Decrepitation Thermometry and Compositions of Fluid Inclusions of the Damoqujia Gold Deposit,Jiaodong Gold Province,China:Implications for Metallogeny and Exploration

The recently discovered Damoqujia (大磨曲家) gold deposit is a large shear zone-hosted gold deposit of disseminated sulphides located in the north of the Zhaoping (招平) fault zone, Jiaodong (胶东) gold province, China. In order to distinguish the temperature range of cluster inclusions from different mineralization stages and measure their compositions, 16 fluid inclusions and 5 isotopic geochemistry samples were collected for this study. Corresponding to different mineralization stages, the multirange peaks of quartz decrepitation temperature (250-270, 310-360 and 380-430℃(2) indicate that the activity of ore-forming fluids is characterized by multistage. The ore-forming fluids were predominantly of high-temperature fluid system (HTFS) by CO2-rich, and SO2-4-K type magmatic fluid during the early stage of mineralization and were subsequently affected by low-temperature fluid system (LTFS) of CH4-rich, and Cl--Na /Ca2 type meteoric fluid during the late stage of mineralization. Gold is transferred by Au-HS- complex in the HTFS, and Au-Cl- complex can be more important in the LTFS. The transition of fluids from deeper to shallow environments results in mixing between the HTFS and LTFS, which might be one of the most key reasons for gold precipitation and large-scale mineralization. The ore-forming fluids are characterized by high-temperature, strong-activity, and superimposed mineralization, so that there is a great probability of forming large and rich ore deposit in the Damoqujia gold deposit. The main bodies are preserved and extend toward deeper parts, thereby suggesting a great potential in future.     

隔震建筑在乌鲁木齐地区应用的可行性分析

隔震技术是近几十年来地震工程最重要成果之一,是一种经济、可靠、有效的防震减灾技术,但在实际工程中应用率较低,主要原因是对其成熟有效性和经济性等不够了解。通过分析相应的规范、标准和隔震工程实例在破坏性地震中的表现来说明隔震技术的成熟性,通过对已建隔震建筑与传统建筑的对比,分析了隔震技术的经济性,结合隔震技术优点与乌鲁木齐地区特殊的地震构造环境和地震危险性,提出在乌鲁木齐地区进一步推广应用隔震技术的可行性和必要性。     

中国铬矿资源2010年保证程度与前景

至１９９３年底，我国已勘查的铬矿区有５６处，累计探明铬矿石储量１３０５．３万ｔ，主要分布于西藏，新疆，内蒙古等省区，贫矿与富矿（Ｃｒ２Ｏ３〉３２％）大体各占一半，多为中小型矿床，矿床成因主要为岩浆晚期矿床。冶金工业生产不锈钢是铬矿石的最大消费领域，按不锈钢与钢产量比和我国铬矿生产能力测算，２０１０年只能满足国内铬矿石需求量的１５％，其余要靠进口解决。西藏是国内找铬矿的最佳远景区。     

Mineralogical and geochemical investigations of the Dajia Salento-type bauxite deposits,western Guangxi,China

The Dajia Salento-type bauxite deposit in western Guangxi is hosted within the Quaternary ferrallitic soil profile, and it formed via breaking up, weathering and oxidizing of Permian bauxite orebodies occurring as a semi-continuous layer in the upper Permian. Mineralogical analyses reveal that diaspore, hematite and kaolinite are the major minerals in bauxite ores with small amounts of anatase, chamosite, gibbsite, goethite, illite, zircon, quartz and pyrite. The ore texture and mineral assemblage reveal that the depositional/diagenetic environment of the Dajia bauxite was much close to phreatic environment. Both the ore texture and the morphology of zircon grains also indicate that most of the bauxitic soils were transported a short distance. Diaspore is suggested to be non-metamorphic in origin and mainly formed in a reducing condition of diagenetic environment, while kaolinite is the product of the in situ epigenetic replacement of alumina in diaspore by dissolved silica. Geochemical analyses indicate that Al₂O₃, Fe₂O₃, SiO₂ and TiO₂ are the main components of the bauxite ores and trace elements such as Zr, Hf, Nb, Ta, Th and U were enriched during the bauxitization process. Simultaneously, Zr vs. Hf and Nb vs. Ta show a high correlation. Geochemical indices such as Zr/Hf, Nb/Ta and Eu/Eu* (among others) denote that the magmatic rocks related to the Emeishan plume in western Guangxi and the carbonates in the underlying Maokou Formation provided the main sources of material for the bauxite ores.     

山东省移动气象台通信网络系统

本文主要介绍移动气象台中的通信网络系统,包括网络的整体结构,各部分的功能与实现方式,及各种网络设备的软硬件配置等.     

川西坳陷中段上三叠统须家河组储层沥青地球化学特征及成因研究

川西坳陷上三叠统须二、须四段致密砂岩的溶蚀孔洞、裂缝及砂岩层理界面上分布大量的沥青,沥青的热演化程度极高,须二段达到干气阶段,须四段达到湿气一干气早期阶段;经过针对砂岩中层理界面及裂缝、溶孔洞中充填的沥青及泥岩层裂缝中充填沥青取样的有机地球化学指标分析后显示:沥青具有较低的H/C、O/C比,须二段沥青残余生烃能力极小,须四段沥青还具有较大的残余生烃潜力;须家河组须二、须四段沥青为马鞍塘-小塘子组与须二段海湾相油型烃源岩在生油窗期成的古油藏,在后来的高温条件下裂解成天然气后残留物;须二,须四的古油藏构成了川西坳陷上三叠统须家河组天然气重要的气源.     

A Combined-Power Model for the Distribution of Axial Force in Shaft Anchor along Its Length

INTRODUCTIONThe anchorage of geomaterial , including shaftanchors and prestressed tendons ,is usually used ingeotechnical engineering. Owing to various advanta-ges ,these two anchorage types are widely used instructures in China ( Cao et al ., 2003 ; Fu et al .,1999 ;Lu et al .,1998 ; Li et al .,1995) . Shaft an-chors can be classifiedinto three kinds by the forceinthe shaft and cement grout :tensile ,press ,and sheartype (Lu et al .,1998) . The tensile type is the mostpopular in China…     

智能化专题地图快速设计制作研究

本文根据专题地图智能化快速设计制作的需求,提出以构建专题地图智能化设计知识库为驱动实现专题地图快速设计制作的模式.在分析其他领域知识和知识库概念的基础上,兼顾该领域的特点,对此模式中知识和知识库的概念重新进行界定.文中以河南省交通图设计为例,基于混合武表示法和此模式下知识库的新特性,构建了专题地图设计知识库的框架体系并进行了阐述.     

用标贯法对盘锦城区砂土液化进行等级分区

本文针对盘锦城区砂土液化不良地质作用,采用工程地质勘察中的原位测试——标准贯入试验法结合前人在此所作的地质调查资料和工程地质勘察资料,按照《建筑抗震设计规范》（GB5001-2001）相关规定,对盘锦城区的砂土液化进行相应的等级分区,对于盘锦市今后的工程建设具有实用意义。     

20世纪80年代以来西南喀斯特地区植被变化对气候变化的响应

气候变化与植被变化的关系已经在全球和区域尺度上得到了研究证明。在前人研究的基础上,基于AVHRR GIMMS NDVI和AVHRR GloPEM NPP数据集,通过对逐个像元信息的提取和分析,研究了20世纪80年代以来,我国西南喀斯特地区植被变化对气候变化的响应。研究结果显示:(1)20世纪80年代以来,西南喀斯特地区植被覆盖度和净初级生产量总体均呈增加的趋势,但不显著。植被指数的年际变化存在着明显的区域差异;(2)植被指数年际变化与气候因子年际变化的相关系数区域分异比较明显;(3)不同的植被类型对气候变化有着不同的响应特征;在该研究区气温变化对植被变化的影响要高于降水量变化对其影响;(4)植被指数年际变化与气候因子年际变化的相关系数在不同气候条件下分布的规律性比较明显。本研究将会增进对影响喀斯特生态系统稳定性的自然过程的认识,同时也会为喀斯特生态系统的管理提供科学依据。