哀牢山成矿带长安金矿床成因：地质特征、流体包裹体测温和H-O-S-Pb同位素制约     

辛未  孟元库  许志河  孙丰月  钱烨 《吉林大学学报(地球科学版)》2022,52(5):1610-1625

中国西南部哀牢山成矿带南段长安金矿床成因机制仍然有待研究,为了解其成矿物质与流体来源,掌握其矿床成因类型,给矿山找矿增储工作提供依据,本文以长安金矿床作为研究对象,通过详细的地质特征描述、流体包裹体测温学和矿石H-O-S-Pb同位素测试来研究成矿物质和流体来源、演化,进而制约矿床成因,建立成矿模式。研究结果表明：前人认为的近南北向构造F₆并非断裂构造,而是隐爆角砾岩筒,其为长安金矿床的主容矿构造;主成矿阶段包裹体冰点温度绝大部分为-2.9~-0.7 ℃ ,对应盐度（w(NaCl)）为1.22%～4.79%,均一温度为162～226 ℃,属于低温低盐度流体体系。长安金矿床成矿主阶段石英的δ¹⁸O_H2O介于4.4‰～5.2‰之间,δD为-93.9‰～-85.9‰,落入岩浆水与大气水演化线之间,说明成矿流体为岩浆流体与大气水的混合物。长安金矿床黄铁矿的δ34S平均值为2.1‰（n=32）,绝大多数介于0.0~3.6‰之间,具有明显的岩浆硫的特点,认为硫来源于岩浆岩;黄铁矿的铅同位素组成特点明显具有二元性,反映了岩浆铅和上地壳围岩铅的双重贡献。综上,认为成矿物质和流体主要来源于岩浆,后期大气水和围岩也对成矿流体物质有一定贡献;长安金矿床受隐爆角砾岩控制,与低硫化型浅成低温热液型金矿的特征相似,尽管其围岩并非传统的火山岩。  相似文献   

A Review of Mineral Resources and GIS Applications in Mineral Resource Assessment in Northeast China     

Zhou Yunxuan  Wang Lei  Liu Wansong  Xu Huiping  Sun Fengyue 《世界地质(英文版)》2000,3(2)

Northeast China is one of the regions in China that possesses a great abundance of mineral resources.Coal, petroleum, natural gas, gold, iron, magnesite, graphite, talc, molding sand, glass sand and some others account for large portion in reserves and yields of that in the whole country. The region faced also shortages of copper, molybdenum, oil shale, zirconium, tantalum, rare earth, and beryllium, although they have large reserves,but limited by economical and technical factors. Geological mapping and mineral exploration activities have been intensive. Only the north part of Daxinanling Mountains in the region leaves unexplored. GIS applications in mineral resource assessment in the region start not long. Databases for GIS applications are on the way of construction.Well - trained technical staff and expertise do not meet the demand.This article reviews the situation of mineral resources and GIS applications for mineral resource assessment in the region. Suggestions on multi - lateral cooperation and GIS training are also made.  相似文献   

鄱阳湖湿地中低滩典型植物群落的生物多样性及影响因子     

郭宇菲  万荣荣  龚磊强  秦风约  王经波  王晓龙 《湖泊科学》2023,35(4):1370-1379

周期性水文节律是影响洪泛湖泊洲滩湿地植物群落物种组成与生物多样性的重要驱动力。本研究以鄱阳湖中低滩典型植物群落为研究对象,通过实地样方调查与统计方法分析植物群落的生物多样性格局及其关键环境因子。结果表明：鄱阳湖中低滩代表性群落分别是灰化薹草群落和虉草群落;植物群落的Shannon-Wiener多样性指数均值为1.5,Pielou均匀度指数均值为0.55,生物多样性与物种均匀度偏低。虉草群落的均匀度、多样性指数高于灰化薹草群落,但二者物种丰富度差异不明显。土壤铵态氮、总磷及土壤含水量和高程是影响植物群落结构与生物多样性的关键因子,其中灰化薹草的物种多样性与土壤铵态氮高度相关,而虉草的均匀度则与土壤总磷关系更密切。此外,鄱阳湖中低滩环境下,灰化薹草群落的均匀度随土壤总磷含量的升高呈现U型响应曲线,虉草则是倒U型,这表明,鄱阳湖中低滩环境下,灰化薹草群落和虉草群落生物多样性对单个、同一的环境因子存在不同的适应机制。  相似文献   

蚌科20种蚌类肛门的比较解剖及其系统学意义     

舒凤月  吴小平 《海洋湖沼通报》2005,(2):29-33

对蚌科11属20种蚌类肛门进行了比较解剖研究。结果表明．蚌科肛门的结构特征具有重要的分类学价值．肛门类型、肛门相对后闭壳肌位置、肛门壁内表面是否具纵嵴、肠沟终止位置等特征因种类不同而有明显差异，可作为分类依据之一。  相似文献   

东昆仑夏日哈木矿区闪长岩锆石U-Pb年代学、地球化学及其地质意义   总被引：1，自引：0，他引：1  

王冠  孙丰月  李碧乐  李世金  赵俊伟  杨启安 《吉林大学学报(地球科学版)》2014,44(3):876

夏日哈木矿区的闪长质岩体呈岩株状出露于矿区南东,岩性主要为石英闪长岩和闪长岩。年代学研究表明,石英闪长岩中岩浆锆石LA-ICP-MS U[CD*2]Pb谐和年龄为(243±1 ) Ma,MSWD＝0.013,属早三叠世晚期。岩石学及化学成分显示其属于准铝质、高钾钙碱性系列闪长岩。稀土配分曲线呈现轻稀土元素相对富集的右倾分布特征((La/Yb)_N=8.7~12.7),无明显的Eu负异常(δEu=0.84~1.01)。岩石富集Rb、Ba、K等元素,而相对亏损Nb、Ta、P和Ti。岩石具有不均一的ε_Hf(T)值(-9.0~-1.0)和古老的二阶段Hf模式年龄(1.34~1.84  Ga)。结合试验岩石学资料判别,闪长岩主要起源于中元古代玄武质下地壳脱水部分熔融,富集地幔组分的加入可能是导致ε_Hf(T)值和Hf模式年龄不均一的主要原因。微量元素及特征比值显示岩体形成于安第斯型活动大陆边缘的构造环境。综合分析认为,早三叠世晚期东昆中隆起带整体处于俯冲晚期的安第斯型活动大陆边缘背景。  相似文献   

Geochronology and geochemistry of Hutouya monzonitic granite of Qimantage,Qinghai     

WANG Yang  SUN Fengyue  GAO Hongchang  HE Shuyue  QIAN Ye  XU Chenghan 《世界地质(英文版)》2017,20(4)

The geochemical features of the monzonitic granite in Qimantage Hutouya deposit area,Qinghai,in respect to the mineralization,suggest that this granite belongs to weak peraluminous and high-k calc alkaline rock series. The REE of the samples show right slope with obvious LREE/HREE differentiation and negative Eu abnormity. The trace elements show enrichment of LILE( Rb,Th,U,La,Nd),and deleption of Ba,Sr,Nd,P,Ti. The Sr-Nb isotopic data indicate that the magma source is mainly aluminosilicate lower crust with a small amount of new crustal materials. The weighted mean zircon U-Pbage of the Hutouya monzonitic granite is 221±1.7 Ma,belonging to Late Triassic. The Hutouya monzonitic granite was formed in the tectonic setting of transition from compression to extension during Middle-Late Triassic.  相似文献   

Geochemistry and Genesis of the Late Jurassic Granitoids at Northern Great Hinggan Range: Implications for Exploration   总被引：2，自引：1，他引：1  

WU Guang  CHEN Yanjing  SUN Fengyue  ZHANG Zhe  LIU Ankun  LI Zhitong 《《地质学报》英文版》2010,84(2):321-332

<正>The Longgouhe and Ershiyizhan intrusions of the Late Jurassic,located in the Upper Heilongjiang Basin of the northern Great Hinggan Range,are closely related to porphyry Cu-Au mineralizations.In lithology the intrusions are quartz diorite,quartz monzodiorite and granodiorite of high-K calc-alkaline series,with minor aspects of shoshonite series.Their SiO_2 and Al_2O_3 contents range from 61.37%to 66.59%and 15.35%to 17.06%,respectively.The MgO content ranges from 2.02%to 3.47%,with Mg~# indices of 44-59.The(La/Yb)_N and Eu/Eu~* values range from 16.85 to 81.73 and 0.68 to 0.93,respectively,showing strong differentiation rare earth element(REE) patterns similar to those of adakites.The rocks are enriched in Ba,Sr and light REE(LREE),obviously depleted in Nb and Ta,slightly depleted in Rb and Ti,and poor in Yb and Y,with Yb and Y contents of 0.31-1.32 ppm and 4.32-12.07 ppm,respectively.As indicated by Sr/Y ratios of 67.74-220.60,the rocks are characterized by low-Y and high-Sr contents,which characterize the adakites in the world.Holistically, geochemical tracers suggest that the interested intrusions are adakitic rocks.Given that the Paleo-Asian Ocean and Mongol-Okhotsk Ocean were closed in the Late Paleozoic and Permian-Middle Jurassic,respectively,the interested intrusions should be formed by partial melting of delaminated crust,which had been thickened during collisional orogeny between the Siberian and Mongolian-Sinokorean continents.  相似文献