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31.
宫同伦 《地球科学与环境学报》1991,(1)
本文用动力成矿观点对小秦岭金矿田富矿体的形成提出了新的解释,对本区的动力成矿特点作了较详细的说明。文中联系到地壳演化的不同阶段对金矿的富化过程进行了较深入的讨论,并提出了新的成矿系列。笔者以基础地质、大地构造和同位素年龄资料为依据对小秦岭金矿田含金石英脉的成因提出了与前人不同的新观点,认为它是晋宁晚期岩浆期后热液矿床。 相似文献
32.
We describe two new species of Sellaphora from Lake Fuxian, Yunnan Plateau, China. Based on both light and scanning electron microscopy, these species are described
as S. yunnanensis sp. nov. and S. sinensis sp. nov. The primary features of S. yunnanensis are: elliptical to linear-elliptical valves with broadly rounded ends, straight filiform raphe, almost straight central endings
and small, slightly expanding central pores, small central area, symmetrical or slightly asymmetrical central nodule. The
primary features of S. sinensis are: elliptical valves, obtusely rounded ends, similar raphe and axial area, transapically less expanded central area, larger,
elliptical central nodule. We compare these species to those of a similar shape and morphology. 相似文献
33.
在远场正演计算的基础上,运用30°~90°的四个不同深源远震记录波形,通过试错法选取台站下方的结构,借助波场反向重建算法,反演确定宜昌台站下方的速度结构。这一算法的实现有助于提高用试错法所得结果的可靠性和精确度,对于利用天然地震资料研究地球深部构造有一定的实用价值。 相似文献
34.
X. Jia T. S. Zha J. N. Gong B. Wu Y. Q. Zhang S. G. Qin G. P. Chen W. Feng S. Kellomäki H. Peltola 《水文研究》2016,30(6):972-985
During the last decade, the widely distributed shrublands in northern China have shown significant signs of recovery from desertification, the result of widespread conservation practices. However, to support the current efforts in conservation, more knowledge is needed on surface energy partitioning and its biophysical controls. Using eddy‐covariance measurements made over a semi‐arid shrubland in northwest China in 2012, we examined how surface energy‐balance components vary on diurnal and seasonal scales, and how biophysical factors control bulk surface parameters and energy exchange. Sensible heat flux (H) exceeded latent heat flux (λE) during most of the year, resulting in an annual Bowen ratio (β, i.e. H/λE) of 2.0. λE exceeded H only in mid‐summer when frequent rainfall co‐occurred with the seasonal peak in leaf area index (LAI). Evapotranspiration reached a daily maximum of 3.3 mm day?1, and summed to 283 mm yr?1. The evaporative fraction (EF, i.e. λE/Rn), Priestley–Taylor coefficient (α), surface conductance (gs) and decoupling coefficient (Ω) were all positively correlated with soil water content (SWC) and LAI. The direct enhancement of λE by high vapour pressure deficit (VPD) was buffered by a concurrent suppression of gs. The gs played a direct role in controlling EF and α by mediating the effects of LAI, SWC and VPD. Our results highlight the importance of adaptive plant responses to water scarcity in regulating ecosystem energy partitioning, and suggest an important role for revegetation in the reversal of desertification in semi‐arid areas. Copyright © 2015 John Wiley & Sons, Ltd. 相似文献
35.
Acta Geotechnica - In this paper, a simple but feasible approach is proposed to predict the time-dependent load carrying behaviours of jacked piles from CPTu measurements. The corrected cone... 相似文献
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主要研究武汉地区小当量爆破(即矿山爆破)事件与小震级(ML 2.0左右)地震事件的识别与判据. 相似文献
39.
This paper investigates in detail the peak frequency of gyrosynchrotron radiation spectrum with self and gyroresonance absorption
for a model of nonuniform magnetic field. It is found that the peak frequency shifts from lower frequency to higher frequency
with increases in the low-energy cutoff, number density, input depth of energetic electrons, magnetic field strength and viewing
angle. When the number density and temperature of thermal electrons increase, the peak frequency also shifts to a slightly
higher frequency. However, the peak frequency is independent of the energy spectral index, high-energy cutoff of energetic
electrons and the height of the radio source’s upper boundary. It is also found for the first time that there is a good linear
correlation between the logarithms of the peak frequency and the low-energy cutoff, number density, input depth of energetic
electrons, magnetic field strength, and viewing angle, respectively. Their correlation coefficients are higher than 0.95 and
the standard errors are less than 0.06. 相似文献
40.
东准噶尔双泉金矿LA-ICP-MS锆石U-Pb测年及赋矿岩石地球化学特征 总被引:1,自引:0,他引:1
为了解双泉金矿成矿时代及成矿环境,分别对双泉金矿含金石英脉和赋矿岩石进行采样测试分析。高精度LA-ICP-MS锆石U-Pb法测年结果表明,双泉金矿含金石英脉加权平均206Pb/238U年龄为(303.53±0.79)Ma,代表了含金石英脉形成年龄,属晚石炭世前后挤压推覆构造体系产物。与双泉金矿主成矿期年龄对比,结合矿区成矿条件及黄铁矿、毒砂等矿物形态特征,认为该金矿的形成不是一期结果,而是经历了预富集、富集的演化历程。赋矿岩石地球化学分析结果表明,岩石的SiO2、K2O、CaO(SiO2=58.82%~89.25%,K2O=1.12%~4.47%,CaO=0.52%~4.47%)含量高,Na2O含量低(Na2O=0.43%~1.76%),A/CNK值大于1,δ值小于3.3,属过铝质、钙碱性岩石,具富钾钙、贫钠镁特点;Ba相对Rb,Th亏损,K2O含量接近活动陆缘K2O含量,TiO2含量与岛弧TiO2含量接近,推断岩体形成于活动陆缘或岛弧环境;稀土元素具弱的负Eu、负Ce异常,(La/Sm)N值较(Gd/Yb)N值大,轻稀土元素分馏程度高于重稀土元素,表明岩浆具壳幔混熔特点。东准噶尔后碰撞阶段早石炭世至二叠纪晚期发生的陆-陆碰撞造山及伸展张弛构造运动可能是造成此结果的主要构造因素。 相似文献