Shear-hosted Mesothermal Vein System in the Jiapigou Goldfield, Northeast China: Implication for Subsequent Exploration

Abstract. The auriferous mesothermal lodes and veins occurred in the Jiapigou Goldfield, Jilin Province, Northeast China, are inevitably hosted by shear zones or fractures of varying orientations and magnitudes. Our recent study suggests that the Jiapigou major shear zone (JMSZ) - a regional NW-SE-trending driving structure, played an essential role in the formation and localization of the shear-hosted auriferous mesothermal systems. Regional dextral shearing of the JMSZ controlled the general occurrences and orientations of lodes and veins, and consequently, constrained the development of the internal structures, geometric details and final localization of lodes and veins. Therefore, the development and final localization of shear-hosted gold system can be comprehensively recognized in terms of both the Riedel shear system theory and the effects of the regional prolonged progressive deformation of subhorizontally right-lateral shearing. The lodes and veins belonging to "R-" and "D-shear" would tend to be much more stable along their strike and dip directions than those belonging to "T-fracture" in the Riedel shear system. However, due to the prolonged progressive deformation, the original T-fractures might undergo local strain localization and partitioning and finally were modified into hybrid fractures filled by auriferous quartz veins, as displayed by many typical lodes and veins occurred in the Jiapigou Goldfield. In order to refine predictive exploration modeling, it is important to understand the structural attributes, geometries, and final localization kinematics of ore-hosting shears in a huge shear system as that developed in the Jiapigou Goldfield.     

Constraints of progressive transmission of spatial data on the web

The progressive transmission of map data on the World Wide Web provides the user with a self-adaptive strategy to access remote data. It not only speeds up the web transfer but also offers an efficient navigation guide for information acquisition. The key technology in this transmission is the efficient multiple representation of spatial data and pre-organization on the server site. This paper aims at progressive transmission investigating some constraints from three aspects: data organization on server site, data control in the transmission process and data restore after reaching the client. Two strategies, namely on-line map generalization and off-line map generalization, are examined respectively for this kind of progressive transmission.     

顾及邻近五点的建筑物多边形化简方法

针对传统的建筑物化简算法无法准确保持建筑物局部细节几何特征,容易产生尖锐凸角等问题,提出了一种基于邻近五点的建筑物多边形化简方法。通过将多边形边界上的邻近五点定义为基本处理单元,实现对建筑物边界Z形平行、Z形不平行、U形平行、U形不平行的4类几何模式划分,进行渐进式化简,并针对化简过程中产生的尖角顾及角度约束对其削尖。对某地区部分1∶1万实际建筑物多边形数据进行试验,结果表明,所提算法在保持建筑物基本几何形态特征的基础上,能够尽可能地避免尖角的产生,化简结果更加符合人类的视觉认知。     

新疆阿勒泰红柱石-矽线石型递增变质带特征及其PT条件研究

新疆阿勒泰地区发育了红柱石-矽线石型递增变质带,由绿泥石-黑云母带、黑云母-石榴石带、石榴石-十字石带、十字石-红柱石带和矽线石带组成,根据石榴石成分环带、变质与变形关系、矿物共生组合演化等特征,将变质作用分为峰前期、峰期和峰后期3个演化阶段。峰前期、峰期为连续的递增变质过程,形成典型的中-低压过渡型递增变质带,峰后期属于退变质过程。据石榴石一斜长石一黑云母-白云母-石英组合内部一致地质温压计估算出峰期温度-压力：T=580℃～670℃,P一0．4GPa～0．5GPa。变质作用演化具有顺时针的PTt轨迹,代表陆壳有一定程度的构造增厚,但幅度不大,没有大规模的陆壳俯冲或拆沉作用,这种增厚可能以陆壳的构造叠置机制为主。总体相当于地体间斜向走滑兼有一定垂直分量的拼合过程的地球动力学机制。     

德兴金山金矿田不同尺度构造特征及其与成矿作用的关系

德兴市金山金矿田是与赣东北深大断裂带内次一级剪切带有关的中温热液矿床。其矿石类型主要由与断裂充填有关的小尺度石英脉组成，这些石英脉主要呈纹层状。不同尺度的构造研究表明，金山金矿是同构造的产物，递进变形作用与成矿作用密切相关，在成矿过程中，普遍发育压溶作用，导致早期的石英颗粒发生溶解以及形成黄铁矿压力影。金山金矿蚀变硫化物以黄铁矿为主，说明成矿流体中硫主要以H2S和HS-形式存在。断层阀机制引起压力波动，进而导致成矿流体的相分离和水—岩反应，是金山金矿的主要成矿机制。     

The method of graphic simplification of area feature boundary with right angles

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干旱区沙漠化土地逆转植被的防风固沙效益研究

使用便携式防沙风速廓线测量仪和阶梯式集沙仪测定了单个植物的阻风作用以及不同恢复阶段植被内的近地面风速、输沙量;同时调查了不同恢复阶段植被的组成、覆盖度,土壤理化性质。结果表明,油蒿、沙蒿、柠条和花棒的个体空间构型分别是:沙蒿、花棒株型为疏散丛生型;柠条株型为中间丛生型;油蒿株型为紧密丛生型;近地面0~50 cm层的阻风阻沙作用效果由强到弱依次为油蒿>沙蒿>柠条>花棒。演替更新过程中,柠条、花棒、沙蒿逐渐衰退,到顶级群落阶段已完全从群落中退出,油蒿形成单一优势种顶级群落。由于优势种群的变化,从初始阶段→发展阶段→相对稳定阶段（顶级群落阶段）的演替更新过程中,近地面粗糙度从0.003 cm、6.039 cm增加到17.726 cm;在流动沙丘2 m高度风速为6.5 m·s-1时,相对稳定阶段没有出现风蚀,发展阶段输沙量只达到1.83 g·cm-1·h-1,占到初始阶段的3.2%。在3 m高度风速相同时,发展阶段近地面风速较初始阶段降低了54.29%,沙结皮厚度达到1~3 mm,所占面积比例达到91%,已经基本实现防风固沙;相对稳定阶段近地面风速较初始阶段降低了83.68%,沙结皮厚度达到5~6 mm,所占面积比例达到98%,完全实现防风固沙。     

基于顶点线性插值的建筑物群聚合的简易方法

提出了基于顶点线性插值的建筑物群聚合的简易方法:首先通过插值加密建筑物轮廓线顶点,以最短邻近连线互不相交为原则,构建相邻建筑物轮廓线顶点之间的最短邻近连线;其次依据这些最短邻近连线自动确定相邻建筑物之间的聚合区域;最后按照渐进式方法聚合建筑物群,获取聚合后的新建筑物轮廓线,该方法还可以处理建筑物群的多边形存在相交和重叠...     

改进局部安全系数法在土坡稳定性分析中的应用

提出一种改进局部安全系数法以考虑土坡渐进破坏过程。该方法是一个涉及搜索危险滑裂面的总体最小安全系数和寻找土条侧面强度发挥系数的最优组合的过程。采用双层MDCP法离散组合型方法解决这一二重优化问题。结果表明,改进局部安全系数法较之以常规方法更合理、高效。