遵义牛蹄塘组发现的多水硫磷铝石   总被引：2，自引：0，他引：2  

罗泰义  李晓彪  姚林波  朱丹 《矿物学报》2003,23(3):205-210

遵义牛蹄塘组黑色岩系发现的多水硫磷铝石主要产出在Ni-Mo多金属层的微裂隙中，偶尔在多金属层下部的黑色粉砂岩中以脉体形式产出。该矿物结构不稳定，结构中一部分水分子很容易失去，在X射线衍射鉴定时其特征谱线变化较大；在自然条件下存放一定时间后，样品具有稳定的X射线衍射特征。此外，对这些样品进行了红外光谱、热重和差热分析、TEM观测、化学分析和晶胞参数计算，与纤磷铝石进行了对比和讨论。  相似文献   

电子政务建设应注意军事应用的几个问题     

胡丹露 《测绘科学》2003,28(1):45-47

电子政务的运行模式必将促使国防动员、军队决策指挥 ,以及战场信息应用等环节发生相应的变化。建设电子政务将促进国防动员工作规范化、制度化 ,将创造条件实现政府对军队的信息支援 ,将有利于未来战争数字战场环境建设。建设电子政务系统和“数字城市”、“数字省区”时 ,应结合国防动员和信息支援的问题从顶层构架 ,统盘考虑军事应用 ,同时制定法规和标准  相似文献   

北京一次大风和强降水天气过程形成机理的数值模拟   总被引：23，自引：5，他引：23  

付丹红  郭学良  肖稳安  孙凌峰 《南京气象学院学报》2003,26(2):190-200

利用3维强风暴冰雹分档模式(IPA—HBM)对2001年8月23日北京的一次伴有大风、暴雨和冰雹的强对流天气过程进行模拟和分析，并与部分观测资料进行了比较分析。结果表明，该模式对此次强风暴的生命史、降水分布、降雹的大小等要素做了较好的模拟，并能够模拟出伴随强风暴过程所产生的强下沉气流和及地面强风速切变(下去暴流)。从云微物理学角度分析了此次局地性大风的形成原因，认为由高空冰雹粒子的拖曳产生的负浮力作用是促发强下沉气流产生的主要原因，其次是冰雹的融化和雨水蒸发冷却对下沉气流起加速作用，冰雹的拖曳和融化作用对下沉气流具有决定性作用。强风暴所产生的爆发性强下沉气流最终导致了局地大风的形成。  相似文献   

Gaussian curvature and the relationship between the shape and the deformation of the Tonga slab     

Sarah Nothard  Dan McKenzie  John Haines  James Jackson 《Geophysical Journal International》1996,127(2):311-327

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A Semianalytical Model to Predict Recovery of Light, Nonaqueous Phase Liquids from Unconfined Aquifers     

Dan W. Waddill  Jack C. Parker 《Ground water》1997,35(2):280-290

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潍坊"5.19"强对流天气过程分析     

鲁丹  王令军 《山东气象》2005,25(2):22-23

利用常规气象资料、T213实况分析资料、全国雷达拼图资料、济南多普勒雷达和潍坊本市雷达资料及自动站资料，对2003年5月19日一次强对流天气过程进行分析，结果表明，快速东移南下的横槽极其槽后的冷空气使不稳定层结加强，是触发此次对流发生的原因。而低层暖湿气流的存在为其发展提供了必要的动力和水汽条件。  相似文献   

对工程勘察信息化的几点认识     

王丹 《中国勘察设计》2005,(9):7-9

从信息技术的角度看,工程勘察实际上是一种“信息获取、信息理解和信息应用”的过程。作为一项技术和服务,工程勘察的信息化应由工程勘察业务信息化和工程勘察管理信息化两方面组成。工程勘察信息化的作用包括信息化辅助业务和管理、信息化支撑业务和管理以及信息化提升业务和管理三个层次。当前,有必要对工程勘察企业信息化的模式、工程勘察业务信息化提升的方式和工程勘察信息化的标准化等问题做进一步研究,以推动工程勘察信息化向深度和广度发展。  相似文献   

Geologic and geochemical study of the Picacho gold mine, California: gold in a low-angle normal fault environment     

Steven Losh  Dan Purvance  Ross Sherlock  E. Craig Jowett 《Mineralium Deposita》2005,40(2):137-155

The Picacho gold deposit, located in southeasternmost California, is a low-grade gold deposit in a nearly flat-lying denudational fault of regional extent and probable Oligocene age. The deposit is hosted by intensely fractured and faulted Mesozoic leucogranite and by chloritic augen gneiss and schist, and is overlain unconformably and in fault contact by unmineralized late Oligocene Quechan volcanic rocks. The deposit is structurally characterized by normal and normal-oblique faults of low to high dip at shallow depths in the mine, merging downward with a synchronous, low-dipping ore-stage extensional fault system (the Chocolate Mountains/Gatuna Fault) of probable Oligocene age in deeper portions of the deposit. The fault system was infiltrated during much of its active life by hot, dilute, highly exchanged meteoric water having temperatures of 170°–210° C, salinity <2 wt% NaCl equivalent and calculated δ¹⁸O_fluid between −2.6‰ and 5.2‰. This main-stage fluid precipitated quartz, pyrite, and specular hematite, accompanied by silicification and sericitization. Auriferous ore-stage pyrite was precipitated late in the fault evolution probably by mixing of reducing ore fluid with relatively oxidized main-stage fluid during regional Oligocene extension on the Chocolate Mountains/Gatuna Fault. The Picacho deposit is characterized by a gold–arsenic–antimony geochemical signature consistent with bisulfide complexing of gold in reducing fluid, in contrast with typical denudation fault-hosted base-metal-rich deposits associated with high-salinity fluids elsewhere in the southwestern United States. The deposit is overprinted by Miocene normal faults having a wide range of dips. These postore faults are associated with red earthy hematite precipitation, pyrite oxidation, and supergene enrichment of gold. Editorial handling: L. Meinert  相似文献   

Probabilistic landslide susceptibility mapping in the Lai Chau province of Vietnam: focus on the relationship between tectonic fractures and landslides   总被引：4，自引：0，他引：4  

Saro Lee  Nguyen Tu Dan 《Environmental Geology》2005,48(6):778-787

This study evaluates the susceptibility of landslides in the Lai Chau province of Vietnam using Geographic Information System (GIS) and remote sensing data to focus on the relationship between tectonic fractures and landslides. Landslide locations were identified from aerial photographs and field surveys. Topographic, geological data and satellite images were collected, processed, and constructed into a spatial database using GIS data and image-processing techniques. A scheme of the tectonic fracturing of crust in the Lai Chau region was established. Lai Chau was identified as a region with many crustal fractures, where the grade of tectonic fracture is closely related to landslide occurrence. The influencing factors of landslide occurrence were: distance from a tectonic fracture, slope, aspect, curvature, soil, and vegetative land cover. Landslide prone areas were analyzed and mapped using the landslide occurrence factors employing the probability–frequency ratio model. The results of the analysis were verified using landslide location data and showed 83.47% prediction accuracy. That emphasized a strong relationship between the susceptibility map and the existing landslide location data. The results of this study can form a basis stable development and land use planning for the region.  相似文献   

松花江上游地区汞污染的化学生态效应   总被引：5，自引：0，他引：5  

王宁  朱颜明  朴明玉  孟丹 《地理科学》2005,25(6):737-741

采样分析了吉林省东部松花江上游金矿开采区及其附近水、土壤、动植物及河流沉积物样品中汞的含量，发现河流沉积物中汞的污染相当严重；受其影响当地的植物和两栖类动物——中国林蛙体内总汞和甲基汞含量也明显高于对照组。实验表明，林蛙内脏对汞的富集能力大于肌肉；秋季对汞的富集大于春季；河流沉积物中甲基汞的含量与林蛙体内甲基汞的含量有较好的正相关。汞污染的来源与区域内个体金矿的滥采滥排有直接关系，表明人类活动所产生的有毒重金属在地表过程中出现了化学生态效应。  相似文献