陕西省勉略宁地区铅-锌矿地质特征及找矿方向     

王启  周静庭  王晖 《矿产与地质》2006,20(4):389-391

勉略宁“三角地区”铅-锌矿可分为晚古生代海底热水喷流沉积型及元古代岛弧火山喷流沉积型两种类型，前者产于勉略古缝合带中，与秦岭褶皱带断陷盆地内铅-锌矿有一定的可对比性；后者产于元古代火山基底内，成矿与火山机构关系密切。以成矿构造背景为依据，结合已知矿床的分布和主要成因类型，区内可划分为关地门-两河口、东沟坝-银硐山及刘家坪-孟家梁三个铅-锌多金属成矿带，指出了不同区带的找矿方向。  相似文献   

Element diffusion ability in metasomatic agents and its effect on chemical characteristics of metasomatized peridotites     

Y S O’Reilly 《中国科学D辑(英文版)》2006,49(9):926-937

The partial melting and metasomatism are two most important geological processes of changing chemical compositions of mantle. Extracting partial melt from primitive mantle leads residual mantle to deplete in- compatible elements, whereas the metasomatism …  相似文献   

胶东西北部玲珑、郭家岭超单元花岗岩成因探讨   总被引：3，自引：0，他引：3  

常裕林  郑小礼  王晖 《地质找矿论丛》2006,21(Z1):90-94

玲珑、郭家岭超单元花岗岩的源岩均为胶东岩群变质岩;玲珑超单元花岗岩表现出岩石的不均匀性,其成因为原地、半原地交代-重熔型花岗岩;郭家岭超单元花岗岩则属于有幔源物质参入的同熔型花岗岩.两个花岗岩均经历了多期构造-岩浆作用,最终形成于燕山期;郭家岭超单元最终形成晚于玲珑超单元花岗岩.  相似文献   

森林冠层上下湍流谱结构和耗散率   总被引：3，自引：1，他引：2  

刘树华  刘和平  X.Mei  M.Y.Leclerc  朱廷曜  金昌杰  洪钟祥  李军  刘辉志 《中国科学D辑》1998,(5)

利用新型三维超声风速 /温度仪 ,根据在长白山原始森林冠层上下两个高度上测量的湍流资料 ,采用涡动相关法计算和分析了森林冠层上下湍流谱的结构、局地各向同性和耗散率 .结果表明 ,在惯性副区 ,归一化湍流谱遵从 - 23的指数规律 ;在森林冠层上 ,尽管谱的形状与均匀表面的一致 ,但是 ,大气湍流是非各向同性的 ;而在森林冠层内则是近似各向同性的 ;森林冠层上下湍流能量和热量耗散率比典型草原和牧场的结果大 ,揭示了森林粗糙表面在湍流输送过程中的动力扰动和对大涡的破碎作用  相似文献   

地球自转长期稳定性的一种解释     

M. A. Richards  Y. Ricard  C. Lithgow-Bertelloni  G. Spada  R. Sabadini  李世愚 《世界地震译丛》1998,(2)

古地磁数据显示了在古地磁和热点参照系之间的不到1000km的运动,即100Ma(百万年)期间的真极移,它意味着地球自转轴一直是相当稳定的。这个长期的自转稳定性可以用晚中生代和新生代的大规模板块运动的缓慢变化来解释,只要俯冲带的岩石层是地幔对流导致的地幔密度不均匀性的主要部分。因此,不需要引入其他诸如自转不规则的缓慢再调整之类的机制,就可以解释所观测到的缓慢的真极移。  相似文献   

CONCENTRATION AND FLUX OF CO_2, TURBULENCE FLUXES AND RADIATION BALANCE IN THE NEAR SURFACE LAYER OVER WHEAT FIELD     

刘树华  Leclerc.M.Y.  徐梅  麻益民 《Acta Meteorologica Sinica》1998,(2)

The gradient of CO_2 concentration, photosynthetically active radiation (PAR). net radiation.soil heat flux, profiles of wind speed, and air temperature and humidity were measured above awheat field during May and June 1985 at Beijing Agro-Ecosystems Experimental Station. Beijing,China. Fluxes of carbon dioxide, sensible heat, latent heat and momentum were calculated byusing the aerodynamic method. The observation site. equipment, calibration techniques, theerrors associated with the measurement, and the computational procedures are described. Theresults show that the diurnal variations of amplitude of CO_2 concentrations were 103.8 to 27. 0. 86.3 to 22.8 and 69.8 to 11.6 ppm: the average CO_2 concentrations were 331.5. 339.9 and 364.6 ppmfor the photosynthesis type, and 369.6. 364.0 and 375.2 ppm for the respiration type at 1. 2 and10 m above surface, respectively, from May 14 to June 15. In the daytime, transfer direction ofthe CO_2 fluxes and gradients is from air to crop canopy, and at noon (1100 to 1300 BT (BeijingTime)) the transfer rate reaches negative maximum value. At night, transfer of CO_2 fluxes andgradients is in the reversed direction and reaches positive maximum in the early morning (0400 to0600 BT). There are strong negative correlations between CO_2 flux and the net radiation (Rn),available energy (H LE). photosynthetically active radiation (PAR) and momentum flux (τ).  相似文献   

THE FLOODS AND DROUGHTS OF THE LOWER YANGTZE VALLEY AND THEIR PREDICTIONS     

K.Y.Cheng. 《地理学报(英文版)》1935,(3)

During Ching dynasty from 1644 to 1911, an interval of 268 years, there occurred in the lower Yangtze valley 197 floods and 156 droughts. The most serious droughts came in 1785, 1814, and 1856; and the most disastrous floods in 1680, 1823  相似文献   

A Comparlson between North Shensi basin&Szechuan basin     

BY C.Y.HSIEH 《地理学报》1934,(2)

One of the most conspicuous feature in Chinese geomorphology is the similardevelopment of some topographic forms such as basins, plateaus etc. betweenthe north and the south China. The basin of North Shensi in the north and  相似文献   

Modelling of sediment movement in the surf and swash zones     

TOKPOHOZIN N. B.  KOUNOUHEWA B.  AVOSSEVOU G. Y. H.  HOUEKPOHEHAM A.  AWANOU C. N. 《海洋学报(英文版)》2015,34(2):137-142

Under the action of marine currents, non-cohesive sediments evolve by bed-load, by saltation or suspension depending on their granulometry. Several authors have considered that the movement of sediment...  相似文献   

Analysis of karst aquifer spring flows with a gray system decomposition model   总被引：1，自引：0，他引：1  

Hao Y  Yeh TC  Wang Y  Zhao Y 《Ground water》2007,45(1):46-52

There are approximately 470,000 km(2) of karst aquifers that feed many large springs in North China. Turbulent flow often exists in these karst aquifers, which means that the classical ground water model based on Darcy's law cannot be applied here. Ground water data are rare for these aquifers. As a consequence, it is difficult to quantitatively investigate ground water flow in these karst systems. The purpose of this study is to develop a parsimonious model that predicts karst spring discharge using gray system theory. In this theory, a white color denotes a system that is completely characterized and a black color represents a system that is totally unknown. A gray system thus describes a complex system whose characteristics are only partially known or known with uncertainty. Using this theory, we investigated the karst spring discharge time series over different time scales. First, we identified three specific components of spring discharge: the long-term trend, periodic variation, and random fluctuation. We then used the gray system model to simulate the long-term trend and obtain periodic variation and random fluctuation components. Subsequently, we developed a predictive model for karst spring discharge. Application of the model to Liulin Springs, a representative example of karst springs in northern China, shows that the model performs well. The predicted results suggest that the Liulin Springs discharge will likely decrease over time, with small fluctuations.  相似文献