黄沙坪铅锌多金属矿的成矿规律及深部找矿远景

众所周知,矿物质的成分是多种多样的,社会的发展和科学的进步需要运用到多重金属矿物质,在专业人员的勘探与挖掘中,发现了黄沙坪铅锌多金属矿,这个矿区中有丰富的有色金属,这个矿的发掘为研究成矿规律提供了物质基础,同时也为深部找矿提供了可靠的依据。本文主要分析黄沙坪铅锌多金属矿的成矿规律及深部找矿远景。     

Attribute Allocation and Retrieval Scheme for Large-Scale Sensor Networks

Wireless sensor network is an emerging technology that enables remote monitoring of large geographical regions. In this paper, we address the problem of distributing attributes over such a large-scale sensor network so that the cost of data retrieval is minimized. The proposed scheme is a data-centric storage scheme where the attributes are distributed over the network depending on the correlations between them. The problem addressed here is similar to the Allocation Problem of distributed databases. In this paper, we have defined the Allocation Problem in the context of sensor networks and have proposed a scheme for finding a good distribution of attributes to the sensor network. We also propose an architecture for query processing given such a distribution of attributes. We analytically determine the conditions under which the proposed architecture is beneficial and present simulation results to demonstrate the same. To the best of our knowledge, this is the first attempt to determine an allocation of attributes over a sensor network based on the correlations between attributes.     

大庆外围盆地侏罗纪-早白垩世早期古气候研究

为扩大勘探领域，运用古生物资料对大庆外围盆地的古气候进行了研究，外围盆地株罗纪－早白垩世早期发育的地层有早侏罗世海拉尔盆地的东宫组，中侏罗世三江盆地的绥滨断陷的绥滨组，晚侏罗世三江盆地的东荣组，虎林盆地的裴德组，七虎林组，早白垩世早期鸡西盆地，三江盆地的滴道组，城子河组、穆棱组，虎林盆地的下云山组，上云山组，在这些组中除晚株罗世东荣组，裴德组，七虎林组外，其它各组都产有比较丰富的孢粉化石，未发现孢粉化石的层位，依据植物化石，得出早株罗世东营组为潮湿的暖温带气候，中侏罗世绥滨组为潮湿的北亚热带气候，晚侏罗世为潮湿的暖温带气候，早白垩世早期滴道组，下云山组为潮湿的北亚热带气候，城子河组、上云山组为潮湿的中亚热带气候，穆棱组为潮湿的南亚热带气候。     

同成矿期构造减压扩容对内生金矿的控制作用

从同成矿期断裂构造与金矿的关系入手，分析了不同断裂构造形迹的减压扩容机制对金矿类型，矿体形态，矿石品位的控制作用，对寻找盲矿体具有借鉴和指导意义。     

闽西南地区推覆构造特征

闽西南地区推覆(滑脱)构造广泛发育,可划分为5种类型:发育于上古生界—中生界下三叠统溪口组中的拆离(滑脱)构造;形成于印支期的拆离(滑脱)构造,后受燕山早期及后期的褶皱作用形成褶皱拆离构造;印支期及燕山早期的中深层次逆冲推覆构造;燕山早期和晚期的浅层次逆冲推覆构造;分布于燕山早期浅层次逆冲推覆构造原地岩系之中的浅层次褶皱逆冲推覆构造,其中燕山早期中深层次逆冲推覆构造规模最大。      

葫芦岛市钢屯镇赵家屯西山铜钼多金属矿成矿远景及找矿标志

赵家屯西山铜钼多金属矿位于葫芦岛市北西的钢屯镇南部,行政隶属于葫芦岛市连山区钢屯镇境内,位于杨家杖子—八家子构造岩浆的活动带内。区内燕山期花岗岩浆多次侵入,对成矿物质的活化集中起到重要的作用,是主要的物质来源及热动力条件;受区域性构造活动的影响,断裂构造发育,为成矿提供了重要的赋矿空间。地层、构造、岩浆岩三位一体的空间有利于多金属矿床的产出,具备形成热液充填交代型矿床的条件。     

广东阳春石菉—鹦鹉岭—锡山铜锡多金属矿集区综合地球物理特征与成矿预测

石菉—鹦鹉岭—锡山一带是粤西地区的一个铜锡钨（铅锌）多金属矿密集区,矿床（点）众多,区内矿床勘查工作多开展于20世纪90年代前,勘查深度浅,且各矿床之间均为大面积第四系覆盖区,研究程度低,各矿床深部和外围均有良好的找矿前景。本文通过对该区开展的1∶5万重力测量、1∶1万地面磁法测量以及典型矿床电磁法剖面测量等工作成果的综合研究,认为本区主要为北西和北东向的区域构造控岩、控矿,综合物探成果反映空白区内隐伏构造发育,成矿地质条件有利,具备寻找新的中大型隐伏矿床的条件。通过进一步工作,该区有望成为粤西地区重要的铜锡多金属矿田。     

The Holy Alignment: Geodesic and Astronomical Fundamentals for Calculating the Adjustment of Medieval Naves

It is commonly believed that the longitudinal axes of churches extend exactly in an east-west direction. However, thorough investigations have shown that this is not always correct; rather, both southern and northern deviations of up to about 25° can occur. The angular deviation between the church axis and true east is called the Holy Alignment. This present study presents the possibility that the nave is oriented towards the direction of the sun-rising point on the name day of the patron saint of the church. If several saints share the patronage, the Holy Alignment equals the algebraic sum of the angular distances for each saint. The orientation of a nave can be analyzed by means of common mathematical relations used in geodesy, astronomy and gnomonics. In order to perform such an analysis, it is necessary to know the history of the patronage of the church; the Gauss-Krüger coordinates of the ground plan; and characteristic astronomical quantities at the time the church was built. A calculated example with the saints Andrew, James and Philip for the year 980 illustrates the analysis. An appendix deals with the influence of atmospheric refraction on the apparent altitude of the sun near the horizon.     

南岭花岗岩重力场特征与找矿意义

南岭地区是我国重要的有色、稀有金属矿产资源产地,是世界上研究燕山期花岗岩成岩成矿理论最典型的地区之一。该地区多金属矿床与花岗岩侵入关系密切,因此,研究花岗岩的空间分布特征对于成矿规律以及成矿远景预测有重要意义。南岭花岗岩密度较围岩低,呈明显重力负异常特征,本文首先建立直立柱体花岗岩的重力正演模型,通过改变模型参数来分析南岭花岗岩局部重力异常的特征;然后对南岭地区实测布格重力异常采用滑动平均法分离出局部重力异常和区域重力场,并对其特征进行了分析;最后选择过骑田岭、香花岭等地区典型剖面,通过二度半人机交互反演方法得出花岗岩体的形态与侵位特征,得知大型花岗岩体下底延深不超过25km,其侵位机制大多受深大断裂控制,说明南岭花岗岩侵入体属浅源型。     

西藏多龙矿集区遥感异常提取与成矿预测

以西藏多龙斑岩型铜矿区为例,根据已知矿床,分别利用比值法和主成分分析法对ETM＋和ASTER数据提取铁染与羟基异常信息,分析研究已知矿体遥感异常特征;通过波谱特征拟合的方法,对研究区进行波谱分类。利用两方面的成果来对多龙矿集区作成矿预测,划定远景成矿区,其中一级预测区6个,二级预测区12个。多种异常对比组合,能够发现更好的指示成矿线索的信息。