缺乏资料条件下倒灌河段流速的近似确定方法   总被引：1，自引：0，他引：1       下载免费PDF全文

华祖林  芮孝芳  黄国如  罗缙 《水科学进展》2001,12(2):210-214

倒灌河段受干流影响往往存在双向流动,其流速的确定与单一河道明显不同,对缺乏必要水文和地形资料的大量中小倒灌河段,使用数学模型或物理模型常常遇到困难.针对这一情形,本文采用物理模型,结合数学模型及多元回归分析方法,提出了确定倒灌河段最大流速的经验公式,具有一定的应用价值,为工程问题中倒灌河段流速确定作了有益的尝试.  相似文献   

Muskingum法及其分段连续演算的若干理论探讨   总被引：7，自引：2，他引：7       下载免费PDF全文

芮孝芳 《水科学进展》2002,13(6):682-688

根据水力学原理和洪水波运动理论,通过对Muskingum法的关键参数X与特征河长、扩散波动力方程和运动波数值扩散之间关系的分析,给出了X更为全面的物理解释;证明了Muskin gum法槽蓄方程是扩散波动力方程近似的表达;指出了Muskingum法演算公式在一定条件下是扩散波方程的二阶精度解。讨论了Muskingum法的使用条件和分段连续演算的必要性;应用Z 变换方法导出了Muskingum法的分段连续演算的汇流系数公式。  相似文献   

一次累积带降雹的雷达观测   总被引：4，自引：2，他引：4  

马振骅 《大气科学》1977,1(2):149-152

在冰雹云中存在水份累积带的理论的提出,不仅对于研究强对流云的结构、机制和冰雹形成条件具有理论上的意义,而且对于探讨人工影响冰雹云的方法具有实际的意义。因此这个理论提出以来,颇受各国云物理工作者和人工影响天气工作者的重视。冰雹是一种发展极为旺盛的对流云,它的结构和生命过程不仅同大、中尺度的天气背景有关,而且与地区、地形有密切的关系。对于具有不同结构特点的冰雹云使用不同的抑制方法,看来是应当的。  相似文献   

Geochemistry and Petrogenesis of the Tongshankou and Yinzu Adakitic Intrusive Rocks and the Associated Porphyry Copper-Molybdenum Mineralization in Southeast Hubei, East China   总被引：11，自引：0，他引：11  

Qiang Wang    Zhen-Hua Zhao    Zhi-Wei Bao    Ji-Feng Xu    Wei Liu  Chao-Feng Li  Zheng-Hua Bai  Xiao-Lin Xiong 《Resource Geology》2004,54(2):137-152

Abstract. The late Jurassic Tongshankou and Yinzu plutons in southeast Hubei have been investigated for their contrasting metal mineralization features. The former is closely associated with porphyry Cu‐Mo mineralization, while the latter is barren of metal mineralization, althouth both are located very close to each other. The Tongshankou granodiorite porphyries and the Yinzu granodiorites are geochemically similar to adakites, e.g., high Al₂O₃ and Sr contents and La/Yb and Sr/Y ratios, enriched in Na₂O, depleted in Y and Yb, very weak Eu anomalies and positive Sr anomalies. However, different geochemi‐cal characteristics exist between the two plutons: the Tongshankou adakitic rocks (1) are relatively enriched in SiO₂, K₂O, MgO, Cr, Ni, and Sr and depleted in Y and Yb; (2) have higher degree REE differentiation; (3) have positive Eu anomalies in contrast with very weak negative or unclear Eu anomalies in the Yinzu rocks; and (4) isotopically have relatively higher eP_Nd(t) values (‐5.19 to ‐5.38) and lower initial ⁸⁷Sr/⁸⁶Sr ratios (0.7060 to 0.7062), while the Yinzu adakitic rocks have relatively lower eP_Nd(t) values (‐7.22 to ‐8.67) and higher initial ⁸⁷Sr/⁸⁶Sr ratios (0.7065 to 0.7074). The trace element and isotopic data demonstrate that the Tongshankou adakitic rocks were most probably originated from partial melting of delaminated lower crust with garnet being the main residual mineral whereas little or no plagioclase in the source. On the contrary, the Yinzu adakitic rocks were likely derived from partial melting of thickened lower crust, with residual garnet and a small quantity of plagioclase and hornblende in the source. Interactions between the adakitic magmas and mantle peridotites possibly took place during the ascent of the Tongshankou adakitic magmas through the mantle, considering that MgO, Cr, and Ni contents and eP_Nd(t) values of the adakitic magmas were possibly elevated and initial ⁸⁷Sr/⁸⁶Sr ratios were possibly lowered due to the contamination of mantle peridotites. In addition, the Fe₂O₃ of the adakitic magmas was likely released into the mantle and the oxygen fugacities (?_o2) of the latter were obviously possibly raised, which made metallic sulfide in the mantle oxidized and the chalcophile elements such as Cu were incorporated into the adakitic magmas. The ascent of the adakitic magmas enriched in Cu and Mo will lead to the formation of porphyry Cu‐Mo deposit. Nevertheless, the Yinzu adakitic magmas were possibly lack of metallogenetic materials due to not interacting with mantle peridotite, and thus unfavorable to metal mineralization.  相似文献   

Alkaline syenites in eastern Cathaysia (South China): link to Permian–Triassic transtension     

Qiang Wang  Jian-Wei Li  Ping Jian  Zhen-Hua Zhao  Xiao-Lin Xiong  Zhi-Wei Bao  Ji-Feng Xu  Chao-Feng Li  Jin-Long Ma 《Earth and Planetary Science Letters》2005,230(3-4):339-354

Two alkaline syenite plutons, the Tieshan and Yangfang plutons, have recently been recognized within NE-trending fault zones in eastern Cathaysia, South China. The rocks are very enriched in K₂O (6.28–9.39 wt.%), rare earth elements (REE; particularly light REE) and large ion lithophile elements, but are relatively low in high field strength elements. Isotopically, they are characterized by high initial ⁸⁷Sr/⁸⁶Sr (0.7093 to 0.7123) and low _Nd(t) values (−5.64 to −10.63). The geochemical data suggest that the alkaline syenites most likely formed via fractional crystallization of enriched mantle-derived magmas. Sensitive High-Resolution Ion Microprobe zircon U–Pb dating indicates that these two intrusions have Late Permian (254±4 Ma) and Early Triassic (242±4 Ma) crystallization ages, respectively. Our data suggest that a tectonic regime dominated by transtension probably existed from at least the latest Permian into the Triassic and was responsible for the formation of the Tieshan and Yangfang alkaline syenites. When combined with previous paleomagnetic, structural, and sedimentology data, we suggest that the transtension along the NE-trending strike-slip fault zones was related to oblique subduction of the Pacific plate underneath South China.  相似文献   

三维物性分布的位场计算   总被引：11，自引：3，他引：11  

冯锐 《地球物理学报》1986,29(4):399-406

本文在连续层状模型的基础上,将Parker位场公式推广到更具一般性的两种三维物性分布模型中。此时岩石的密度ρ和磁化强度J不仅在水平方向上可以任意变化,而且在深度上可依指数或线性函数形式变化。新的位场公式仍具有严密而简明的特点。结合圣安德烈斯断层带的重力反演,介绍了它的应用、模型分解和双界面同时反演的技术。  相似文献   

试论中国斑岩型矿床系列   总被引：2，自引：0，他引：2  

芮宗瑶  张洪涛 《地球学报》1986,8(3):89-100

斑岩型矿床具有特定了范畴和定义。根据我国已发现的斑岩型铜、钼、金、铀、铅锌、锡和稀土等矿床类型,可将斑岩型矿床系列划分为七个亚系列和十四个建造。与斑岩型矿床成因密切相关的热流体是多源的,按其性质可分为富氧富硫热流体和贫氧贫硫热流体两种类型。在特定的地质历史和地质背景下产出的斑岩型矿床具有重大差异。 斑岩型矿床只是浅成—超浅成条件下与长英质斑岩——热液体制有关的有用矿物堆积的一部分。在同一深部机制控制下,斑岩矿床可以与矽卡岩型矿床、脉状矿床以及其他热液矿床共存于同一矿区或矿田,它们之间往往具有内在联系。 本文旨在对斑岩型矿床提出简要的分类方案和讨论这些矿床的基本特征。  相似文献   

基于OLE海量空间数据管理系统的设计   总被引：1，自引：0，他引：1  

孙雅荣  芮建勋  陈能 《上海国土资源》2006,(3):40-42

以泰宁基础地理信息系统的开发为例,探讨了基于OLE技术的海量空间数据管理系统的设计与数据库访问机制,提供了一种管理海量空间数据的方法。  相似文献   

关于鲁西侏罗纪-白垩纪岩石地层单位使用之我见   总被引：4，自引：0，他引：4       下载免费PDF全文

李守军  洪铭  徐永梅  芮志锋  王金香 《地质论评》2007,53(1)

在中生代山东分为鲁东、鲁西、华北平原三个地层分区。鲁西地层分区在不同时期、不同研究者建立和使用了许多不同的岩石地层单位,使用比较混乱。本文对相关的岩石地层单位进行了讨论,提出了新的划分方案。侏罗系建议使用淄博群,划分为中、下侏罗统的坊子组和中、上侏罗统的三台组;白垩系建议使用下白垩统蒙阴组和西洼组;上白垩统固城组。其中固城组的时代根据所产化石由原来归为古新统而改为上白垩统。同时建议,废除“汶南(亚)组”和“分水岭(亚)组”,并且在鲁西地层分区不使用鲁东地层分区的“杨家庄组”、“曲格庄组”、“八亩地组”等岩石地层单位。  相似文献   

基于Oracle 10g实现多元空间数据管理     

魏华  芮小平  杜聪  熊金国 《物探化探计算技术》2007,29(4):353-358

地理信息系统中的多元空间数据包括专业化的空间数据(矢量数据和栅格数据)、属性数据,以及与之相关的各种多媒体数据。多元空间数据来源多样,数据量大,操作复杂,难以在传统关系数据库中存储管理。为了有效管理多元空间数据,在关系数据库中引入了数据对象,利用数据对象存取并操作多元数据,将地理信息系统应用中的各种多元空间数据,纳入到统一的系统框架内。基于对象关系数据库,提出了设计多元空间数据管理系统的完整思路。最后,利用最新的ORACLE10g数据库实现多元空间数据存储,使用ADO.Net连接数据库,实现了多元空间数据管理系统。  相似文献