Ore-forming Fluid Characteristics of the Saishitang Cu-polymetallic Deposit in Qinghai Province, China     

LAI Jianqing  JU Peijiao  MAO Yin  AN Jianghu  WANG Xiongjun 《《地质学报》英文版》2015,89(2):485-504

Saishitang Cu-polymetallic deposit is located in the southeast section of Late Paleozoic arcfold in the southeastern margin of Qaidam platform. Accoring to the geological process of the deposit,four mineralization episodes were identified: melt/fluid coexisting period(O),skarn period(A),first sulfide period(B) and second sulfide period(C),and 10 stages were finally subdivided. Three types of inclusions were classified in seven stages,namely crystal bearing inclusions(type I),aqueous inclusions(type II) and pure liquid inclusions(type III). Type I and II inclusions were observed in stage O1,having homogenization temperature from 252 to 431°C,and salinities ranging from 24.3% to 48.0%. Type I inclusion was present in stage A1,having homogenization temperature from 506 to 548°C,and salinities ranging from 39.4% to 44.6%. In stage B1,type II and III inclusions were observed,with homogenization temperature concentrating between 300–400°C,and salinities from 0.4% to 4.3%. Type II inclusions were present in stage B2,with homogenization temperature varying from 403 to 550°C. In stage C1,type I and II inclusion commonly coexisted,and constituted a boiling inclusion group,having homogenization temperatures at 187–463°C,and salinities in a range of 29.4%–46.8% and 2.2%–11.0%. Type II and III inclusions were developed in stage C2,having homogenization temperature at 124–350°C,and salinities ranging between 1.6% and 15.4%. In stage C3,type II and III inclusions were presented,with a homogenization temperature range of 164–360°C,and salinities varying from 4.0% to 11.0%. The results of micro-thermal analysis show that fluids are characterized by high temperature and high salinity in stage O1 and A1,and experienced slight decrease in temperature and dramatic decrease in salinity in stage B1 and B2. In stage C1,the salinity of fluid increased greatly and a further decrease of temperature and salinity occurred in stage C2 and C3. Fluids boiled in stage C1. With calculated pressure of 22 MPa from the trapping temperature of 284–289°C,a mineralization depth of 2.2 km was inferred. Results of Laser Raman Spectroscopy show high density of H2 O,CH4 and CO2 were found as gas composition. H-O isotope study indicates the oreforming fluids were the mixture of magmatic water and meteoric water. Physicochemical parameters of fluids show oxygen and sulfur fugacity experienced a decrease,and redox state is weakly reducing. Along with fluid evolution,oxidation has increased slightly. Comprehensive analysis shows that melt exsolution occurred during the formation of quartz diorite and that metal elements existed and migrated in the form of chlorine complex. Immiscible fluid separation and boiling widely occurred after addition of new fluids,bringing about dissociation of chlorine-complex,resulting in a great deal of copper precipitation. In conclusion,Saishitang deposit,controlled by regional tectonics,is formed by metasomatism between highly fractionated mineralization rock body and wall rock,and belongs to banded skarn Cu-polymetallic deposit.  相似文献   

一种面向异常检测的高光谱图像降维算法     

马丽  鞠才  朱菲 《测绘科学》2015,40(7):29-33

针对高光谱数据预处理中传统降维算法的不足,文章提出采用线性局部切空间排列(LLTSA)算法进行降维,并在低维空间中,以数据点到背景流形的最小距离为度量进行异常目标检测。面向异常目标检测问题的降维算法,需要考虑计算量和异常污染两个问题:为减少计算量,选择图像中一部分具有代表性的训练数据进行LLTSA降维并求取用于泛化的投影矩阵;为避免异常信息对背景特性的影响,应该选择不含异常的背景训练数据建立背景流形。背景训练点的选择基于递归多层分割算法,结合分割块的大小和分割块被近邻点重构的误差,去除分割结果中可能包含异常的区域并尽可能多地保留背景信息。实验结果表明LLTSA可以利用少数特征有效区分背景和异常,基于LLTSA的检测算法比经典RX和核RX算法具有更好的异常检测性能。  相似文献   

浙江省国内旅游流系统网络结构演变研究     

琚胜利  陶卓民  赖正清  陈浩  徐喆 《地理与地理信息科学》2015,31(2):91-97,114

运用社会网络理论的块模型、网络密度、网络中心性,结合锡尔指数、ArcGIS空间分析方法,基于省外客流的面板数据,研究近十年来浙江省大尺度国内旅游流系统网络结构演变特征。结果发现:1)旅游流网络系统整体变化缓慢,局部变化明显。客源网络系统与目的地网络系统联系在加强,客流有向主要客源地和主要目的地集中态势。目的地地带间网络中心性整体锡尔系数呈现先降后升,总体处于波动增加趋势。2)客源地、目的地中心性与块的密度值呈正比例关系。旅游流网络空间系统演变过程,体现了总体稳定性和自相似性的空间等级特征。3)浙江省省外旅游流目的地系统网络结构,形成了"一个核心—边缘旅游带,四级城市,五级旅游区"的空间等级结构。客源地网络空间格局具有明显的"核心—边缘,圈层等级扩散"特征。  相似文献   

在海洋环境中的酵母菌分布与多样性   总被引：1，自引：0，他引：1  

池振明  居靓  王祥红  池哲  刘光磊 《中国海洋大学学报(自然科学版)》2009,39(5)

最近几年作者对不同海洋环境中的酵母资源、分布和多样性进行的大量研究,从中发现了22属63种1051株。并且发现这些广泛分布在海水、海泥、高盐海水、深海、各种大型海藻表面、各种海鱼体表和体内和红树林生态系统中。不同种的酵母可以产生蛋白酶、脂酶、植酸酶、菊糖酶、纤维素酶、β-1,3-葡聚酶、嗜杀因子、核黄素、铁载体等活性产物,所以这些酵母菌具有广泛的实际用途。  相似文献   

THE RELATIONSHIP OF THE PRECEDING WINTER MJO ACTIVITIES AND THE SUMMER PRECIPITATION IN YANGTZE-HUAIHE RIVER BASIN OF CHINA   总被引：2，自引：0，他引：2  

李汀  琚建华  甘薇薇 《热带气象学报(英文版)》2012,18(1):32-44

The first two series(RMM1 and RMM2) of RMM Index(all-Season Real-time Multivariate MJO Index) are computed to obtain the interannual variation of the preceding winter(preceding December to current February) MJO strength,according to which active(or inactive) years of preceding winter MJO are divided.By utilizing the data provided by NCEP/NCAR,CMAP and China’s 160 stations from 1979 to 2008,we studied the preceding winter MJO strength and discovered that the summer precipitation in the basin are of significantly negative correlation,i.e.when the preceding winter MJO is relatively active,the summer precipitation in the basin decreases,and vise verse.We also analyzed the causes.When the preceding winter MJO is relatively active,its release of potential heat facilities Inter-Tropical Convergence Zone(ITCZ) to strengthen and locate northward in winter and propagate northeastward.This abnormal situation lasts from winter to summer.In mid-May,ITCZ jumps northward to the South China Sea,the western Pacific subtropical high withdraws eastward,and the South China Sea summer monsoon sets off and strengthens.In summer,ITCZ propagates to South China Sea-subtropical western Pacific,the zonal circulation of subtropical Pacific strengthens,and a local meridional circulation of the South China Sea to the basin area forms,giving rise to the East Asia Pacific teleconnection wave-train.An East Asian monsoon trough and the Meiyu front show opposite features from south to north,the East Asian summer monsoon strengthens and advances northward.As a result,the summer monsoon is weakened as the basin is controlled by the subtropical high continually,with less rain in summer.On the contrary,when the preceding winter MJO is inactive,ITCZ weakens and is located southward,the subtropical high is located southward in summer,and the basin is in a region of ascending airflow with prevailing southwest wind.The East Asian monsoon trough and EASM weaken so that summer monsoon is reduced in the basin where precipitation increases.  相似文献   

导线覆冰极值的概率分布模拟及其应用试验   总被引：2，自引：0，他引：2  

江志红  刘冬  刘渝  熊海星  鞠晓慧 《南京气象学院学报》2010,33(4):385-394

利用南方地区多个气象站和电力部门观冰站的导线覆冰逐日冰厚资料,将广义极值分布和广义帕雷托分布引入导线覆冰的概率模型研究中,通过超门限覆冰次数的泊松分布拟合检验,结合H ill图解,提出了基于超门限峰值法门限值的确定方法;对两种分布在导线覆冰极值模型拟合的适用性研究表明,广义帕雷托分布对各站覆冰冰厚极值的拟合精度最高;重现期冰厚极值估计随样本长度的变化分析表明,广义帕雷托分布模型极值估计的稳定性比广义极值分布强,一般样本容量达到25 a左右时,广义帕雷托分布重现期冰厚极值的估计趋于稳定,可以作为短序列下估计导线覆冰极值的较好方法。  相似文献   

一次梅雨锋暴雨云物理特征的数值模拟研究   总被引：4，自引：1，他引：3  

鞠永茂  王汉杰  钟中  宋帅 《气象学报》2008,66(3):381-395

利用中尺度数值模式MM5(V3.6),选用模式中不同的显式云物理方案,对2003年7月4-5日发生在江淮流域的梅雨锋暴雨过程进行了数值模拟,并根据模拟结果对造成此次暴雨过程的对流云团的微物理特征进行了分析.研究结果表明:(1) 具有详细云物理过程的中尺度模式MM5对短时强降水过程具有较好的模拟能力,提高MM5模式的分辨率,可以更好地模拟短时梅雨锋暴雨过程,模式中的Goddard云物理方案的模拟结果要优于Reisner方案和Schultz方案.(2) 梅雨锋对流云团是一种复杂的固、液、气三相混合体结构,在云体区域内的平均质量密度分布中,水汽的质量密度最大,其次是霰,而冰晶、雪、云水和雨水的质量密度较小且数值大小彼此接近,各种相态粒子质量密度峰值出现的高度随时间无明显变化.雨水、云冰和霰的质量密度随时间演变规律与地面降水强度的变化特征相一致,近地面层水汽密度随时间的演变规律比地面降水强度提前1-2个小时,水汽通量的辐合对暴雨时段内水汽的补充和维持起到了重要的作用.(3) 除了最基本的云水向雨水转化的云微物理过程之外,此次降水过程还显示,在中层500-700 hPa范围内雪、冰晶等冰相粒子首先转化为霰粒子,而霰和云水的结合进一步加速(剧)云水向雨水的转换,成为短时特大暴雨形成不可或缺的动力机制,云物理过程中的相变潜热与对流运动的正反馈机制是促进暴雨维持和发展的最重要热力因子.  相似文献   

上海地区最高气温资料的恢复试验   总被引：3，自引：0，他引：3  

李庆祥  黄嘉佑  鞠晓慧 《热带气象学报》2008,24(4):349-353

对上海最高气温1924～2001年期间的缺测资料进行了恢复试验,以期通过该个例的研究,探讨我国台站历史资料集中缺测或中断序列的恢复、插补的一般方法.选取使用上海气象观测站的相邻若干台站的最高气温资料,分别用回归分析法、判别分析法和偏最小二乘法,对上海站相应期间缺测资料进行逐年逐月的恢复,并利用交叉检验的均方误差作为恢复效果的评判.结果发现对缺测资料恢复的总效果以偏最小二乘法为最好,因此选用该方法作为资料恢复的主要方法.恢复过程为每次仅恢复某月份、某测站、某年份的缺测资料,恢复后的估计值作为观测值使用,再进行其它缺测资料恢复的新资料集,如此反复地进行,以近期资料开始,逐步向前期资料延拓.这样做的目的是为了使得和后续的观测资料直接连接.  相似文献   

S波段多普勒天气雷达旁瓣回波的特征分析   总被引：4，自引：2，他引：2  

廖玉芳  俞小鼎  吴林林  李耨周  居晶琳 《热带气象学报》2008,24(2):183-188

通过对2002～2005年S波段多普勒天气雷达上旁瓣回波的分析,描述了其在基本反射率因子、径向速度、速度谱宽PPI图及反射率因子和径向速度垂直剖面图上的形态特征.在7次强对流事件的19个雹暴云中发现有6次强对流事件10个雹暴云共产生旁瓣回波110次(基于反射率因子仰角产品的统计).统计结果表明:形成旁瓣回波最小反射率因子强度为60 dBz,97.3%的旁瓣回波出现在反射率因子强度≥63 dBz时,旁瓣回波出现在50～100 km距离段内的机率最大;旁瓣回波出现的最大高度为11 km,最低高度是1 km,97.3%的旁瓣回波出现在1～9 km高度之间,69.1%的旁瓣回波出现在3～6 km高度之间,以4～5 km高度出现次数最多,然后向上、向下减少.据灾情调查报告分析,强降雹发生在旁瓣回波首次出现后的0～42 min内,表明旁瓣回波对强降雹具有一定的临近预警作用.  相似文献   

气候变化对重庆农业的影响及对策研究     

GAO Yanghua  JU Hui  JAN Verhagen  ZHANG Jianping 《四川气象》2008,(4)

本文分析了重庆市气候特点及其对重庆农业的影响;并在全球气候变暖的大气候背景下,分析了重庆气候的变化趋势,并就气候变化对重庆农业可能造成的影响进行了初步的探讨;提出了重庆农业应对气候变化的适应性战略和技术措施。  相似文献