应用SAR特征匹配方法估计音苏盖提冰川表面流速

喀喇昆仑山区冰川因位于高海拔地区且远离人类正常活动的区域,使得连续的表面流速的地面观测很难实施,因此,对该区域冰川运动机理研究相对比较少.采用日本高级陆地观测卫星携带的相控阵型 L 波段合成孔径雷达(Advanced Land Observing Satellite,Phase Array L-band Synthet...     

玉龙斑岩铜矿带莽总含矿斑岩体岩石学特征及锆石U-Pb年龄研究

莽总斑岩铜钼矿床位于玉龙斑岩铜矿带中部,含矿岩体侵入下二叠统和上三叠统火山岩和硅质沉积岩中.含矿岩体出露面积约0.27km2,普遍发生蚀变,可分为早晚两个阶段.本文分析了含矿岩体化学组成及用锆石LA-ICP-MS U-Pb 年龄分析斑岩体形成时代.早阶段岩体主要为花岗闪长斑岩,晚阶段岩体为石英二长斑岩及碱长花岗斑岩,晚...     

迟缓爱德华氏菌OppA蛋白的免疫原性及免疫保护分析

迟缓爱德华氏茵(Edwardsiella tarda)是水产养殖动物重要的病原茵,引起鱼类爱德华氏茵病,免疫防治是针对该病的一个有效途径.OppA是迟缓爱德华氏茵的一个寡肽透过酶组分,作者开展OppA的免疫原性及免疫保护性的研究,旨在评价其作为鱼类爱德华氏菌病疫苗候选抗原的可行性.将致病性的迟缓爱德华氏菌LSE40的o...     

Geochemistry and genesis on saturated hydrocarbon of crude oils in Gas Hure Oilfield in Qaidam Basin

Gas Hure Oilfield is the biggest one in the Qaidam Basin.Through intensive sampling and GC-MS analysis,the authors analyzed the geochemical characteristics of the crude oils in the Gas Hure Oilfield.The results show that the crude oils have even-odd carbon predominance for n-alkanes.In shallow reservoir,part of crude oils suffered biogenic degradation.As for normal oils,they have low Pr/Ph ratios with abundant gammacerane and C35 homohopane,which indicate that the crude oils are formed in strong reducing sa...     

基于灰色自记忆模型的城市月需水量预测

建立了以灰色微分方程为动力核的自记忆模型,并首次应用于城市月需水量预测.先将具有季节性特征的实测历史数据通过季节指数法获得相对平滑的序列,再用所建灰色自记忆模型进行模拟、预测.研究表明,灰色自记忆模型建模方法简单且模拟和预测精度较为满意,平均相对误差为5.74％,灰色GM(1,1)模型预测平均相对误差是8.77％,其精...     

青海虎头崖多金属矿床地球化学特征及成矿-控矿因素研究

虎头崖铜铅锌多金属矿床的成矿作用十分复杂,成矿-控矿因素仍不明,已成为制约找矿突破的瓶颈.鉴于此,笔者对该矿床的地质、地球化学特征和侵入岩年龄及地球化学开展了研究.结果表明,Ⅵ矿带二长花岗岩LA-MC-I CP-MS锆石U-Pb同位素年龄为(217.5±1.1) Ma(MSWD=1.4).Ⅵ矿带和Ⅱ矿带二长花岗岩钾、钠含量均较高,w(K2O)大于w(Na2O),分异程度较高,稀土元素球粒陨石标准化曲线向右缓倾斜,强烈富集LILE,中等富集HFSE,贫Ti、Ba,具有后碰撞阶段岩石的特点.成矿受侵入岩岩浆源区、演化方式,地层,构造,以及岩体与围岩接触方式的综合控制.源区具有地幔物质贡献的Ⅵ矿带二长花岗岩,成矿作用较强,主要形成近接触带矽卡岩型和远接触带矽卡岩型Cu-Pb-Zn多金属矿.而壳源特征为主的Ⅱ矿带二长花岗岩成矿能力较弱,主要形成矽卡岩型Sn、Mo、Fe等矿产.     

广元三堆镇康家沟剖面寒武系地层及沉积特征

丹凤群分布于天水市南部,向东延入陕西凤县。通过原岩恢复,其下部层位的岩石以变玄武岩为主,夹安山岩、石英岩、大理岩,中部为变石英砂岩夹玄武岩、薄—微层状石英岩夹安山岩、英安岩,上部为玄武岩、玄武安山岩、安山岩、石英砂岩、大理岩夹流纹岩及硅质条带。火山岩为碱性—拉斑系列,锶同位素初始比值低,地球化学特征与岛弧玄武岩的地球化学模型相似。通过对丹凤群火山岩地质特征、岩石组合、岩石地球化学特征的综合分析,认为丹凤群的沉积环境,处于当时的秦岭古陆南侧的古大洋岛弧。     

Characteristics of particle size for creeping and saltating sand grains in aeolian transport

Creep and saltation are the primary modes of surface transport involved in the fluid‐like movement of aeolian sands. Although numerous studies have focused on saltation, few studies have focused on creep, primarily because of the experimental difficulty and the limited amount of theoretical information available on this process. Grain size and its distribution characteristics are key controls on the modes of sand movement and their transport masses. Based on a series of wind tunnel experiments, this paper presents new data regarding the saltation flux, obtained using a flat sampler, and on the creeping mass, obtained using a specifically designed bed trap, associated with four friction velocities (0·41, 0·47, 0·55 and 0·61 m sec^?1). These data yielded information regarding creeping and saltating sand grains and their particle size characteristics at various heights, which led to the following conclusions: (i) the creeping masses increased as a power function (q = ?1·02 + 14·19u_*³) of friction wind velocities, with a correlation (R²) of 0·95; (ii) the flux of aeolian sand flow decreases exponentially with increasing height (q = a exp(–z/b)) and increases as a power function (q = ?26·30 + 428·40 u_*³) of the friction wind velocity; (iii) the particle size of creeping sand grains is ca 1·15 times of the mean diameter of salting sand grains at a height of 0 to 2 cm, which is 1·14 times of the mean diameter of sand grains in a bed; and (iv) the mean diameter of saltating sand grains decreases rapidly with increasing height whereas, while at a given height, the mean diameter of saltating sand grains is positively correlated with the friction wind velocity. Although these results require additional experimental validation, they provide new information for modelling of aeolian sand transport processes.