Late Paleozoic Fluid Systems and Their Ore-forming Effects in the Yuebei Basin, Northern Guangdong, China

Based on detailed and systematic researches of the geology of ore deposits, fluid inclusions and isotope geochemistry etc., and regarding the Late Paleozoic fluid system of the Yuebei Basin as an integrated object in this paper, we have revealed the temporo-spatial evolution law of the basin＇s fluid system and discussed its ore-forming effects by simulating and analyzing the distribution of ore-forming elements, the fluid thermodynamics and dynamics of evolution processes of this basin. The results show that Late Paleozoic ore-forming fluid systems of the Yuebei Basin include four basic types as follows. （1） The sea floor volcanic-exhalation system developed during the rapid basin slip-extension stage in the Mid-Late Devonian, which affected the Dabaoshan region. It thus formed the Dabaoshan-type Cu-Pb-Zn-Fe sea floor volcanic-exhalation sedimentary deposits. （2） The compaction fluid system developed during the stable spreading and thermal subsidence-compression stage of the basin in the Mid-Late Devonian. The range of its effects extended all over the whole basin. It resulted in filling-metasomatic deposits, such as the Hongyan-type pyrite deposits and pyrite sheet within the Fankou-type Cu-Pb-Zn-S deposits. （3） The hot water circulation system of sea floor developed during the stage of basin uplifting and micro-aulacogen from the late Late Carboniferous to Middle Carboniferous. The range of its effects covered the Fankou region. It thus formed MVT deposits, such as the main orebody of the Fankou-type Pb-Zn-S deposits. （4） The gravity fluid system developed during the stage of fold uplifting and the basin closed from Middle Triassic to Jurassic, forming groundwater hydrothermal deposits, e.g. the veinlet Pb-Zn-calcite orebodies of the Fankou-type Pb-Zn- S deposits. Migration and concentration of the ore-forming fluids were constrained by the state of temporo-spatial distribution of its fluid potential. Growth faults not only converged the fluids and drove them to move upwards, but also the fluids often crossed the faults to the edges of the basin at the bottom of these faults and the lithologic interfaces, and even migrated to the basin＇s edges from top to bottom along the faults, which may be one of the basic reasons for the stratabound deposits to cluster mainly along the contemporaneous faults on the inner border of the basin. The superposed mineralization resulting from the multi-stage activity of contemporaneous faults and ore-forming fluid systems in the basin may be one of the key factors for forming superlarge ore deposits.     

云南省制造业的地区专业化研究

长期以来,制造业是云南省新型工业化进程和经济发展的重要引擎,发挥规模经济效应、提升生产效率、改进产业结构的专业化分工将是云南省进一步推进"桥头堡"建设下制造业发展的重要方式。文章运用云南省第二次经济普查数据,选用樊福卓的地区专业化系数,从地区和行业两个角度研究云南省制造业的地区专业化状况。结果表明,云南省制造业整体的地区专业化水平较低,制造业发达州市的地区专业化水平低,欠发达州市的地区专业化水平高;区位条件、行业规模与特征是影响地区专业化水平的重要因素。在此基础上,根据各州市的区位条件、资源禀赋和城市规模给出相应的制造业专业化分工方式,以期为云南省新型工业化建设和经济发展提供理论和实践依据。     

Estimation of Turbulent Fluxes Using the Flux-Variance Method over an Alpine Meadow Surface in the Eastern Tibetan Plateau

The flux-variance similarity relation and the vertical transfer of scalars exhibit dissimilarity over different types of surfaces,resulting in different parameterization approaches of relative transport efficiency among scalars to estimate turbulent fluxes using the flux-variance method.We investigated these issues using eddycovariance measurements over an open,homogeneous and flat grassland in the eastern Tibetan Plateau in summer under intermediate hydrological conditions during rainy season.In unstable conditions,the temperature,water vapor,and CO2 followed the flux-variance similarity relation,but did not show in precisely the same way due to different roles(active or passive) of these scalars.Similarity constants of temperature,water vapor and CO2 were found to be 1.12,1.19 and 1.17,respectively.Heat transportation was more efficient than water vapor and CO2.Based on the estimated sensible heat flux,five parameterization methods of relative transport efficiency of heat to water vapor and CO2 were examined to estimate latent heat and CO2 fluxes.The strategy of local determination of flux-variance similarity relation is recommended for the estimation of latent heat and CO2 fluxes.This approach is better for representing the averaged relative transport efficiency,and technically easier to apply,compared to other more complex ones.     

北山花岗岩热破裂室内模拟试验研究

岩石热破裂是高放废物地质处置工程中需深入研究的课题。对我国高放废物重点预选场址甘肃北山的花岗岩开展室内热破裂模拟试验研究,采用多通道温度测试仪、声发射、波速层析成像和数码显微镜等手段研究了该花岗岩热破裂过程。试验表明,（1）热破裂从试件端部开始产生,逐步向内缓慢扩展,表现出分段性和独立性;（2）根据声发射撞击率可将热破裂可分为稳定热损伤、宏观裂纹形成、宏观裂纹扩展、裂纹冷却闭合4个阶段,声发射定位的时空演化规律清楚地揭示了裂纹从试件上端部向内部扩展的规律;（3）波速层析成像指示了宏观裂纹位置及高温对岩石造成显著损伤的区域,热应力产生的损伤集中在试件边界,范围小,损伤严重,高温造成的损伤集中在钻孔附近高温区,范围较大,损伤略轻微;（4）监测多通道温度,获得了试件内的温度场并为数值模拟参数选取提供验证,采用有限元程序进行了热力耦合数值模拟,从机制上初步解释了热破裂现象,研究认为综合声发射实时监测热破裂过程和波速层析成像能实现对热损伤的量化的特性可实现岩石热破裂的动态监测和损伤量化,为今后地下实验室相关试验的开展和认识高放废物处置长期稳定性做了有意义的探索。     

贵州关岭生物群海百合Traumatocrinus的再研究

在前人的研究基础上,通过对大量新发掘的贵州关岭地区晚三叠世海百合化石标本的再研究,肯定了Trauma-tocrinus的有效性。根据目前的材料,认为该属只有1个有效种,即Traumatocrinus hsui;而根据化石的埋藏学特征,认为幼年体Traumatocrinus hsui营假浮游生活,成年体是否能够适应底栖生活环境尚需进一步证实。     

基于GPRS的监控软件和网站的设计与实现

针对野外恶劣自然环境条件制约冻土温度现场采集和远程监控的问题,本文设计和开发基于通用分组无线业务(GPRS)的冻土实时监控软件和监控中心网站。冻土远程实时监控软件实现野外冻土温度数据的自动采集、实时显示、数据存储和远程控制等功能,降低数据采集的成本,提高数据采集的效率,已经成功应用于野外现场监控。配套开发的监控中心网站将冻土温度数据发布至Internet网络,解决冻土数据共享问题,扩大冻土温度监控的范围,实现多用户的实时数据远程监控。     

基于SPSS和GIS的BP神经网络农用地适宜性评价

以中原城市群为研究区,在应用GIS基础上运用SPSS软件进行主成分分析,根据因子贡献率提取主导性强的综合因子,利用提取的主导因子进行系统聚类选择典型样本;依据因子的贡献率调整BP神经网络初始权值,建立评价模型,进行农用地适宜性评价方法的探讨。通过检验,改变初始权值建立的BP模型预测合格率为50%,相对误差最大值为18.9%;为了进一步改进BP网络,把第一次调整权值训练得到的网络权值作为下一次建模的初始权值,训练得到的BP模型预测合格率为100%,相对误差最大值为9.5%。其后运用层次分析法、主成分聚类法作为对照,验证了这种BP模型在农用地适宜性评价中的可靠性与精确性。最后根据所建立的BP模型预测获得中原城市群农用地适宜性分区图,各土地类型适宜性从西往东呈现由低到高的分带性,其中高度适宜区占总面积的32.4%;中度适宜、勉强适宜、不适宜区分别占总面积的28.9%、22.1%、16.6%。     

一种移动空间信息服务系统的设计与实现

在介绍移动空间信息服务系统(MSISS)的概念、体系结构及技术背景的基础上,探讨了MSISS系统中导航定位、移动通信、嵌入式系统、移动计算等关键技术,提出了一种具有创新性的设计与实现策略。     

植被生态用水结构及绿水资源消耗效用——以黄河三门峡地区为例

以黄河三门峡地区为研究对象,构建适用于流域尺度植被生态用水估算的生态水文模型,对三门峡地区20世纪50年代以来植被生态用水量进行了定量模拟,得到研究区植被生态用水时空结构差异.在此基础上,对三门峡地区不同植被类型绿水资源消耗效用进行了分析,提出该区域植被结构调整方案.结果表明:三门峡地区植被生态用水量自20世纪50年代以来,由于气候和土地利用状况的变化,总体呈现出降低-稳定-上升的趋势;生态用水空间结构主要表现在不同植被类型下生态用水量差异上:林地最大,其次为农作物、灌丛,草地最小;林地高效消耗比例最大,其次为草地和灌丛,农用地最小.基于不同植被类型绿水资源消耗效用分析,提出三门峡地区植被结构调整方案.在一定水资源消耗量状况下,减少无效和低效消耗量,增加高效消耗量,是缓解该地区生产、生活、生态用水矛盾,提高总体生态效益的重要途径.