中国碳硅泥岩型铀矿地球化学指示元素特征及异常模式     

付锦  赵宁博  裴承凯  李新春 《铀矿地质》2014,(5):298-304

根据全国铀矿资源潜力评价项目研究成果,在大量研究我国碳硅泥岩型铀矿地球化学异常特征的基础上,总结了一套对碳硅泥岩型铀矿勘查稳定且行之有效的指示元素及其组合,确定了碳硅泥岩型铀矿地球化学异常模式,并以实例说明。  相似文献   

云南南秧田钨矿床流体包裹体特征及其意义   总被引：3，自引：0，他引：3  

冯佳睿  周振华  程彦博 《岩石矿物学杂志》2010,29(1):50-58

对南秧田矽卡岩型钨矿床的石英和石榴石流体包裹体的岩相学特征研究表明,与成矿有关的包裹体主要有3类:富液相、富气相和含子晶的多相包裹体。石英包裹体均一温度范围为232～337℃,盐度w(NaCl)=0.53%～9.98%;石榴石包裹体的均一温度范围为228～306℃,盐度w(NaCl)=6.45%～14.04%。激光拉曼探针分析表明,南秧田白钨矿的成矿流体中气相成分以H2O为主,含少量CO2、CH4、H2S和N2等气体,液相成分以H2O为主,属NaCl-H2O流体体系。成矿溶液的密度为0.72～0.87g/cm3,表明形成这种矽卡岩型矿床的成矿流体均属于中温、低盐度、低密度的流体。成矿压力为18～32MPa,成矿深度约为0.6～1.2km。石英包裹体水的δD为-72.16‰～-65.10‰,δ18O为7.98‰～8.45‰,钨矿床中硫化物δ34S为6.6‰。成矿流体主要来自燕山晚期的岩浆热液作用。  相似文献   

应用新古典增长模型研究湛江经济发展问题     

李飞星  王波 《广东海洋大学学报》2005,25(5):60-64

运用产出增长率模型对湛江的主要行业的增长率和劳动份额进行了测算,分析了湛江经济增长不均衡及其经济增长率低下的原因,并提出了以工业为主导、发展旅游、贸易、农林牧副渔资源加工等资金积累型产业和加速农村城镇化和机械化的见解。  相似文献   

卡拉高莱斯油田U油组储层特征及其评价     

李喜安  吴少波  谭成仟  宋子齐 《地球科学与环境学报》2002,24(3):36-40

以取心井的毛管压力曲线等分析资料为基础 ,结合储层物性测井参数解释结果 ,对卡拉高莱斯油田U油组储层从岩性组成、物性特征、孔隙类型及孔隙结构、非均质性等方面进行了综合评价。认为该储层为一套中高孔、中高渗储层 ,其物性主要受沉积微相、粒度中值、泥质含量等因素影响 ,其层内、层间和平面非均质性均较强。  相似文献   

瞬变电磁测深快速拟地震解释方法及应用效果     

李貅  郭文波  胡建平 《地球科学与环境学报》2001,23(3):42-45

详细讨论了电磁波与地震波在介质中的传播规律.根据瞬变电磁测深(TEMS)中心回线装置观测成果与大地电磁测深(MTS)成果的一致性,提出了瞬变电磁资料拟地震解释的思路.大量理论模型的正、反演计算结果表明方法理论是正确的,野外实测资料处理结果进一步说明了该方法的实用性.  相似文献   

大理机场雷暴特征及潜势预报分析          下载免费PDF全文

毕波  高兵  杨航 《中低纬山地气象》2020,44(6):71-75

利用大理机场5年天气观测资料和FNL 1.0X1.0数据,对大理机场雷暴特征及潜势预报进行分析,结果发现：大理机场全年各月都有可能出现雷暴天气,雷暴天气主要出现在6~9月,每年7月和8月雷暴天气出现最为频繁;雷暴天气持续时间0~1小时的次数最多,持续时间1~2小时的雷暴也比较常见,持续时间4~6小时的次数较少,没有出现持续时间6小时以上的雷暴;雷暴可以出现在大理机场的任何方向,出现在东边的次数最多,出现在天顶的次数最少;雷暴初期平均在1月31日,雷暴终期平均在11月14日,雷暴的初期和终期年际差别较大。选取对流有效位能、500hPa相对湿度、0度层高度、近地表四层等压面的抬升指数和可降水量作为预报因子建立大理机场雷暴预报方程,预报方程是显著的,有较好的雷暴潜势预报能力。  相似文献   

Towards hydrological triggering mechanisms of large deep-seated landslides   总被引：3，自引：3，他引：0  

Roberta Prokešová  Alžbeta Medveďová  Petr Tábořík  Zora Snopková 《Landslides》2013,10(3):239-254

It is a widely accepted idea that hydrologically triggered deep-seated landslides are initiated by an increase in pore-water pressure on potential slip surface induced by rising groundwater level after prolonged period of intense rainfall although the process is not fully understood. In order to contribute to better understanding, the rainfall–groundwater relationships, hydrogeological monitoring and repeated geoelectrical imaging were carried out from March 2007 to April 2011 in large deep-seated landslide near ?ubietová (Western Carpathians) catastrophically reactivated at the end of February 1977. Based on our observations, groundwater level (GWL) response to precipitation differs considerably with respect to both overall hydrological conditions and GWL mean depth. While the rate of GWL increase up to 25 cm/day were measured after some rainfall events during wet periods, noticeably lower recharge rate (up to 1–2 cm/day) and delayed GWL response to rainfall (usually from 2 weeks to 2–4 months) were observed at the beginning of the wet season after considerable depression of GWLs due to previous effective rainfall deficit. Likewise, slow GWL fluctuations without short-term oscillations are typical for deeper GWLs. Thus, long-term (several seasons to several years) hydrological conditions affect markedly groundwater response to rainfall events in the studied landslide and can be crucial for its behaviour. Comparison of hydrological conditions characterising the analysed period with those that accompanied the landslide reactivation in 1977 allow us to assume that slightly above-average rainy season following the prolonged wet period can be far more responsible for movement acceleration (and possibly failure initiation) in deep landslides than the isolated season of extreme precipitation following a longer dry period. This is true especially for landslides in regions with significant seasonal temperature changes where potential effective precipitation (PEP), calculated as excess of precipitation (P) over potential evapotranspiration (PET), may be efficiently used for estimation of slope saturation condition.  相似文献   

小净距隧道爆破开挖中夹岩累积损伤计算方法及其应用   总被引：1，自引：0，他引：1  

孟凡兵  林从谋  蔡丽光  李博 《岩土力学》2011,32(5):1491-1494

为了获得小净距隧道中夹岩爆破累积损伤规律,建立了爆破荷载作用下中夹岩累积损伤新计算方法,并应用该方法对大坪山隧道中夹岩爆破施工过程中的累积损伤进行预测,同时进行了现场测试验证。结果表明,新计算方法不仅能反映爆破力学作用过程,而且计算参数也易于获取;预测结果与实测平均误差在12%左右,可以用来预测岩石的累积损伤;大坪山隧道中夹岩累积损伤规律为二次爆破后6个测孔波速平均降低率为4.3%;各测孔最大累积损伤增量为6.1%。其结果可为小净距隧道中夹岩稳定性研究提供依据  相似文献   

Imaging the Mariánské Lázně Fault (Czech Republic) by 3-D ground-penetrating radar and electric resistivity tomography     

Tomá? Fischer  Petra ?těpan?íková  Magda Karousová  Petr Tábo?ík  Christina Flechsig  Mahmoud Gaballah 《Studia Geophysica et Geodaetica》2012,56(4):1019-1036

Geodynamic activity in the area of West Bohemia is typified by the occurrence of earthquake swarms, Quaternary volcanism and high flux of mantle-derived CO₂. The highest swarm activity occurs beneath the eastern edge of the Cheb basin, which is delineated by the NW-SE trending morphologically pronounced Mariánské Lázn?? Fault (MLF) controlling the formation of the basin. The previous trenching survey across the MLF zone has identified several fault strands with possible Quaternary activity. In this paper we present the results of the geophysical survey focused to trace the faults signatures in geophysical sections and to build an image of near surface tectonics. The method of electric resistivity tomography (ERT) along two profiles parallel to the trench identified a strong resistivity contrast between the bodies of sandy gravels in the middle and conductive clayey sands to the west and weathered crystalline basement to the east. The 2-D ground penetration radar (GPR) sections show direct correlation of reflections with lithological boundaries identified in the trench. As expected, the GPR signal amplitudes increase with the resistivities found in the ERT sections. Two of the four faults identified in the trench are indicated in the resistivity and GPR sections. A 3-D GPR measurement has identified a spot of high amplitudes elongated parallel to the MLF trend, which coincides with the high resistivity body. To improve the signal-to-noise ratio of the time slices we stacked the GPR time slices within vertically homogeneous blocks. This provided a contrast image of the sand-gravel body including its boundaries in three dimensions. The detailed analysis of the 3-D GPR cube revealed additional fault that limits the highly reflective sands and appears to be offset by another younger fault. Our results suggest a complex fault pattern in the studied area, which deserves a further study.  相似文献   

导航卫星历书参数拟合改进算法     

陈刘成  唐波  梁红梅 《天文学进展》2008,26(1):80-86

该文对导航卫星历书拟合问题进行了综合研究,结合J2项分析解,提出了一种新的卫星历书拟合方法和用户算法.该方法只需下列参数表示历书: Week、Toa、a、e,i、Ω0、ω0、M0,比正常的GPS卫星历书参数少一个:Ω.用户算法可以根据一阶摄动理论,由新历书参数a、e、i计算Ω,并对MEO、IGSO、GEO卫星的历书参数近地点角进行改进.通过多组模拟轨道和IGS精密轨道的历书拟合实验,结果表明采用新方法具有参数少、计算量少、迭代收敛快、拟合MEO卫星历书精度高等优点,同样适用于高轨GEO、IGSO卫星.  相似文献