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1.
辽西南部中生代花岗岩为活动大陆边缘陆内型钙碱性—富钾钙碱性系列岩石。花岗质岩浆具有深源性,可能为下地壳—上地幔部分熔融产生的安山质岩浆与硅铝层地壳的重熔岩浆混合而形成的“混熔岩浆”。各期花岗岩体的形成温度为750—1010℃,氧逸度10~(-6)—10~(-8)Pa,水逸度660×10~5—1513×10~5Pa,水分压1120×10~5—2200×10~5Pa。岩体定位深度为3.7—7.3km。  相似文献   

2.
南口前一带金矿床的稳定同位素研究表明,金矿成矿与太古宙花岗岩—绿岩带,南口前花岗岩体关系密切。依据金矿床硫、碳同位素组成判定金矿床属热液成因,热液体系处于 H_(?)S 占优势的化学环境。在成矿过程中成矿介质由弱酸性向酸性,再向碱性方向演化;氧逸度随着成矿介质温度降低,金属硫化物的沉淀而逐渐升高。氢、氧同位素组成显示了岩浆热液有天水混入。铅同位素组成表明金矿中的铅属古老正常铅,与花岗岩中长石铅为同源。据此,作者认为南口前一带金矿属再平衡岩浆热液矿床。  相似文献   

3.
辽西火山岩型金矿分布在中生代陆相火山盆地边缘活动带内,受辽西弧形构造带控制,为火山期后热液矿床,可初步划分为3种成因类型:次火山(斑岩)热液型(二道沟式),火山—次火山热液型(红石砬子式)和爆发角砾岩型(水泉式),成矿作用与中酸性火山—次火山岩关系密切,成矿时代为燕山期(90—110Ma)。稳定同位素研究结果表明,含矿热液为富含挥发组份和多金属成矿元素的富金水溶液,来源于地壳深部或上地幔,即高温热卤水对镁铁质、超镁铁质岩石长期侵蚀、淋滤和溶解,获取大量的金属成矿元素,在不透水层之下形成深部液态矿源层。  相似文献   

4.
蔡家坪铅锌矿位于著名的北武夷铜铅锌银多金属成矿带内,矿体主要赋存于侏罗系下统水北组层间破碎带内—大致顺层侵入的流纹斑岩与围岩接触带和流纹斑岩墙或斑岩脉内、外接触带中。矿体呈透镜体状、带状。不同成因矿体的产状差异较大,产状在20~75°之间。矿体主要金属矿物组合为方铅矿、闪锌矿、黄铁矿等。矿石构造以块状构造为主,次为细脉状、网脉状构造等。矿床属中低温火山沉积—层间破碎带—岩浆热液叠生型及次火山斑岩型矿床,属次火山热液矿床。  相似文献   

5.
皇城山银矿床产于白垩系下统陈棚组以流纹质为主的钙碱性火山岩系中。矿化发生于皇城山段流纹质火山喷发活动行将结束的阶段。矿床受火山地层岩石、火山机构、次火山岩控制。成矿物质主要来自火山岩浆热液和火山岩。矿液主要由岩浆水和原生雨水组成。矿床的形成经历了火山喷发沉积期、次火山热液充填期和局部风化淋滤期。矿床成因类型属陆相火山作用形成的中(低)温热液充填成因的单一型银矿床。为目前国内较罕见的银矿床,可称之谓“皇城山式银矿床”。  相似文献   

6.
辽阳隆昌—本溪草河口一带的硫铁矿及其它硫化物矿床(点),赋存于早元古宙北辽河群里尔峪组钠质火山岩段向碳酸盐岩过渡的层状岩系中,严格受里尔峪组控制。里尔峪组厚度为400—600m,由3个岩段组成,原岩为火山—沉积岩,火山岩属钙碱性火山喷发系列。矿床既受层位控制,亦受岩性控制。成矿物质通常来源于辽东早元古宙裂陷槽(构造活动带)内的钠质火山喷发,具工业价值的矿床受一定的岩相古地理条件及后期褶皱构造所控制。  相似文献   

7.
本文根据“七五”项目:《广西贵港市龙头山金矿床地质特征及找矿方向》的研究成果基础上撰写而成。文中侧重地论述了火山机构与矿床特征,并探讨了矿床成困。研究认为:矿床构造是一个晚中生代的残存火山颈机构。在其管道内的隐爆角砾岩、火山角砾岩、角砾熔岩、流纹斑岩和花岗斑岩等岩相带以及中酸性脉岩相,均属贫硅、富钾钙碱性系列的铝过饱和类岩石,是一套陆相中心式火山—次火山喷发—侵入岩系,属同源不同阶段的产物;该矿床金矿体受火山颈机构内的角砾状岩石及其内外接触带的断裂构造控制,多呈直立脉状,具有火山岩型与断裂充填型两类金矿化;成矿物质与流体主要源于火山岩浆喷气、热液,应属火山—次火山岩热液型金矿床。  相似文献   

8.
古利库金(银)矿床位于中生代大杨树火山断陷盆地北东缘与新元古代-早寒武世落马湖隆起的接壤部位。矿体主要赋存于下白垩统龙江组火山岩及其与新元古界-下寒武统落马湖群变质岩接触带附近,严格受古火山机构及其外围的环形断裂控制。热液成矿阶段分为早期石英阶段、玉髓-黄铁矿阶段、石英-黄铁矿阶段、石英-多金属硫化物阶段、石英-碳酸盐阶段。对古利库矿床进行的系统岩相学和流体包裹体研究表明,流体包裹体类型为富液相包裹体、富气相包裹体和纯气相包裹体,以富液相包裹体为主。成矿温度为136~367℃,从成矿早期至晚期分别为270~367,255~304,179~318,136~279℃。盐度w(NaCleqv)为1.4%~8.0%,成矿深度为1.0 km,成矿流体以大气降水为主,显示低硫型浅成低温热液金矿成矿特征。含矿石英脉中广泛发育冰长石和叶片状方解石-石英,结合流体包裹体特征表明,流体的沸腾作用是引起成矿流体中矿质发生沉淀富集的主要成矿机制。   相似文献   

9.
桃园—测鱼铜成矿远景区是河北省重要的成矿远景区之一。在前人工作基础上,初步总结了该地区铜多金属矿六种成矿模式:与火山、次火山浅成岩浆侵入活动有关的铜锌矿床、与海底火山活动有关的块状硫化物矿床、热液充填脉状铜矿、变质辉绿岩型铜矿、角砾集块岩型铜矿和中低温热液充填脉状铅锌矿,提出了五种找矿模型:变质辉绿岩型,热液充填脉状,与海底火山活动有关的块状硫化物矿床,与火山、次火山浅成岩浆侵入活动有关的铜锌矿和角砾集块岩型铜矿类型。  相似文献   

10.
华北地台南缘活动带,中上元古代为华北地台南缘的裂陷海槽,沉积了一套官道口群、栾川群和陶湾群冒地槽型类复理式建造。这套地层以含火山岩夹层的富镁、高硅、多碳沉积为特征,对多金属成矿极为有利,形成了丰富的多种类型的铅锌矿床,占全省铅锌矿床(点)总数的50%以上。主要矿床类型有:①与中酸性斑岩小侵入体有关的热液交代型银家沟硫铁多金属矿床;②与断裂破碎带有关的热液充填型西灶沟铅锌矿床;③与碱性(次)火山岩有关的块状硫化物型曲里铁锌铜矿床;④陶湾群中的沉积改造型维摩寺铅锌矿床;⑤与闪长岩体有关的寒武系中沉积再造型尚洞铅锌多金属矿床。  相似文献   

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Based on the hydrographic data in austral summer during the 22nd Antarctic Expedition of China(2005/2006),some features can be found about the northern margin of Emery ice shelf as follows.The heat content in the surface layer(0-50 m) at the eastern end and the western end of the ice-shelf margin is much higher than that at the middle.The upper mixing-layer depth and the seasonal thermocline depth at the middle of the ice-shelf northern margin are much shallower than those at the both ends.However there is much less difference between the middle and the ends in the bottom layer.The remote sensing photos show that the inhomogeneity in the surface-layer water is closely related to the spatial distribution of the floes and polynia in the area.  相似文献   

13.
Phylogenetic analysis based on 16S rDNA of 8 strains of cultivable bacteria isolated from Arctic sea-ice was studied.The results showed that strain BJ1 belonged to genus Planococcus,which was a genus of low mole percent G C gram-positive bacteria;strain BJ6 belonged to genus Burkholderia of β-proteobacteria and the rest 6 strain all belonged to γ-proteobacteria,of which strain BJ8 was a species of Pseudoalteromonas,strain BJ2-BJ5 and BJ7 were members of genus Psychrobacter.Phylogenetic analysis also indicated that bacteria of genus Psychrobacter of the isolates formed a relatively independent phylogenetic cluster in comparison with other bacteria belonged to genus Psychrobacter.  相似文献   

14.
正1 Aims and Scope Advances in Polar Science(APS)is an international,peer-reviewed journal jointly sponsored by the Polar Research Institute of China and the Chinese Arctic and Antarctic Administration.APS is a comprchensive academic journal dedicated to presentation of multi-disciplinary achievements in Arctic and Antarctic expeditions and research.Its primary purpose is to publish achievements in fundamental research,applied  相似文献   

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《山地科学学报》2014,(4):I0004-I0009
<正>AIMS AND SCOPE(Editorial Policy)The Journal of Mountain Science(JMS)is devoted to mountains and their surrounding lowlands-ecoregions of particular global importance,with a particular emphasis on the important highlands/mountains in the world,such as the Tibetan Plateau,the Himalayas,the Alps,the Andes,the Rockies and many other mountain ranges of our planet.  相似文献   

17.
<正>The Journal of Mountain Science(JMS),founded in2004,is an international English-language journal on mountain sciences.JMS is supervised by the Chinese Academy of Sciences(CAS),sponsored by the Chengdu Institute of Mountain Hazards and Environment,CAS,published by Science Press China,and distributed by Springer exclusively throughout the world(excluding Mainland China).The JMS is published bimonthly,fulltexted in SpringerLink and CNKI,indexed/abstracted by  相似文献   

18.
Using the NCEP/NCAR reanalysis monthly 500 hPa height data on a 2.5 latitude-longitude grid and 1°×1° sea ice data,the polar vortex area,intensity index and arctic sea ice area index are calculated respectively,and the meridional distribution,period variation and the abrupts in the long range trend are analyzed to study their relationship.The results show that the meridional distribution of sea ice and polar vortex h-ave distinctive difference,the relative positions of them are different in the eastern and western hemispheres,and exept they have periods of 4 months,quasi half year,quasi year,4-5 years and 10 years commonly,and each of them has its own respective variation as well.The sea ice area is decreasing apparently since 1980's,so is the polar vortex area,but their abrupt changge time are different totally.The area of sea ice and polar vortex has prominent positive correlation,but the relationship of sea ice intensity,polar vortex intensity,polar vortex area is complicated.  相似文献   

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<正>The Journal of Ocean University of China(Oceanic and Coastal Sea Research)is a comprehensive academic quarterly sponsored by the Ocean University of China,published one volume per year.This journal is devoted to the publication of the theoretical and applied research  相似文献   

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