某核反应堆预选区含水介质渗透性变化特征     

王建林  李晓 《地下水》2012,(1):45-47

在简要介绍预选区水文地质条件基础上,主要通过压水试验、抽水试验等水文地质试验得出各种水文地质参数从而分析预选区含水介质渗透性变化特征以及地层渗透性变化规律。  相似文献   

甘肃舟曲县庙儿沟泥石流形成条件及运动特征研究     

张旭光  张泽林  王志强  窦晓东  张永军 《甘肃地质》2012,(1):54-58

庙儿沟为白龙江中游右岸河段的一条沟谷,历史上曾发生多次泥石流。在查明泥石流形成条件的基础上,分析了庙儿沟泥石流的运动特征,包括泥石流的流速、流量、冲击力。这一结论为评价该泥石流对该地区居民的生命安全及财产的影响具有现实意义。建议右岸前期施工场地和右岸上游备料场沿江设置挡墙,且场地要注意少占行洪断面,防止泥石流沉积淤塞河道。  相似文献   

重庆及其周缘地区下古生界页岩气成藏条件及有利区预测   总被引：4，自引：1，他引：3       下载免费PDF全文

龙鹏宇  张金川  李玉喜  唐玄  程礼军  刘珠江  韩双彪 《地学前缘》2012,19(2):221-233

从野外地表露头、井下岩心及典型剖面等基础资料出发,以富有机质页岩形成地质背景及其展布特征-页岩气成藏条件-有利区预测为主线,对重庆及周缘地区下古生界页岩气成藏条件进行分析,并采用综合信息叠合法对该区有利区进行预测。指出研究区下寒武统筇竹寺组和上奥陶统五峰组—下志留统龙马溪组两套富有机质页岩普遍发育,分布广,厚度大,埋藏适中,有机质类型好,有机质含量高,具有充足的储集空间和运移通道,并且等温吸附模拟和现场解析实验也表明,这两套页岩均具有较强的气体吸附、较好的含气性能;多口井钻遇黑色页岩段气显异常普遍,也为页岩气的存在提供证据。总之,该区与美国东部典型页岩气盆地有诸多地质可比性,具有形成页岩气藏的有利地质条件,是页岩气勘探研究值得关注的重要领域。  相似文献   

DX14井区火山岩气藏水平井适应性分析     

李炜  李凡华  王彬  杨作明  郭建军 《四川地质学报》2012,(4):445-448

KL气田DX14井区为一火山岩气藏,现有4口水平井。通过对该区火山岩气藏水平井地质条件适应性和设计适应性进行分析,结合已投产2口水平井的生产情况,预测即将投产2口水平井生产效果。提出了该区水平井适应性的评价指标：1、应从气藏类型、气藏深度、气层有效厚度、气层各向异性指数等8个方面,来分析气藏水平井开发的地质适应性;2、认为该区水平井段应沿气层上部部署,水平段长度应根据火山岩体范围控制在600--800m左右,效果较好。  相似文献   

胶东金矿成矿构造背景探讨     

李洪奎  禚传源  耿科  梁太涛 《山东地质》2012,(1):5-13

在编制1∶50万山东省大地构造相图基础上,通过对大地构造相研究显示：胶东微地块是经多期增生和碰撞而形成的,其漫长的板块构造演化明显具有阶段性。侏罗纪是该区板块构造演化史上的一个重要转换期,构造演化由原来的南、北分异转变为东、西分异,胶东地区NE向新生构造起了主要作用。胶东地区中生代有2次重要的碰撞造山事件,印支造山作用主要表现为扬子板块向华北板块俯冲,形成苏鲁高压-超高压变质带及同造山花岗岩及后造山高碱正长岩;燕山造山作用的大陆动力学环境起源于中亚-特提斯构造域向滨太平洋构造域转化和太平洋板块的俯冲,在胶东地区表现为3次造山和3次伸展。晚侏罗世造山早期玲珑片麻状花岗岩组合是区域构造挤压导致地壳增厚引起地壳重熔的产物,代表了大陆弧花岗岩特征;早白垩世造山中期郭家岭花岗闪长岩-花岗岩组合代表了造山期大陆弧花岗岩的特点;造山晚期伟德山闪长岩-花岗闪长岩-花岗岩组合表现为大陆弧花岗岩,后造山A型崂山晶洞过碱性碱长花岗岩-正长花岗岩组合为大陆造陆隆升花岗岩与后造山花岗岩,代表燕山构造的结束。胶东地区构造-岩浆事件和金矿成矿作用受控于特提斯、古亚洲洋和太平洋三大构造域的相互作用,金矿形成的动力学背景是中生代构造体制转折和岩石圈减薄,起因与太平洋板块向华北板块的俯冲机制有关。  相似文献   

青海化隆基性-超基性岩带铜镍矿成矿条件与找矿潜力     

张照伟  李文渊  高永宝  郭周平  张江伟  李侃  张利忠 《西北地质》2012,45(1):140-148

青海化隆基性-超基性岩带是南祁连山一条重要岩带,其内产出若干基性-超基性岩体。通过对化隆基性-超基性岩带的基本地质特征及化隆群结晶基底的综合研究,结合已有研究成果及其相关其他地质信息,发现该基性-超基性岩带中的岩体都不同程度侵位于化隆群中,并具有相似的地质地球化学特征和成矿地质条件。加之带内几处典型的铜镍成矿表现,可见青海化隆基性-超基性岩带具有较好的铜镍成矿条件与找矿潜力。现有的野外工作及找矿实践亦表明了在巨厚红层覆盖下所发育的基性-超基性岩体表现了重要的铜镍矿化显示,同时提示在化隆基性-超基性岩带还有发现新的同类型岩体和铜镍矿床的潜在条件,其资源潜力较好。  相似文献   

Geographical Conditions and National Strategies   总被引：3，自引：0，他引：3  

Dadao Lu 《地球科学进展》2020,35(3):221-230

This paper is a summary based on the relationship between national conditions and development strategies for decades of consulting research. Through cases, the paper outlined the basic meaning of national conditions and geographical conditions and their close relationship with national development strategies, and emphasized the importance of comprehensive thinking and scientific judgment in the process of carrying out the governments’ strategies and development policies, and making development policies. At last, suggestions were made that the points of China’s national conditions and the rules of connection with government decision-making should be written into geography textbooks as well as into textbooks for party schools of the Communist Party of China.  相似文献   

Abundance,distribution, and feeding patterns of juvenile coho salmon (Oncorhynchus kisutch) in the Juan de Fuca Eddy     

Suzan S. Pool  Richard D. Brodeur  N. Lynn Goodman  Elizabeth A. Daly 《Estuarine, Coastal and Shelf Science》2008

The Juan de Fuca Eddy is a seasonal, counter-clockwise gyre off the mouth of the Strait of Juan de Fuca between Washington, USA and British Columbia, Canada that may provide favorable feeding habitat for juvenile coho salmon (Oncorhynchus kisutch) during their early marine existence. In late September 2002, physical and biological sampling was conducted along two transects of the eddy region. Surface rope trawling was conducted to capture juvenile salmon and other nekton, along with bongo and neuston net tows to examine potential mesozooplanktonic salmon prey. Presence of the Juan de Fuca Eddy was confirmed with vertical water profiles. In addition, nutrient and chlorophyll a concentrations collected from 3-m depth were within the range observed in previous studies within the eddy region. In the mesozooplankton community, euphausiids, chaetognaths, and decapod megalopae were common. In the diet of juvenile coho salmon, euphausiids and decapod megalopae were dominant by percent number, and larval and juvenile fish were dominant by percent weight. Feeding intensity (percent body weight) based on stomach contents was variable, but not significantly different among stations. To compare the Juan de Fuca Eddy region with an upwelling area, we sampled along a transect off La Push (LP), Washington, USA which is south of the eddy. The eddy region was found to be less productive than the LP transect. Nutrients were lower, chlorophyll a concentrations were higher, and zooplankton abundance was generally higher along the LP transect than in the eddy region. In addition, more juvenile coho salmon were captured from the LP transect than the eddy region. Prey items in stomachs of salmon from the LP transect were heterogeneous compared to those from the eddy region. Feeding intensity along the LP transect was slightly lower and more variable than in the eddy region, and differences in feeding intensity among LP stations were significant. In addition, feeding intensities among stations nested within regions were significantly different.  相似文献   

The relationship between rock glacier and contributing area parameters in the Front Range of Colorado     

Jason Janke  Regula Frauenfelder 《第四纪科学杂志》2008,23(2):153-163

Rock glaciers are an end unit of the coarse debris system that links frost weathering and rockfall to debris transport in mountainous environments. By examining topographic and climatic controls on creep, a better understanding of rock glacier formation and evolution could be obtained. A series of statistical tests were run comparing contributing area parameters (width, length, area, slope, headwall height, etc.) and rock glacier variables (width, length, area, thickness, slope, creep and temperature) in the Front Range of Colorado. Results showed that rock glacier width had the strongest correlation with contributing area width due to an abundance of lobate rock glaciers (r = 0.78). Rock glacier area and contributing area size were also related (r = 0.74), but are also a function of talus production factors. Mean surface velocity appears to be better correlated with thickness (r = 0.58) and length (r = 0.62), rather than slope (r = 0.33). Mean annual air temperature had a stronger exponential relationship with maximum velocities (r = 0.76) compared to mean annual velocity (r = 0.60). Front Range rock glacier velocities tend to decrease with warming, suggesting that the volume of ice and debris, rates of shear in plastic layers, or melt water may have a greater influence on deformation. Copyright © 2007 John Wiley & Sons, Ltd.  相似文献   

室内模拟试验确定横向扩散系数的研究--以吉林市第二松花江某江段为例     

梁秀娟  刘耀莹  张文静  盛洪勋  肖长来  王德成  杜艳荣  兰盈盈  杨天行 《吉林大学学报(地球科学版)》2004,34(4):560-565

确定河流横向扩散系数的主要方法有经验公式法和河流示踪试验法.以室内模拟试验求横向扩散系数的方法是一种新的尝试,采用几何相似原理,通过不同流量、流速条件下的室内模拟试验,计算出与河流相应条件下的横向扩散系数,所得结果(0.086 m2/s)与同条件下现场分析计算的结果(0.079～0.088 m2/s)基本一致.模拟试验不仅克服了野外条件下示踪剂投放和测试条件的不便,还能够更好地研究不同水动力条件下污染物的扩散运移规律.  相似文献