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91.
吴敬炳 《华东地质学院学报》1986,(2)
本文以寻找铀矿为目的,在该岩体140Km~2面积上进行水化学普查,发现水异常370个,其特征为:若异常多且成片出现,则预示着有单个矿体规模不大的矿体群存在;条带状展布的水异常预示着存在方向相同的矿化带;阻水阻气构造带近旁之异常预示水源上方存在矿化;水温偏高之水异常与矿化关系密切;与矿化有关的多为铀—氡混合异常;大构造处之水异常并不表示此构造存在矿化,面往往是在其附近次一级构造中成矿. 相似文献
92.
A study on two closed salt lake basins, Tal Chapar and Parihara in the eastern margin of the Thar Desert, Rajasthan, was carried
out to unravel late Quaternary geomorphic evolution of these saline lakes. Both lakes are elliptical in shape bordered by
stabilised dunes, and are oriented in a NE-SW direction, i.e., in the direction of the prevailing summer monsoon wind. Both
lakes have been formed in the wind-shadow zones of isolated hills of Precambrian quartzite. Our study indicates that the late
Quaternary sediments in the lakes began with the cyclic deposition of laminated fine silt layers (0.5 m thick), rich in organic
matter, alternating with ripple cross-bedded sand layers (each ∼1.5–2 m thick). Sand layers that are moderately sorted are
separated by laminated silt-clay layers with gypsum/calcite and this unit occurs in the upper most 4 m sequence in deeper
sections. The presence of gypsum crystals within the laminated sediments suggests a high concentration of Ca in the inflowing
water.
At Parihara Lake the organic carbon-rich sediments at 95 cm depth was dated to 7,375 + 155/−150 year BP. At Tal Chapar radiocarbon
dates of 7,190 + 155/−150 and 9,903 + 360/−350 was obtained from the sediments rich in organic carbon occurring at a depth
of 1.35 m and 1.80 m, respectively. The study reveals strong hydrologic oscillations during the past ∼14,000 year BP (13,090 + 310/−300 year
BP).
Quaternary geomorphic processes, especially the strong aeolian processes during dry climatic phases, played a major role in
the formation of the lake basins, as well as the fringing linear dunes. Geochemical and mineralogical analyses of the lacustrine
sediments, supported by radiocarbon dates indicate the existence of an ephemeral lake earlier than ∼13,000 year BP as sediments
began to be deposited in a lacustrine environment implying sustained runoff in the catchments. A freshwater lake formed between
9,000 year and 7,000 year BP. The lake dried periodically and this strong fluctuating regime continued until about ∼7,000 year
BP. Mid-Holocene was wet and this was possibly due to higher winter rains A saline lake existed between 6,000 year and 1,300 year
BP and finally present day semi arid conditions set in since 1,200 year BP. Remnants of a habitation site (hearth and charred
bones) on stabilised dune at Devani near Tal Chapar were dated to 240 ± 120 year, while that at Gopalpura was dated to 335 ± 90 year.
These historical sites on stabilised dunes were, according to the local accounts, settlements of people who used the lake
brine for manufacturing salt. 相似文献
93.
94.
基于等高线数据的地性线追踪技术研究 总被引:11,自引:0,他引:11
通过研究特征点的提取技术和建立系统的特征点匹配的数学模型,研究了基于矢量等高线数据的地性线的自动追踪技术,利用所述方法,提取的特征点完整,准确;理论和实验表明,所建立的数学模型简捷,实用,有可靠的数学理论基础,且地性线追踪效果良好。 相似文献
95.
低序次断裂是地壳变形的直接产物,具有丰富的构造变形信息,经过转换的低序次构造。形式多样,图案复杂,是构造研究的重要对象,也是地表稳定性研究的重要基础。利用香港地区航空雷达图像资料,提取其中低序次构造的弱信息,建立转换变形模型,以分析区内不稳定地表的构造背景。区内北东向断裂是主要构造,其右行剪切形成一系列低序次R面,P面,R^1面构造,在雷达图像上表现为线性弱信息并且与微地貌发育有关。利用线性构造增强,提取技术和低序次构造组合分析方法,结合野外地质调查,确定马鞍山地区EW向的张性破裂是NE向张剪断裂的转换,是造成马鞍山滑坡的重要地质因素。 相似文献
96.
铜山铜矿床矿化类型可划分为层状含铜黄铁矿型,含铜角砾岩型,含铜夕卡岩型和含铜班岩型,控矿因素为地层,岩浆岩及构造,其中层间断裂与接触带构造是主要的容矿构造,铅,硫,氢,氧同位素特征及成矿温度研究表明矿物质和热液主要来源于铜山岩体,矿床成因为层控夕卡岩型铜矿床。 相似文献
97.
98.
M. I. Todorovska S. S. Ivanovi M. D. Trifunac 《Soil Dynamics and Earthquake Engineering》2001,21(3):705
For transient, high frequency, and pulse like excitation of structures in the near field of strong earthquakes, the classical design approach based on relative response spectrum and mode superposition may not be conservative. For such excitations, it is more natural to use wave propagation methods. In this paper (Part I), we review several two-dimensional wave propagation models of buildings and show results for theoretical dispersion curves computed for these models. We also estimate the parameters of these models that would correspond to a seven-story reinforced concrete building in Van Nuys, California. Ambient vibration tests data for this building imply vertical shear wave velocity βz=112 m/s and anisotropy factor βx/βz=0.55 for NS vibrations, and βz=88 m/s and βx/βz=1 for EW vibrations. The velocity of shear waves propagating through the slabs is estimated to be about 2000 m/s. In the companion paper (Part II), we estimate phase velocities of vertically and horizontally propagating waves between seven pairs of recording points in the building using recorded response to four earthquakes. 相似文献
99.
A new formulation is proposed to model pounding between two adjacent structures, with natural periods T1 and T2 and damping ratios ζ1 and ζ2 under harmonic earthquake excitation, as non‐linear Hertzian impact between two single‐degree‐of‐freedom oscillators. For the case of rigid impacts, a special case of our analytical solution has been given by Davis (‘Pounding of buildings modelled by an impact oscillator’ Earthquake Engineering and Structural Dynamics, 1992; 21 :253–274) for an oscillator pounding on a stationary barrier. Our analytical predictions for rigid impacts agree qualitatively with our numerical simulations for non‐rigid impacts. When the difference in natural periods between the two oscillators increases, the impact velocity also increases drastically. The impact velocity spectrum is, however, relatively insensitive to the standoff distance. The maximum relative impact velocity of the coupled system can occur at an excitation period Tn* which is either between those of the two oscillators or less than both of them, depending on the ratios T1/T2 and ζ1/ζ2. Although the pounding force between two oscillators has been primarily modelled by the Hertz contact law, parametric studies show that the maximum relative impact velocity is not very sensitive to changes in the contact parameters. Copyright © 2001 John Wiley & Sons, Ltd. 相似文献
100.
利用发展的包含海洋表面边界展和大气辐合反馈过程的热带太平洋海气耦合距平模式,对ENSO循环进行了模拟。通过30a积分,用合模式所展示的热带太平洋海气耦合系统的ENSO循环的水平结构演变特征和观测事实甚为一致,成功地模拟出了ENSO循环的冷暖态的发生发展、衰亡及相互转换等各个位相的动力和热力场的水平结构及其对季节循环的依赖性特征。本文数值模拟结果表明,ENSO循环的主要动力学过程可由热带海气相互作用系统自身所确定。ENSO循环的正确模拟是揭示其形成机制的前提。 相似文献