郯庐断裂带在辽北地区三叠纪左行韧性剪切带的发现及变形特征

郯庐断裂带位于辽北地区的部分为区域上郯庐断裂北延分支依兰-伊通断裂带的一段,在1：5万区调中发现有北东向展布的三叠纪左行韧性剪切带,此韧性剪切带控制一系列三叠纪侵入岩的分布并对古生代地质体的展布进行改造.     

月潭水库洪水预报模型研究及水库建设对黄山市中心城区的水文效应分析

洪水预报是水库科学调度的关键依据,本文利用流域水文模拟方法,分别建立月潭水库洪水预报模型、建库后水库～屯溪区问流域水文模型及水库～屯溪之间河道演算模型,并基于成果,选择历史典型洪水,分析月潭水库建设对黄山市屯溪中心城区的防洪效应.     

鄂尔多斯盆地中部地区下古生界碳酸盐岩生烃潜力探讨

下古生界高成熟－过成熟碳酸盐岩的生烃潜力一直是困扰我国海相地层油气评价和勘探的重要问题，至今尚未得到很好的解决。本采用有机岩石学和有机地球化学方法，系统剖析了鄂尔多斯盆地中部地区下古生界碳酸盐岩的基本特征及其生烃潜力。结果表明，鄂尔多斯盆地中部地区发育下古生界海相碳酸盐岩，烃源岩厚度较大，有机质丰度较低，有机质类型主要为I型和Ⅱ型，有机质热演化已达到过成熟阶段，这套烃源岩是该区重要的有效气源岩，具有较好的生烃潜力，可为中部大气田提供良好的气源条件。     

CO_2 Density-Raman Shift Relation Derived from Synthetic Inclusions in Fused Silica Capillaries and Its Application

Abstract: The densities of CO2 inclusions in minerals are commonly used to determine the crystallizing conditions of the host minerals. However, conventional microthermometry is difficult to apply for inclusions of small size (< 5–10 μm) or low density. Raman analysis is an alternative method for determining CO2 density, provided that the CO2 density–Raman shift relation is known. This study aims to establish this CO2 density–Raman shift relation by using CO2 inclusions synthesized in fused silica capillaries. By using this newly-developed synthetic technique, we formed pure CO2 inclusions, and their densities were determined by microthermometry. The Raman analysis showed that the relation between CO2 density (D in g/cm3) and the separations (Δ in cm?1) between the two main bands (i.e. Fermi diad bands) in CO2 Raman spectra can be represented by a cubic equation: D (g/cm3)=0.74203(?0.019Δ3+5.90332Δ2?610.79472Δ+21050.30165)?3.54278 (r2=0.99920). Our calculated D value for a given Δ is between those obtained from two previously-reported equations, which were derived from different experimental methods. An example was given in this study to demonstrate that the densities of natural CO2 inclusions that could not be derived from microthermometry could be determined by using our method.     

考虑颗粒抗转动的砂土双轴试验离散元模拟

颗粒间抗转动作用是影响砂土力学行为的重要因素。将蒋明镜等（2005年）提出的考虑颗粒抗转动作用的颗粒接触模型植入PFC2D中,对砂土双轴试验进行了模拟,研究颗粒抗转动作用对砂土力学行为的影响。研究显示：颗粒抗转动对砂土力学行为影响显著。抗转作用越强,砂土强度越高;抗转系数为0.4时,松砂亦出现软化及剪胀现象。抗转动作用对孔隙比及配位数变化趋势影响也很显著。     

水泥—丙烯酸盐复合浆液的实验性研究

水泥-丙烯酸盐复合浆液是在丙烯酸盐浆液的基础上研制出来的一种复合浆液，它既保留了丙烯酸盐浆液流动性好，固结体弹性好的优点，又大幅度地提高了浆液的抗压强度和粘结强度，因此在注浆时可以带来良好的综合灌注效果，还对复合浆液的粘度和强度进行了试验性研究。     

Anomalous Enrichment of Silver in Organic Matter of the Songxi Shale-hosted Ag-Sb Deposit in Northeastern Guangdong

The silver contents of organic matter in the host rocks of the Songxi shale-hosted Ag-Sb deposit of northeastern Guangdong, South China, have been directly determined using the electron microprobe technique. The silver contents in two types of organic matter, marine vitrinite and solid bitumen, vary in the range from 100×10-6to 350×10-6, which are from tens of times to thousands of times higher than those of the host rocks in the ore deposit. The average silver content of the organic matter is also several times higher than the pay grade of silver for commercial mining of the ore deposit. It is quite obvious that the organic matter of the host rocks in the ore district is characterized by an anomalous enrichment of silver. The results of this study indicate that the silver anomalies in the organic matter have been derived from both the host rocks and the silver-bearing fluids of the Songxi black shale ore source. In the course of sedimentation and later hydrothermal reworking, organic matter was able     

在"数字国土工程"中我区地学数据库建设的现状及发展趋势

近年来,在国土资源部的高度重视下,我区相继建立了一系列地学数据库。这些地学数据库的建立不仅为地矿行业提供了基础性数据,也加速了"数字国土工程"和国土资源信息化建设的步伐。随着信息技术的高速发展,利用地理信息系统(GIS)将各类地学数据有机地结合起来,形成地学数据应用与管理系统,最终通过网络服务于社会,必将是各类地学数据发展的必然趋势。     

微细浸染型金矿床及其成矿作用

微细浸染型金矿是找矿潜力很大的一种矿床类型。近几年来逐渐将其作为一种独立的矿床类型加以研究和勘查。本文综合有关研究成果。总结了微细浸染型金矿成矿地质条件和矿床特征。并在此基础上讨论该类矿床的成矿作用。提出层控地下热卤水成矿作用。层控有机成矿流体作用和层控深源成矿流体成矿作用是该类矿床的三种主要成矿作用。该类矿床的成因类型总体上可以归属于层控热液改造型矿床。     

云南昭通毛坪铅锌矿床成矿物质来源的新证据--NE向断裂构造岩微量元素R型因子分析结果

R型因子分析可通过研究地质变量在时间和空间上的组合、变化和分布特征而形成地质概念,并恢复地质过程,指示物质来源.在研究云南昭通毛坪铅锌矿床地质特征的基础上,分别对矿区910和846中段Ⅱ、Ⅲ号矿带NE向断裂构造岩微量元素进行了R型因子分析,提出成矿物质来源的新证据.在时间上,指示了主要成矿期次为沉积成岩期和热液成矿期,热液期又划分为黄铁矿-闪锌矿阶段、闪锌矿阶段、闪锌矿-方铅矿阶段和碳酸盐-黄铁矿矿化4个成矿阶段;在成矿物质来源上,锌来源于赋矿地层(C1b和C2w)和外来成矿流体,铅主要由外来成矿流体带入.