吐哈盆地大南湖地区层间氧化带特征及铀找矿前景     

黄国龙  朱捌  王建永 《地质学报》2005,79(5):679-689

利用前人钻孔资料并结合野外调查,研究了找矿目的层西山窑组沉积环境、岩相古地理特征、砂体厚度及空间展布;对比各岩层的后生氧化程度,确定了层间氧化带的分布范围和空间展布形态。通过对目的层砂岩岩石学和岩石化学特征的研究,初步查明了本区砂岩孔隙度、密度与其结构构造密切相关,以及氧化带中次生矿物变化和化学元素如Fe、CO2、C有、S、U、Th、Se、Mo、V等含量变化与地下水的氧化作用有关,符合水成铀矿床的变化规律。在此基础上,圈定出氧化砂体,其底板埋深小于300m、厚度达50-100m、氧化带前锋长达60km。并在氧化带前锋发现铀矿化、硒矿化多处,初步显示该区具有良好的找矿前景。  相似文献   

地幔流体参与胶东金矿成矿作用的氢氧碳硫同位素证据   总被引：41，自引：5，他引：36  

毛景文  李厚民  王义天  张长青  王瑞廷 《地质学报》2005,79(6):839-857

胶东地区金矿床可以分为三种类型,即石英脉型、破碎蚀变岩型和胶(州)—莱(阳)盆地北缘拆离带中的角砾岩型。挑选玲珑、焦家、三山岛、仓上、望儿山、大尹格庄、邓格庄、蓬家夼、发云夼和大庄子10个矿床中成矿主期的黄铁矿、绢云母和钾长石进行了硫、氢、氧同位素测试,还对个别矿床成矿晚期的碳酸盐矿物进行了碳、氧同位素测定,同时对比测定了玲珑花岗岩和郭家岭花岗闪长岩中黑云母和钾长石的氢、氧同位素,结果表明这些金矿虽然产出形式有差别,但都是同一深部流体库中流体上涌、与围岩发生强烈水岩反应和与地壳流体混合,通过交代和沉淀成矿。胶东金矿在形成时代上晚于侏罗纪玲珑花岗岩(160～150Ma)和白垩纪郭家岭花岗闪长岩(130～126Ma),与煌斑岩墙及其他中基性岩墙同时生成(121～114Ma),两者具有富CO2流体和伴随着以钾交代为特征的蚀变作用,都是中生代岩石圈快速减薄过程的地壳浅部响应。  相似文献   

西秦岭中、晚二叠世生物群更替事件   总被引：2，自引：0，他引：2  

曾学鲁  高金汉 《地质学报》2005,79(2):145-149

西秦岭地区中、晚二叠世的生物,在其发展过程中经历了一次动物群的更替事件,表现为中二叠世茅口晚期迭山组底部开始的竺蜓类化石的突然锐减或消失及腕足动物的大量繁盛。茅口中期的热让沟组上部,有Afghanella及丰富的Parafusulina,Chusenella等竺蜓类化石。但上覆的迭山组底部开始,仅有少量Parafusulina,Chusenella及Schwagerina等断续出现。而同时交替出现了以Urushtenia,N eoplicatifera为代表的小型腕足动物群及小型单体四射珊瑚。这一动物群的更替事件受到当时沉积环境变迁和区域构造活动的制约。迭山组底部的沉积环境由开阔台地的浅水环境转入半局限台地较深水滞流环境,导致了竺蜓类的消失和小型腕足动物的兴起。这种沉积相的变化与动物群的更替在层位上是完全吻合的。研究区处于西秦岭晚海西裂陷带两侧的碳酸盐台地或台地边缘,其生物群的更替和沉积相的变化必然受到区域上裂陷活动的影响。根据本区生物地层的研究,可以更为确切地认为,本区二叠纪裂陷活动的时间始于中二叠世茅口期Afghanella schencki时的后期(或N eoschwagerina时的后期) ;约终于晚二叠世长兴期Palaeofusulina时之前。  相似文献   

库车前陆盆地天然气成藏过程及聚集特征   总被引：10，自引：5，他引：5  

赵孟军  王招明  张水昌  王清华  宋岩  柳少波  秦胜飞 《地质学报》2005,79(3):414-422

天然气的组分和碳同位素主要受母质类型和成熟度双重因素的控制,这是我们研究天然气的基础。但是越来越多的证据显示成藏过程对天然气组分和碳同位素也具有明显的控制作用。尽管库车前陆盆地不同构造单元的天然气来源一致,即主要来源于侏罗系烃源岩、其次为三叠系烃源岩,但是库车前陆盆地冲断构造带、斜坡区和前缘隆起区在天然气组分、干湿程度和碳同位素组成上具有明显的差异。库车前陆盆地经历了早期油气的聚集、破坏和晚期天然气聚集、调整的过程,研究认为成藏过程对库车前陆盆地不同构造单元的天然气组分和碳同位素特征具有明显的控制作用。  相似文献   

The Changing Cold Regions Network:Observation,diagnosis and prediction of environmental change in the Saskatchewan and Mackenzie River Basins,Canada     

Chris M DEBEER  Howard S WHEATER  William L QUINTON  Sean K CAREY  Ronald E STEWART  Murray D MACKAY  Philip MARSH 《中国科学:地球科学(英文版)》2015,(1):46-60

Climate change is causing rapid and severe changes to many Earth systems and processes,with widespread cryospheric,ecological,and hydrological impacts globally,and especially in high northern latitudes.This is of major societal concern and there is an urgent need for improved understanding and predictive tools for environmental management.The Changing Cold Regions Network(CCRN)is a Canadian research consortium with a focus to integrate existing and new experimental data with modelling and remote sensing products to understand,diagnose,and predict changing land,water,and climate,and their interactions and feedbacks over the geographic domain of the Mackenzie and Saskatchewan River Basins in Canada.The network operates a set of 14 unique and focused Water,Ecosystem,Cryosphere and Climate(WECC)observatories within this region,which provide opportunities to observe and understand processes and their interaction,as well as develop and test numerical simulation models,and provide validation data for remote sensing products.This paper describes this network and its observational,experimental,and modelling programme.An overview of many of the recent Earth system changes observed across the study region is provided,and some local insights from WECC observatories that may partly explain regional patterns and trends are described.Several of the model products being developed are discussed,and linkages with the local to international user community are reviewed—In particular,the use of WECC data towards model and remote sensing product calibration and validation is highlighted.Some future activities and prospects for the network are also presented at the end of the paper.  相似文献   

空间应用短波CCD系统增益的放射源标定和估算     

曾智蓉  李保权  彭吉龙 《天文研究与技术》2010,7(1)

为满足国内空间天气监测预报研究,建立自主的空间天气数据获取系统,正在开发太阳软X-EUV空间成像望远镜。CCD作为空间望远镜的成像器件,在研制的过程中需要掌握其基本特性,对其进行标定测试。介绍了在热真空罐中使用Fe55放射源进行CCD增益标定的实验和实验数据的两种处理方式,得到了-8℃至0℃温度范围内的增益值,结果表明两种处理方式的结果符合较好,温度变化对增益的影响较小,并以这些温度下增益的平均值作为最终的增益值结果。  相似文献   

Tectonic Landform of Quaternary Lakes and Its Implications for Deformation in the Northern Qinghai-Tibet Plateau     

WANG An WANG Guocan LI Dewei XIE Defan LIU Demin Faculty of Earth Sciences  China University of Geosciences  Wuhan  Hubei  China State Key Laboratory of Geological Processes  Mineral Resources  China 《《地质学报》英文版》2009,83(1)

The Hohxil region in the northern Qinghai-Tibet Plateau is occupied by numerous plateau lakes,which have long been inferred as being tectonic products.However,so far little evidence has been found to support this tentative inference.Field survey and morphotectonic analysis of TM satellite images in the eastern segment of the Hohxil region revealed that Kusai Lake and Yelusu Lake are S- shaped pull-apart basins,which were dominated by left strike-slip master faults trending WNW-ESE. The pull-apart distanc...  相似文献   

Differential Tectonic Deformation of the Longmen Mountain Thrust Belt,Western Sichuan Basin,China   总被引：1，自引：1，他引：0  

TANG Liangjie YANG Keming JIN Wenzheng WAN Guimei L Zhizhou YU Yixin State Key Laboratory of Petroleum Resource  Prospecting  Beijing  China Key Laboratory for Hydrocarbon Accumulation Mechanism  China University of Petroleum  Ministry of Education  China Basin  Reservoir Research Center. China University of Petroleum  China Southwest Branch Company  SINOPEC  Chengdu  Sichuan    China 《《地质学报》英文版》2009,83(1)

Field investigation and seismic section explanation showed that the Longmen Mountain Thrust Belt has obvious differential deformation:zonation,segmentation and stratification.Zonation means that,from NW to NE,the Longmen Mountain Thrust Belt can be divided into the Songpan- Garz(?) Tectonic Belt,ductile deformation belt,base involved thrust belt,frontal fold-thrust belt,and foreland depression.Segmentation means that it can be divided into five segments from north to south: the northern segment,the Anxia...  相似文献   

Deep Background of Wenchuan Earthquake and the Upper Crust Structure beneath the Longmen Shan and Adjacent Areas     

LI Qiusheng  GAO Rui  WANG Haiyan  HE Rizheng Lithosphere Research Centre 《《地质学报》英文版》2009,83(4)

By analyzing the deep seismic sounding profiles across the Longmen Shan,this paper focuses on the study of the relationship between the upper crust structure of the Longmen Shan area and the Wenchuan earthquake.The Longmen Shan thrust belt marks not only the topographical change,but also the lateral velocity variation between the eastern Tibetan Plateau and the Sichuan Basin.A lowvelocity layer has consistently been found in the crust beneath the eastern edge of the Tibetan Plateau, and ends beneath the ...  相似文献   

Characteristics of Abnormal Pressure Systems and Their Responses of Fluid in Huatugou Oil Field,Qaidam Basin   总被引：1，自引：0，他引：1  

CHEN Xiaozhi  XU Hao  TANG Dazhen  ZHANG Junfeng  HU Xiaolan  TAO Shu  and CAI Yidong 《《地质学报》英文版》2009,83(5):939-950

Abstract: Based on the comprehensive study of core samples, well testing data, and reservoir fluid properties, the construction and the distribution of the abnormal pressure systems of the Huatugou oil field in Qaidam Basin are discussed. The correlation between the pressure systems and hydrocarbon accumulation is addressed by analyzing the corresponding fluid characteristics. The results show that the Huatugou oil field as a whole has low formation pressure and low fluid energy; therefore, the hydrocarbons are hard to migrate, which facilitates the forming of primary reservoirs. The study reservoirs, located at the Xiayoushashan Formation (N21) and the Shangganchaigou Formation (N1) are relatively shallow and have medium porosity and low permeability. They are abnormal low-pressure reservoirs with an average formation pressure coefficient of 0.61 and 0.72 respectively. According to the pressure coefficient and geothermal anomaly, the N1 and N21 Formations belong to two independent temperature-pressure systems, and the former has slightly higher energy. The low-pressure compartments consist of a distal bar as the main body, prodelta mud as the top boundary, and shore and shallow lake mud or algal mound as the bottom boundary. They are vertically overlapped and horizontally paralleled. The formation water is abundant in the Cl– ion and can be categorized as CaCl2 type with high salinity, which indicates that the abnormal low-pressure compartments are in good sealing condition and beneficial for oil and gas accumulation and preservation.  相似文献