七星河金矿床地质特征及找矿方向     

汪明灿  衣存昌 《矿产与地质》2003,17(4):536-539

七星河金矿床是老柞山大型金矿床外围的一小型矿床，矿床的形成与地层、构造及岩浆岩活动有关，根据矿床分布规律可确定找矿方向。  相似文献   

应力状态改变对土压力影响的分析   总被引：1，自引：0，他引：1  

王报子  丁邦平 《安徽地质》2002,12(4):278-281

对基坑开挖引起地基土应力状态以及地下水状态改变给土压力计算带来的影响进行了深入的分析,提出了应采用侧压减少试验和卸荷试验方法确定的强度指标来计算主、被动土压力等计算方法.  相似文献   

Integrity of Local Ecosystems and Storm Water Management in Residential Areas     

WANG Lin WANG Weida GONG Zhaoguo 《中国海洋大学学报(英文版)》2006,5(4):363-367

1IntroductionPopulation growth has created escalating pressureson our resources(natural,humanandsocial)onlocal,regional,and global scales.These pressures negativelyi mpact the natural environment,our communities andthe quality of our lives.In the face of …  相似文献   

基坑水泥搅拌桩帷幕止水施工质量控制     

林福林 《福建地质》2007,26(3):193-198

基坑止水,对基坑(特别是深基坑)开挖及地下结构施工至关重要。根据多年的工程施工实践,总结和分析用于基坑开挖止水的水泥搅拌桩施工工艺流程和质量控制方面的有关问题。  相似文献   

填充沟屏障远场被动隔振三维分析   总被引：6，自引：0，他引：6  

高广运  李志毅  邱畅 《岩土力学》2005,26(8):1184-1188

把填充沟看作存在于弹性半空间的异质体,运用瑞利波散射的积分方程,对填充沟连续屏障远场被动隔振进行了三维分析,详细讨论了影响隔振效果的几个主要参数。研究表明,刚性材料比柔性材料具有更好的隔振效果,在隔振设计时应选择刚性屏障材料;填充沟的深度在一倍瑞利波波长内对隔振效果有较大影响,并且与宽度一起决定其隔振效果,但当屏障深度超过一倍瑞利波波长后,屏障深度对隔振效果的影响很小。  相似文献   

Trench infiltration for managed aquifer recharge to permeable bedrock     

Victor M. Heilweil  Dennis E. Watt 《水文研究》2011,25(1):141-151

Managed aquifer recharge to permeable bedrock is increasingly being utilized to enhance resources and maintain sustainable groundwater development practices. One such target is the Navajo Sandstone, an extensive regional aquifer located throughout the Colorado Plateau of the western United States. Spreading‐basin and bank‐filtration projects along the sandstone outcrop's western edge in southwestern Utah have recently been implemented to meet growth‐related water demands. This paper reports on a new cost‐effective surface‐infiltration technique utilizing trenches for enhancing managed aquifer recharge to permeable bedrock. A 48‐day infiltration trench experiment on outcropping Navajo Sandstone was conducted to evaluate this alternative surface‐spreading artificial recharge method. Final infiltration rates through the bottom of the trench were about 0·5 m/day. These infiltration rates were an order of magnitude higher than rates from a previous surface‐spreading experiment at the same site. The higher rates were likely caused by a combination of factors including the removal of lower permeability soil and surficial caliche deposits, access to open vertical sandstone fractures, a reduction in physical clogging associated with silt and biofilm layers, minimizing viscosity effects by maintaining isothermal conditions, minimizing chemical clogging caused by carbonate mineral precipitation associated with algal photosynthesis, and diminished gas clogging associated with trapped air and biogenic gases. This pilot study illustrates the viability of trench infiltration for enhancing surface spreading of managed aquifer recharge to permeable bedrock. Published in 2010 by John Wiley & Sons, Ltd.  相似文献   

基于ESDA的闽西发展不平衡格局动态分析   总被引：4，自引：2，他引：2  

陈文成 《地理与地理信息科学》2010,26(2)

区域发展不平衡格局动态涉及空间、时间、属性多维信息,根据1999-2007年闽西区域经济面板数据,构建空间时态数据库。筛选20项指标构建县域经济综合评价指标体系,进行县域经济粒度闽西区域发展变权法三维评价。在此基础上,从县域经济综合角度,应用基于空间探索分析的全局空间相关分析、热点分析及相应的局域统计分析等方法,通过探测县域经济空间联系模式挖掘闽西发展不平衡格局图式与动态,并利用时空一体化模型逼近。  相似文献   

探地雷达在探测玉树走滑断裂带活动性中的初步应用   总被引：4，自引：1，他引：3  

张迪  李家存  吴中海  钟若飞  田婷婷  张铎  刘晓东 《地质通报》2015,34(1):204-216

探地雷达具有快速、检测范围广、探测深度深、分辨率高及对地表环境无破坏等特点,在活动断层探测应用中具有很大的优势。在简要介绍玉树走滑断裂带活动性的基础上,选择高分辨率的探地雷达对隆宝、昔日达和盘琼沟处断裂带附近的活动断层进行探测。采用时间域有限差分法建立活动断层的数值模型对其雷达波响应特征进行模拟,分析断层在探地雷达剖面上的反射波特征。根据断层的反射波特征解译探地雷达图像,判断断层的位置、走向及空间展布。结合探槽开挖对比,探地雷达图像的解译结果与探槽开挖后的断裂带剖面展示的断层活动性质基本一致。根据隆宝、昔日达和盘琼沟处的探地雷达图像与探槽剖面上断层反射波特征的对比研究,解译了玉树地震震中位置探地雷达剖面上的断层展布。研究表明,探地雷达是一种快速探测活动断层的有效方法,尤其是在地表破裂不明显的区域,不仅可以准确地判断断层的位置、走向及空间展布,还可以将断裂带附近地下岩层的层位信息及探槽断面之外的地表下图像清晰地呈现出来,为以后运用探地雷达探测活动断层提供参考。  相似文献   

Late Quaternary Large Earthquakes on the Western Branch of the Xiaojiang Fault and Their Tectonic Implications   总被引：1，自引：0，他引：1  

LI Xi  RAN Yongkang  CHEN Lichun  WU Fuyao  MA Xinquan  CAO Jun 《《地质学报》英文版》2015,89(5):1516-1530

The Xiaojiang fault is a major active left-lateral fault along the southeastern margin of the Tibetan Plateau.The largest historical earthquake in Yunnan Province, with a magnitude 8 and a mean coseismic left-lateral displacement of ~ 6.9 m, occurred on the western branch of the Xiaojiang fault.Studying this fault is important in understanding current deformation and kinematic characteristics of the Tibetan Plateau.Activities and stretches have been well undertaken on the Xiaojiang fault, while paleoseismic research work is always the weak link on this fault.To investigate the paleoseismic history and large earthquake activity of the Xiaojiang fault, we opened a large trench at the northern edge of Caohaizi sag pond on the western branch of the Xiaojiang fault.Six paleoseismic events have been identified, and named E1 through E6 from the oldest to the youngest.Charcoal and woods are abundant, 20 samples were dated to constrain the ages of the paleoseismic events at 40 000–36 300 BC, 35 400–24 800 BC, 9 500 BC–AD 500, AD 390–720, AD 1120–1620 and AD 1750–present.We associate the youngest event E6 with the 1833 M8 earthquake.Events E4, E5 and E6 show a continuous record of the western strand of the Xiaojiang fault in the late Holocene, with a average recurrence interval of 370–480 yr.Large earthquake recurrence in the late Holocene is far less than the recurrence of 2000–4000 yr posed in previous studies.Thus, the seismic hazard on the Xiaojiang fault should be reevaluated.Furthermore, the irregular recurrence of large earthquakes on the Xiaojiang fault and other faults in the Xianshuihe-Xiaojiang system, indicates the uneven southeastward extrusion of the Sichuan-Yunnan block along the southeastern margin of the Tibetan Plateau.  相似文献   

断层崩积楔单片再生法光释光测年:以山西忻定盆地西田探槽为例   总被引：3，自引：0，他引：3  

赵俊香  任俊杰  于慎谔  张世民  丁锐 《现代地质》2011,25(2):356-362

为了研究断层崩积楔各部位沉积物光释光信号晒退情况及崩积楔形成年龄,利用中颗粒石英(63~90μm)单片再生法(SAR)对山西忻定盆地西田探槽断层崩积楔3个部位的4个样品进行光释光(OSL)定年。选择一代表性样品(08-OSL-22)进行等效剂量(DE)、LN/TN、循环比率、回授率与预热温度的关系分析,结果表明预热温度260℃、预热时间10 s为样品最佳预热条件。4个样品的测片循环比率基本在0.9~1.1之间,回授率均小于5%,表明所采用的中颗粒SAR法流程可以很好地校正测量过程中产生的释光感量变化,其等效剂量可信。利用等效剂量分布直方图和累积频率图,发现古地形面和坡积物的样品晒退均匀,崩积层样品则较差。对于晒退较差的样品利用累积频率法得到其等效剂量,从而得到崩积楔的近似年龄。最后获得该期崩积楔的形成年龄为(27.09±0.71)ka。  相似文献