华南两类不同成因花岗岩的铅同位素组成特征     

饶冰  沈渭洲 《岩石学报》1988,4(4)

本文论述了华南两类不同成因花岗岩的铅同位素组成特征。不同类型的花岗岩,具有明显不同的铅同位素组成。改造型花岗岩相对富放射成因铅,其铅同位素比值较高,Pb/~(204)Pb>72;且相对富铀铅而贫钍铅,~(208)Pb/~(206)Pb<2.1。同熔型花岗岩则反之。利用有关的铅同位素图解和参数,可对花岗岩的成因类型进行划分。岩石的铅同位素组成与其成岩物质来源的关系,可从铀(钍)铅同位素的演化得到解释。研究结果表明,花岗岩的铅同位素组成特征,能够提供有关成岩物质来源的信息,从而作为划分花岗岩成因类型的又一个稳定同位素标志。  相似文献   

内蒙正镶白旗岩体中长石的初步研究     

姚培琳  饶明辉 《华东地质学院学报》1989,12(1):7-17

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Latitudinal variation of air sea fluxes in the western Indian ocean during austral summer and fall     

M. R. Ramesh Kumar  L. V. Gangadhara Rao 《Boundary-Layer Meteorology》1989,48(1-2):99-107

Daily and zonal (latitudinal belt) averages of heat and momentum fluxes were computed using bulk aerodynamic formulae, from the meteorological parameters measured onboard M. S. Thuleland during the sixth Indian scientific expedition to Antarctica (26th November, 1986 to 22nd March, 1987). Both estimates showed significant variations, the momentum flux showing the largest variation. The maximum values of sensible and latent heat fluxes were observed over the 30°–40° S and 10°–20° S zones during the southern summer and fall respectively while the minimum values of latent heat flux were observed in the 60°–70° S zone for both seasons. The sensible heat flux minimum was observed in the 50°°60° S and 60°–70° S zones for summer and fall, respectively. Higher momentum flux values over the 40°–50° S zone in summer shifted to the 50°–60° S zone during fall.  相似文献   

Occurrence of thorite and radioactive zircon in syenite pegmatite,North of Ashwaraopet,Khammam district,Andhra Pradesh,India     

K. Surya Prakash Rao  R. S. N. Sastry  Gautam Roy 《Journal of Earth System Science》1989,98(2):183-187

This paper reports the occurrence of thorite and confirms the earlier find of radioactive zircon by Subbarao, Murali and others from syenite pegmatite in the Vinayakapuram-Kunavaram alkaline belt in the Khammam district of Andhra Pradesh, India. Thorite has also been found as residual concentrations in soil overlying the pegmatite.  相似文献   

Use of remote sensing in lineament analysis for tectonic evolution and resource study of a part of Vindhyan Basin,Jhalawar area,India     

S. M. Ramasamy  P. C. Bakliwal  K. L. V. Ramana Rao 《Journal of the Indian Society of Remote Sensing》1988,16(1):63-71

Synoptivity and the exemplified fracture systems exhibited by the space borne imagery data has helped in solving many of the geological enigma in various parts of the world. The study conducted, using such remotly sensed data, in Jhalawar anticline, part of Proterozoic Cratonic Vindhyan Basin, Rajasthan, India, led to infer the history of tectonic evolution of peribasinal deformation which has been a matter of controversy for a century and more. In Landsat MSS data the Jhalawar region displays a panorama of lineaments and their analysis through azimuthal frequency diagrams, isofracture, lineament incidence and lineament intersection incidence density maps shows that the mean orientation of the lineaments fall in NW-SE and NE-SW and the shape of the various lineament density contours also show NE-SW and NW-SE orientations. In aerial photographs the area exhibits four sets of lineaments in NE-SW, NW-SE, N-S and E-W directions. Amongst these the former two sets are expressed as wide open master fracture systems with prolific vegetation fills along them and the latter two sets are characteristically observed as thin vegetation linears with frequent strike slip faulting along them. The further analysis of these fracture/lineament systems derived from multi-level remote sensing data shows that the Jhalawar anticline, which followed the pattern of flexural slip fold mechanism, was evolved by horizontally disposed σ1 (greatest principal stress) and 3σ (least principal stress) with the former oriented in NE-SW and the latter aligned in NW-SE directions with vertically disposed 2σ. The inference of such palaeostress environment of the Jhalawar region lead in the identification of a buried rigid basement high southwest of Jhalawar anticline, beneath the Deccan pile and loci of ground water, silica sand and probable igneous plug.  相似文献   

Random-walk model studies of the transport and diffusion of pollutants in katabatic flows     

Ashok K. Luhar  K. Shankar Rao 《Boundary-Layer Meteorology》1993,66(4):395-412

The flow and turbulence quantities governing dispersion in katabatic flows vary with both height and downslope distance. This variation cannot be accounted for in conventional plume dispersion models. In this study, three random-walk models of varying complexity are formulated to simulate dispersion in katabatic flows, and their strengths and weaknesses are discussed. The flow and turbulence parameters required by these models are determined from a high-resolution two-dimensional katabatic flow model based on a turbulent kinetic energy closure. Random-walk model calculations have been performed for several values of source height and slope angle to examine the influence of these parameters on dispersion. Finally, we simulated the perfluorocarbon and heavy methane tracer releases for Night 4 of the 1980 ASCOT field study over a nearly two-dimensional slope in Anderson Creek Valley, California. The observed peak concentrations are generally well-predicted. The effects of the pooling of the drainage air could not be taken into account in our katabatic flow model and, consequently, the predicted concentrations decay much more rapidly with time than the observed values.  相似文献   

On the crosscorrelation between drought indices and solar activity     

G. Padmanabhan  A. Ramachandra Rao 《Theoretical and Applied Climatology》1990,41(1-2):55-61

Summary Crosscorrelation structure between solar activity and drought indices is investigated by analyzing the cross correlation of the residual time series of solar activity and drought indices. Double Sunspot Cycle, Zürich Sunspot number, Palmer's Drought Index and Drought Area Index data are used in the study. White residual series derived from the observed data series by using valid time series models are used for the crosscorrelation analysis. Weak correlations between solar activity and drought area indices are inferred. The lags of significant correlation appear to vary for the different time series used in the study.With 3 Figures  相似文献   

地球化学计算中误差传递分析的应用   总被引：1，自引：0，他引：1       下载免费PDF全文

徐伟彪  饶纪龙 《地质科学》1990,(2):187

 通过两个实例讨论了地球化学计算中的误差传递问题,对照了四种不同方法的潜力和限制,拓广了蒙特卡洛方法在相关变量分析中的应用,指出其在不同条件下总能用有限机时逼近合理结果,揭示出协方差矩阵法的特殊效益,可相对于独立初始变量展现中间变量的相关关系。  相似文献   

地球化学计算中误差传递分析的应用          下载免费PDF全文

徐伟彪  饶纪龙 《地质科学》1990,(2):187-193

通过两个实例讨论了地球化学计算中的误差传递问题,对照了四种不同方法的潜力和限制,拓广了蒙特卡洛方法在相关变量分析中的应用,指出其在不同条件下总能用有限机时逼近合理结果,揭示出协方差矩阵法的特殊效益,可相对于独立初始变量展现中间变量的相关关系。  相似文献   

Applications of Error Propagation Analyses to Geochemical Calculation     

徐伟彪  饶纪龙 《中国地球化学学报》1991,10(2):166-173

Two examples are given for comparing applications and limitations of four methods which can be used to deal with error propagation in geochemical calculations.The examples indicate that the Monte Carlo method can also be employed to evaluate the effect of covariance.A special function of the method for covariance matrix shown here can reveal the correlations of middle variables relative to the independent primary variables.  相似文献