应用计算机进行固体矿产储量计算,提高地质工作水平     

张文宽  徐洪恩  谯小平  杨本锦 《四川地质学报》2007,27(1):75-76

Windos XP版储量计算程序是作者90年代DOS版的全面升级。该程序按照目前地质工作普遍采用的公式和做法,符合现行规范规定和要求。程序对储量计算中矿体圈定等难点解决较好。该程序已经多个矿区应用检验,最近又为南非英铂公司采用推广。  相似文献   

公路隧道围岩地质条件评价方法及其富溪隧道应用研究     

朱正国  乔春生  高保彬 《工程地质学报》2007,15(6):789-795

为了达到快速、准确、可靠的围岩分类,有效指导隧道施工,在充分研究和吸取国内外有关围岩分类的经验和成果基础上,针对隧道施工期间的围岩类别鉴定方法,提出了一种可用于隧道施工期间围岩类别鉴定的快速分类方法,该方法以定量与定性相结合、多专家评分的方式在开挖掌子面现场进行观察、量测及评价,无需复杂试验或测量以及繁杂计算,可迅速得出评价结果。为了更加全面地反映隧道围岩情况,准确评价围岩工程性质,结合目前国际上流行的Q分类系统,在富溪隧道第一手实测资料的基础上,根据快速分类结果和Q指标分类结果对富溪隧道围岩条件进行综合评价,为其隧道施工提供了合理的支护参数。  相似文献   

Mesoproterozoic Earthquake Events and Breakup of the Sino-Korean Plate   总被引：3，自引：0，他引：3       下载免费PDF全文

QIAO Xiufu GAO Linzhi PENG Yang 《《地质学报》英文版》2007,81(3):385-397

In the Mesoproterozoic time, the northern part of the Sino-Korean Plate experienced a period of intensive tectonic extension and breakup. 1. An abundance of sedimentary earthquake records is preserved in the Chuanlinggou, Tuanshanzi and Gaoyuzhuang formations in the Mesoproterozoic Changcheng System （1800-1400 Ma） and in the Mesoproterozoic Wumishan Formation of the Jixian System （1400-1000 Ma）. These earthquake records are characterized by various liquefied sand-veins, carbonate microspar and coarser spar veins, limestone dikes, liquefied breccia and various forms of liquefied contorted bedding. This deformation is always associated with synsedimentary faults and igneous activity. 2. Three liquefaction models for soft carbonate sediments are recognized, including liquefaction in laminated carbonate rocks, liquefaction in thin-bedded carbonates and large-scale liquefaction along huge carbonate dikes. 3. Based on the record of earthquake and volcanic activities, the Sino-Korean Plate experienced at least twice intraplate breakups. One occurred between 1800-1400 Ma, and the other occurred at about 1200 Ma. The last breakup resulted in formation of the Yan-Liao aulacogen, a tectonic zone characterized by deeper material vibrancy, active faults, major igneous activity and frequent earthquakes.  相似文献   

新疆伊吾县马依当地区二叠纪地层的发现及其意义     

白龙  石远华  石磊  谯文浪 《贵州地质》2007,24(2):134-137,141

在新疆伊吾煤矿一带1:5万区域地质矿产调查中,首次在原定石炭系上统妖魔梁组中发现大量透镜状钙质结核,并具明显的陆相冲积扇沉积特征;通过该地层的大量孢粉鉴定属为二叠世晚期,故将原石炭系上统妖魔梁组更名改为库莱组。其时代定为晚二叠世。并初步探讨了它的地质意义。  相似文献   

卫星光学相机MTF在轨检测方法研究     

王先华  乔延利  易维宁 《遥感学报》2007,11(3):318-322

调制传递函数是反映卫星光学相机成像性能的重要参数,针对调制传递函数多种在轨检测方法,本文在分析了可利用地面景物的基础上,结合目前卫星光学相机分辨率不断提高的现状,着重从原理和方法上介绍了利用不同亮度地块接壤的地面靶标进行检验的刃边法,同时依据实验研究成果,介绍了对原始刃边数据拟合和调制传递函数的频谱增密技术,这些技术对提高调制传递函数获取精度具有重要的作用。  相似文献   

兴隆60 cm望远镜主焦CCD系统测光性能的研究     

石火明  乔琪源  胡景耀  林清 《中国天文和天体物理学报》1998,(1)

对兴隆６０ｃｍ望远镜主焦ＣＣＤ系统的测光性能进行了测试和研究．测定了ＣＣＤ快门时间函数,讨论了快门延迟效应对短时间曝光观测的可能影响．通过观测大批Ｌａｎｄｏｌｔ标准星,较准确地定出了ＢＶＲＩ宽带测光的星等系统转换关系,结果表明本系统与标准ＢＶＲＩ系统很接近．对ＣＣＤ系统的天文测光精度作了仔细的检验和分析,并对ＰＳＦ拟合测光和孔径测光两种方法进行了比较  相似文献   

珠江三角洲城市化进程中耕地面积的变化特征分析   总被引：23，自引：1，他引：22  

黄宁生  朱照宇  乔玉楼  孙大中 《热带地理》1998,18(4):296-301

讨论了１９８０－１９９５年珠江三角洲地区７个主要城市在城市化进程中耕地面积的变化特点;分析了城市化发展的不同阶段以及不同速度与耕地面积减少之间的关系。以耕地面积减少系数为主要指标,总结出珠江三角洲地区基于耕地资源利用特征的４种城市化模式。研究发现,部分城市出现的耕地资源过度消耗现象,不应简单地归因于城市化发展,而主要与当地城市发展规划和管理工作不力有关。  相似文献   

从地方病和环境污染性疾病看微量元素与钙的关系   总被引：1，自引：0，他引：1  

李广生  井玲 《矿物岩石地球化学通报》1998,(2)

从地方病和环境污染性疾病看微量元素与钙的关系李广生井玲（白求恩医科大学,长春１３００２１）关键词微量元素钙地方病环境污染性疾病我国几种主要地方病都与一定的微量元素有关,这已为大家所熟知。而值得重视的是,除了微量元素之外,它们又都在某些环节上与宏量元素...  相似文献   

由土卫九(Phoebe)轨道数值改进求解土星质量     

沈凯先  乔荣川 《时间频率学报》2007,30(1):62-67

为测定土星质量,对收集到的1905年至2006年期间的686次观测[其中包括182次照相观测和504次CCD(电荷耦合器件)观测]通过数值积分进行拟合来改进土星的暗弱的外卫星Phoebe的轨道,并得到土星系总质量msa的新的测定值:3 497.0-1msun(太阳质量),为更精确地测定土星质量提供了一个有价值的参考值。  相似文献   

Spatial scale effect on seasonal streamflows in permafrost catchments on the Qinghai–Tibet Plateau     

Genxu Wang  Guangsheng Liu  Lin'an Liu 《水文研究》2012,26(7):973-984

The scale issue is of central concern in hydrological processes to understand the potential upscaling or downscaling methodologies, and to develop models for scaling the dominant processes at different scales and in different environments. In this study, a typical permafrost watershed in the Qinghai‐Tibet Plateau was selected. Its hydrological processes were monitored for 4 years from 2004 to 2008, measuring the effects of freezing and thawing depth of active soil layers on runoff processes. To identify the nature and cause of variation in the runoff response in different size catchments, catchments ranging from 1·07 to 112 km² were identified in the watershed. The results indicated that the variation of runoff coefficients showed a ‘V’ shape with increasing catchment size during the spring and autumn seasons, when the active soil was subjected to thawing or freezing processes. A two‐stage method was proposed to create runoff scaling models to indicate the effects of scale on runoff processes. In summer, the scaling transition model followed an exponential function for mean daily discharge, whereas the scaling model for flood flow exhibited a linear function. In autumn, the runoff process transition across multiple scales followed an exponential function with air temperature as the driving factor. These scaling models demonstrate relatively high simulation efficiency and precision, and provide a practical way for upscaling or downscaling runoff processes in a medium‐size permafrost watershed. For permafrost catchments of this scale, the results show that the synergistic effect of scale and vegetation cover is an important driving factor in the runoff response. Copyright © 2011 John Wiley & Sons, Ltd.  相似文献