的空间概念却绝非易事。因此,许多著名的晶体学家和矿物学家都十分强调制作模型的重要性。     

The Orogeny in the Altaides

Studies of the deformation styles, formation types and isotopic age data indicate that the Altaides has successively experienced 5 stages of orogeny: (1) the Kanas orogeny forming the angular unconformity between the Baihaba Formation (O_3) and the Habahe Group (Z-O_2); (2) the Daqiao orogeny (S_3-D_(1-2) giving rise to the early Hercynian quasi-aulacogen extensional continental crust of the area; (3) the Altay orogeny (middle-late Hercynian) leading to the oblique intracontinentai collision and the formation of large shear arc-shaped thrust system and representing a strong orogeny stage; (4) the pan-Altay orogeny (latest Hercynian-Indosinian) resulting in the uplifting and erosion of the mountains as a whole; (5) the Himalayan movement causing the rejuvenation of fault systems and block uplift of the Aitaides since the Cenozoic.     

Tectonic Units and Their Fundamental Characteristics on the Northern Margin of the Alxa Block

The northern margin of the Alxa block is the junction of a tectonic units. Four first-order tectonic units are distinguished: 1. the Yagan structural zone characteristic of an immature island arc; 2. the Zhusileng-Hangwula structural zone, which was a passive continental margin in the Early Palaeozoic and was transformed into an active continental margin in the Late Palaeozoic;3. the Shalazha structural zone characteristic of a mature island arc; 4. the Nuru-Langshan structural zone, which was a Proterozoic orogenic belt and later evolved into an extensional transtional crust in the Palaeozoic. The above-mentioned tectonic units differ remarkably in sedimentary formations, magmatic rock associations, metamorphism and geochemistry and are bounded by faults between one another.     

双峰县金坑冲金矿地质特征及找矿前景

本文概述了金坑冲金矿地质特征,并对其矿化规律作了总结。在此基础上,依据地质类比与土壤地球化学测量成果,指出王家湾一丫头山一带,是找石英脉一蚀变岩型金矿的远景区。     

上海附近地区水域的地质灾害及其对工程建筑的影响

本区水域的地质灾害分为直接的、潜在的和人为的三种,类型有冲刷槽、滑坡、活动沙波和沙脊、不稳定岸坡、快速侵蚀和堆积,浅滩和暗礁,埋藏古河道、古洼地、埋藏基岩、含气沉积物、“鸡蛋壳”地层,断层和地震,人为障碍物等。本文讨论了各类水域地质灾害的分布、特征、对工程建筑的影响和防治措施。     

海洋沉积物可溶铁测定条件的探讨

海洋沉积物可溶铁Fe~(3+)/Fe~(2+)比值,已被海洋地质工作者作为海洋油气化探的一项间接指标应用于东海油气化探中。这种铁的含量受提取酸的种类、浓度、样品微沸时间、放置时间等条件的影响。必须采用统一的可溶铁测定方法,只有在同一标准条件下测定的海洋沉积物可溶铁结果才有对比意义。     

机房干扰源的分析

从理论上分析了机房中干扰产生的原因,提出了压低干扰的措施。     

青海湖人湖沙质物的计算与水下沙堤的形成

青海湖流域沙漠以环湖分布为特点,又以ENE为集中。这一状态使多方向的风沙流入湖,而实际上入湖沙量是以W、N、E三个方向的流沙为主。根据入湖风沙公式计算,入湖风沙量为887.08×10~4t/a。并推算出河流泥沙入湖为35.77×10~4t/a,空中降尘为30.36×10~4t/a。入湖后的沙质物在湖流、波浪的作用下,由西向东运移,堆积成水下沙堤,逐渐增高加宽露出水面,分隔成子湖。同时在干燥的气候作用下,导致湖面收缩,生态环境恶化。     

福建省龙海—漳浦沿海第四纪地壳运动特征与地震

本文论述了福建龙海—漳浦沿海地区的第四纪地层及沉积结构、构造地貌、第四纪地壳运动特征及其与地震活动的关系。