Geochemistry and chronology of Se＇ ertengshan greenstone, Inner Mongolia

This paper deals with the meta-mafic volcanic rocks of the Gongyiming iron deposit at Baotou, Inner Mongolia. The major and trace elements and REE data indicate that the meta-mafic volcanic rocks occurred in the environment similar to a modern continental rift. Sm-Nd and Rb-Sr isotopic studies indicated that the meta-basic rocks were formed during the Early Neoarchean from 2800 Ma to 2900 Ma and reworked during the Late Neoarchean (2500 Ma) by metamorphism. Because of the separation of the North China Craton from the Siberia Craton during the Middle Proterozoic (1600 Ma), the Rb-Sr systematics of the rocks has been changed. The Se‘ ertengshan greenstone seems to occur during the Middle Archean. A stable continental crust may have existed during the Paleoarchean.     

弱透水层基坑降水实例分析

通过对基坑降水工程实例的现象及成因分析，提出弱透水层滞后疏干现象，并提出了在降水工程中合理应用的建议。     

广东河源白石冈岩体:一个高分异的I型花岗岩

广东河源白石冈岩体位于近东西向展布的佛冈花岗岩带的东端,主体岩性为中粗粒黑云母花岗岩,主要组成矿物为石英(25%～35%)、微纹长石(45%～50%)、斜长石(An=20～30,15%～20%)和黑云母(5%～10%)。锆石U-Pb定年结果表明其形成年龄为148.5±1.6Ma,属晚侏罗世岩浆活动的产物。化学成分上,该岩体铝弱过饱和,A/NKC值主要变化于1.0～1.1之间;富硅,富钾(K2O/Na2O=1.31～1.70),全碱含量中等偏低(K2O Na2O=7.44%～8.48%),碱铝指数(AKI值)为0.75～0.88,可归为高钾钙碱性岩系。微量和稀土元素组成上,岩体富Rb、Th、U、Pb和轻稀土,贫Ba、Sr、P、Ti,Rb/Sr比值高,K/Rb比值低,铕负异常显著(δEu=0.05～0.28),Nb、Ta、Zr、Hf等高场强元素含量及104×Ga/Al比值(2.43～3.26)较之典型A型花岗岩均偏低。岩体的εNd(t)值为-5.99～-7.51,TDM值偏低(1.42～1.54Ga),综合地球化学资料指示其应属高分异的I型花岗岩。结合对区域动力地质背景的全面分析,表明白石冈岩体形成于后造山的伸展引张环境,是由底侵的幔源基性岩浆及其诱发的长英质岩浆在深部岩浆房混合,并经高程度分离结晶的产物。     

Acoustic Borehole Images for Fracture Extraction and Analysis in Second Pre-pilot Drillhole of CCSD

INTRODUCTIONThesecondpre pilotdrillholeofChineseContinentalScientificDrilling (CCSD PPⅡ)ProjectislocatedintheeastofDabie Suluultra highpressuremetamorphic (UHPM)belt,andthesouthofSuluareainthenorthofMaobeiVil lage ,DonghaiCounty ,JiangsuProvince ,China .PPⅡwasdrilleddownto 10 2 8.6 8mdepthwith 75 .5cmbits ,andcasedatadepthof 6 9.5m .TheinvestigationintodrillcoresrevealsthatPPⅡpenetratesmetamorphicformations .Fivemajorlithologicalunitsareidentifiedasfollows :parag neiss,ortho…     

城市测绘成果数据库管理系统

本文介绍一种测绘成果数据管理系统，采用Ｆｏｘｐｒｏ２．５编写，只要用户准备好需要管理的控制点成果信息及图形信息，该系统就可以对给定的数据信息进行录入，修改，删除，查询，统计及打印操作，该系统功能齐全，具有很强的实用性。     

洪涝灾害灾情分析和评估的遥感方法研究

探讨了基于遥感和地理信息系统手段进行洪涝灾害灾情分析和损失估计的途径，研究了利用灾后一定时期内的遥感影像再现淹没状况的方法。     

四川会理巴松金矿地质特征及成因

从控矿因素、产出部位、蚀变矿物组合、自然金的特征、矿物包体特征等方面探讨了矿床成因。该金矿属中低温热液型金矿。     

2000年来我国旱涝气候演化的阶段性和突变

过去气候的突变以地质方法得到很多证据，但在历史时期则发现不多。本文利用文献档案资料建成2000年来的旱涝气候序列，发现280年和1230年前后有过两次突变。本工作着重给出突变前后的旱涝气候分布类型的差别，即从空间分布上探讨被突变界开的气候阶段所具有的特色，280～1230年间，我国气候大趋势是不稳定的，而且涝的界线一再受到NE-SW走向的等高线阻挡。气候突变事件的证据说明，气候系统的运动具有两种模式：渐变和突变。     

开采沉陷中的抽样定理及其应用

根据数字处理中的数学原理，提出了开采沉陷中的抽样定理。以此为基础，导出了地表移动观测站的合理点间距ｒ·其值为Ｈ（５ｔ），获得了以离散的地表移动观测值或预计值，恢复其连续性的地表移动变形值的计算公式。并以计算实例，给出了其计算方法。     

A Study of the Rhenium-Osmium Geochronometry of Molybdenites

This study deals with the first application of the isotope dilution - inductively coupled plasma mass spectrometry in the rhenium-osmium geochronometry in China. The chemical separation procedure included decomposition of samples by means of alkali fusion, extraction of rhenium by acetone and extraction of osmium by distillation. The recovery of both elements in the entire process was more than 90% . The blanks of analyses were 0.07 ng for rhenium and 0.01 ng for 187Os. The mineralization ages of molybdenites from four molybdenum deposits in China were determined by using this method, with a precision (2σ)of about ±3% . These results agree satisfactorily with their geological backgrounds. The Re-Os method can directly determine ages of metal deposits and reflect the true ages more reliably than other dating methods that only determine the ages of country rocks from which mineralization ages are inferred. As many hydrothermal sulphide deposits usually contain molybdenites, this method has bright prospe