在国内处于领先水平的光谱分析

光谱分析工作从５０年代初创立至今,在矿物分析、地质找矿等领域得到了广泛的应用。率先在地矿部门将光谱分析应用在定量分析领域,并将此领域的研究和应用推向了新阶段。经过４５年的发展,目前,光谱分析在理论研究和分析技术研究方面的某些领域,处于国内领先水平。     

伽玛能谱快速找金方法在新疆北部的应用研究

概述了采用伽玛能谱测量方法在新疆北部富蕴、托里、包古图、青河等地开展找金应用研究。快速有效地评价了一批综合化探异常和金矿点,圈定了成矿有利地段和富矿化段,对工程布置和采坑掘进给予了及时指导。     

江苏武进漕桥地区第四纪更新世海侵初步研究

根据漕桥地区更新世沉积物不同层位中产出的微体古生物,对该地区的更新世海侵问题作了初步研究。从有孔虫复合分异度的变化,介形虫与有孔虫化石群比值的变化等,阐明了太湖海侵旋回、湖海侵旋回的海侵与海退过程,结合微体古生物的生态类型及丰度,论述了古地理环境。     

南京汤山地下热水的控制因素与资源前景

在介绍南京汤山地下热水地热地质背景的基础上,探讨了其“源”、“通”、“储”、“盖”控制因素,初步提出了该区地下热水的形成模式与资源前景,对该区地下热水的勘查开发提出了建议。     

Approach to Calculating Methods of Wave Breaking Depth and Height

- Engineers in coastal engineering have been paying much attention to the research subject on wave breaking. In this paper, previous research results on the calculating methods of wave breaking depth and height are enumerated, the laws of wave transformation before and after wave breaking are investigated, an adequate supposition is made, and the effect of beach slope, bed friction and breaking turbulence on wave breaking is considered. By applying the theory of wave energy dissipation rate and combining with proper formulas of solitary waves, a new calculating formula of wave breaking depth and height on the movable bed is derived and examined with the data from experimental pools of different sizes, and it is proved to be of practicability.     

The Program Application on the Relative Method of Fuzzy Mathematics

The method of fuzzy mathematics for simultaneous assessment of time and intensity of earthquake hazards has been studied.This method is based on fundamental statistical indices of regional seismicity.Applying the retrieval method of fuzzy information,we can classify the time and intensity into several intervals and classes of seismic activity,then the possible time interval of large earthquakes with magnitude of M≥Ms can be estimated in a given region.Based on the preceding idea,an FRPP program is constructed.For the automatic data processing when this method is used,it is very important to design the statistical process of each index decomposition so that the program could be fit to a different sample discussed.There are some functions in the FRPP program.The man-made impact on results is reduced to the minimum as far as possible.Computation time is saved.There is a menu on which time interval,index,intensity class,and output data all can be selected.The catalog input that can be displayed on the scre     

娘娘山碱性火山-侵入岩特征及成岩定量模拟

本文通过对铜井娘娘山旋回中生代火山-侵入岩系岩石化学、微量、稀土元素以及铷锶、钐钕等同位素详细研究,认为这套岩石具高碱、硅不饱和、强烈富集不相容元素和轻稀土特征。岩石的~(87)Sr/~(86)Sr初始比值为0.7070—0.7073,∈_(Nd)值为-3.4—3.3,利用二元混合模式计算得出蓝方石响岩和霓辉正长岩源区物质成分相当41%、42%上部陆壳和59%、58%亏损地幔组成的混合物,源区物质经6.4%、6.6%部分熔融形成初始岩浆,表明娘娘山旋回碱性火山-侵入岩系是壳幔混合物经部分熔融后所形成的产物。     

Source process of the 14 November 2001 western Kunlun Mountain M_S=8.1 earth-quake

Introduction On November 14, 2001, a great earthquake occurred in the western Kunlun Mountain area(Figure 1). The original time is 09h26min10.0s (UTC); the hypocentral location is 35.95°N,90.54°E; focal depth is 10 km from USGS National Earthquake Information Center (NEIC);MS=8.1 from China Seismic Network and Mw=7.8 from Harvard and Earthquake Research Insti-tute (ERI), University of Tokyo. This earthquake, known as the western Kunlun Mountain earth-quake, is an extraord…     

基于1∶100万土壤空间数据库的有机碳储量估算研究——以中国东北三省为例

以最近建成的中国1∶100万土壤空间数据库以及《中国土种志》和省级土种志的土壤属性为基础,共收集东北三省736个土壤剖面理化分析数据,估算出该地区土壤有机碳总储量,并分析讨论了土壤有机碳密度在空间上的分布特征。结果表明,东北三省土壤有机碳密度平均为16.13kg/m2,在空间分布上的总趋势为东北部高,西南部低,密度较高的有机碳主要分布在原始森林、湿地及部分农业耕作区中。土壤有机碳密度最高的土类为泥炭土和沼泽土等土类,最低的为石质土、风沙土等土类。     

Microorganisms Linked to Neoproterozoic Microspar Carbonate Sedimentation in the Jilin-Liaoning Area

Molar-tooth carbonate refers to a sort of rock that has ptygmatical folded structure comparable to the ivory. This kind of carbonate exists in a special time range (from Middle to Neoproterozoic). Its origin and the possibility to use it in stratigraphic correlation of the paleocontinent is the key task of the IGCP447, a project on Proterozoic molar tooth carbonates and the evolution of the earth (2001-2005). The importance lies in that the molar-tooth structure is the key to solving problems related to Precambrian biological and global geochemical events. The molar-tooth structure is associated with microorganisms. Development and recession of such carbonates have relations with the evolution process of early lives and abrupt changes in sea carbonate geochemistry. In recent years, based on researches on petrology, geochemistry and Sr isotope of molar-tooth carbonate in the Jilin-Liaoning and Xuzhou-Huaiyang area, the authors hold that it can be used as a marker for stratigraphic sequence and sedimentary