我国北方前寒武区域变质岩区变质作用对镁铁云母成分的影响     

贺义兴  胡大千  范春光 《矿物学报》1987,(1)

辽宁鞍山、冀东、密云和内蒙古地区镁铁云母的寄主岩石类型有变沉积岩和变火山岩。其镁铁云母的Al_2O_3含量和Mg/(Mg+Fe~(2+))比值随寄主岩石类型不同而有明显的差异。而在同类寄主岩石中,镁铁云母的成分,特别是Mg/(Mg+Fe~(2+))比值,则随变质作用强度而出现规律性的变化。 研究表明,从鞍山-冀东-密云、内蒙古、变质作用强度(主要是温度)升高;在翼东水厂矿区,从南至北,变质作用强度也有增加的趋势。镁铁云母成分可为变质岩区的地层对比、确定构造形迹和找矿提供有益的信息。  相似文献   

An analytical method for determining shear stiffness of an inclined grouted bolt installed across an open discontinuity     

B. Stimpson 《Geotechnical and Geological Engineering》1987,5(3):299-305

Summary The shear stiffness of a grouted, rock bolt intersecting a discontinuity controls the amount of shear movement that can occur for a given shear force. In this paper an analytical model is developed for estimating the shear stiffness of a single bolt as a function of bolt inclination, hole and bolt diameter, bolt, grout and rock Young's moduli, and aperture (opening) across the discontinuity, and sensitivity studies conducted to determine the most significant of these variables as predicted by the model.  相似文献   

Case study of Pampa,Texas, multicell storms     

R. J. Hung  D. Y. Tsao  R. E. Smith 《Pure and Applied Geophysics》1983,121(5-6):1019-1034

Analysis of the Pampa, Texas, multicell storms showed prestorm environmental conditions of a strong horizontal convergence of moisture, mixing ratio 12 g/kg at the 850 mb level in the Texas Panhandle areas and strong winds with shear veering with height. Rapid-scan satellite imagery showed that the clouds penetrated above the tropopause and cloud-top temperatures were at least 4 to 9° C colder than the temperature of the tropopause. This formation and collapsing of high-mass-density overshooting cloud tops above the tropopause is characteristic of tornadoes in the middle portion of the United States.  相似文献   

The stability of underground workings in the soft rocks of the Coal Measures   总被引：2，自引：1，他引：2  

A. H. Wilson 《Geotechnical and Geological Engineering》1983,1(2):91-187

Summary The characteristics of soft rocks typical of the British Coal Measures are defined and a series of working hypotheses are developed to provide improved design methods for underground roadway and face supports and pillars in coal mines. Proposed design equations are tested against case history data.  相似文献   

岩溶地层水文水井泡沫钻井压力和排量计算          下载免费PDF全文

郑秀华夏柏如  陈庆寿 《探矿工程》2001,(6):45-48

分析了岩溶地层水文水井施工中,泡沫实现平衡压力或欠平衡压力钻井的原理及影响泡沫钻井有效井眼压力的因素,采用迭代法逆循环计算方法,计算井口压力和井口气液排量。  相似文献   

疏勒河流域中游生态环境变化及成因分析   总被引：7，自引：1，他引：6  

陈德华  刘少玉  王昭 《水文地质工程地质》2001,28(6):23-25

近三十年来,疏勒河流域中游地区生态环境不断恶化,主要表现为绿色生产严重退化,湿地面积缩小,盐碱地,沙地迅速增加。通过不同时段的遥感解译,分析了不同生态景观的定量变化及成因。恶劣的地理环境加上人类活动对水资源利用量的不断增加是造成该区生态环境日趋恶化的主要因素。保护地下水平衡和合理用水结构,实行水资源优化管理,提高水的利用率是社会经济,环境可持续发展的有力保证。  相似文献   

Hydrodynamical Modeling Of Oceanic Vortices   总被引：1，自引：0，他引：1  

Xavier Carton 《Surveys in Geophysics》2001,22(3):179-263

Mesoscale coherent vortices are numerous in the ocean.Though they possess various structures in temperature and salinity,they are all long-lived, fairly intense and mostly circular. Thephysical variable which best describes the rotation and the density anomaly associated with coherent vortices is potential vorticity. It is diagnostically related to velocity and pressure, when the vortex is stationary. Stationary vortices can be monopolar (circular or elliptical) or multipolar; their stability analysis shows thattransitions between the various stationary shapes are possible when they become unstable. But stable vortices can also undergo unsteady evolutions when perturbed by environmental effects, likelarge-scale shear or strain fields, -effect or topography. Changes in vortex shapes can also result from vortex interactions. such as the pairing, merger or vertical alignment of two vortices, which depend on their relative polarities and depths. Such interactions transfer energy and enstrophy between scales, and are essential in two-dimensional and in geostrophic turbulence. Finally, in relation with the observations, we describe a few mechanisms of vortex generation.  相似文献   

内蒙古中西部多岛海构造演化   总被引：10，自引：0，他引：10  

高计元  王一先  裘愉卓  张乾 《大地构造与成矿学》2001,25(4):397-404

内蒙古中西部大陆由一个微大陆、三条弧后盆地和三条火山岛弧,即华北微大陆、白云鄂 傅弧后盆地、白乃庙火山岛弧、温都尔庙弧后盆地、苏尼特左－锡林浩特火山岛弧、贺根山弧后盆 地和二连浩特－锡林郭勒火山岛弧组成。经过了长期而复杂的微大陆和火山弧的裂解、弧后盆地 的消减衰亡及弧－陆和弧－弧碰拉等构造演化,才最终形成今天所见到的这种构造样式。  相似文献   

西藏易贡崩塌——滑坡—泥石流的地质地貌与运动学特征   总被引：4，自引：0，他引：4  

任金卫  单新建  沈军  格桑  扎桑  邓桂英  张军  索仁 《地质论评》2001,47(6):642-647

2000年4月9日19时59分18.2秒,在西藏自治区波密县境内易贡乡发生了特大崩塌—滑坡—泥石流。构造上它发生在印度板块阿萨姆楔入角复合地带的西侧,也是高原腹地向东侧山地下降的过渡带,重力作用明显。根据便携式GPS定位仪实地测定和滑坡前后的卫星影像分析,崩塌—滑坡—泥石流堆积物形成了一座长约5.7km、宽约1.5km的“天然大坝”,完全堵塞了易贡藏布河干流,崩塌滑坡体总方量超过3.8×10~8m~3。根据区域地震台网的记录,其振动持续的时间为6min,其中最大振幅的持续时间为2min。震相分析表明有3组较为明显的震相,对应着3次较大的地表振动。计算获得崩塌滚落的平均速度约为48m/s,伴随崩塌滚落的同时,滑坡泥石流的平均滑动速度也达到了16 m/s,比一般泥石流流动速度要大一倍。  相似文献   

混合沉积和混积岩的讨论   总被引：36，自引：6，他引：30  

沙庆安 《古地理学报》2001,3(3):63-66

混合沉积物是指陆源碎屑与碳酸盐(包括异化粒等)在沉积上的混合。混合沉积可分为狭义的和广义的,狭义的是指陆源碎屑与碳酸盐组份的混合(在同一岩层内),而广义的混合则包括了狭义的和陆源碎屑与碳酸盐层构成交替互层或夹层的混合。混合沉积很早就引起了人们的注意,尽管碎屑岩和碳酸盐岩的研究与应用已很成熟,但对混积岩的研究多被忽视了。对狭义的混合沉积物有必要起一成因名称——混积岩。当人们接触到混合沉积时,除了分析研究它们的组分和结构特征外,还必须去思考,它们为什么能经常频繁地交互出观,或是直接混合在一起?倒底是：①陆源碎屑跑到碳酸盐的沉积背景里?②碳酸盐跑到陆源碎屑的沉积背景里?③二分别从各自的源地跑到第三种沉积背景里?还是④二本来就在同一沉积背景里?接下来就要思考是什么动力条件使它(们)能从这个沉积背景(环境)“跑”到另一个沉积背景(环境)里去?是水?是风?是自身?还是别的什么力量?那么,又是怎样的水动力或风动力条件呢?是正常条件,还是突发事件?很明显,要分析研究混合沉积和混积岩。这些问题就不得不细细加以考虑,深入进行研究。  相似文献