赣南大吉山五里亭岩体的锆石ELA-ICP-MS定年及其与钨成矿关系的新认识   总被引：39，自引：3，他引：36  

邱检生  McInnes BIA  徐夕生  Allen C M 《地质论评》2004,50(2):125-133

大吉山是南岭地区一个著名的大型钨多金属矿床,五里亭岩体是矿区出露规模最大的火成岩体,岩性为中粗粒似斑状黑云母二长花岗岩。锆石 ELA-ICP-MS 定年结果表明其形成年龄为 237.5±4.8 Ma,属印支期岩浆活动的产物。与南岭地区典型钨多金属矿床成矿岩体相比,五里亭岩体贫硅,富钙、镁、铁,Rb/Sr、Rb/Ba 和 U/Th 比值低,K/Rb 比值高,铕负异常不显著,分异指数低,尚未达到矿化岩体的分异演化程度,不具备矿化岩体的地球化学特征。元素—同位素综合示踪显示区内白云母碱长花岗岩为五里亭岩体经高度分异演化的产物,它与钨多金属矿成矿直接有关。矿区范围内出露的闪长岩起源于地幔,这一岩浆侵位所引起的高热场环境有利于花岗质岩石的形成与演化,对成矿具有重要的意义。  相似文献   

Geologic relationships and mineralization of peralkaline/alkaline granite-syenite of the Zargat Na’am ring complex, Southeastern Desert, Egypt     

Gehad M. Saleh 《中国地球化学学报》2006,(2)

Tungsten-bearing hydrothermal veins range from tensional veinlets to lodes containing multiple injections of hydrothermal quartz veins. Major composite lodes display greisen alteration envelopes characterized by enrichments in volatiles, K2O, Al2O3, Rb, L…  相似文献   

南海的右行陆缘裂解成因   总被引：33，自引：2，他引：31  

周蒂  俞何兴等 《地质学报》2002,76(2):180-190

南海成果是西太平洋边缘海动力学研究的重要部分,也关系到特提期,环太平洋两大超级会聚带的相互作用,是国内外地学界长期研究的热点问题。西太平洋边缘海内带,尤其是日本海和南海在形成时代,海盆形态和海底地貌,海底扩张的多轴,多阶段,由东向西扩展特征,岩石圈地幔的地球化学异常等方面具有共同特征,可能在成因上也相似,南海的海盆的楔形的楔形形状,海底扩张及陆架盆地的断陷的由北向南发展和自东向西推进的特征,地壳伸展减薄和海底扩张程度的由东向西减弱都可用尖端向西的“剪刀模型”来描述,即南海的张开是近南北向右行剪切力作用下东亚陆缘发生裂解的结果。南海张开的同时在海盆内及其西缘印支半岛上发育大量近南北向右行走滑断裂,表明当时存在区域性的近南北向右行剪切应力,而在其东缘现在看不到大型近南北向右行走滑断裂,可能是在中中新世以后受从赤道附近近滑移北上并沿马尼拉海沟仰冲的菲律宾群岛所破坏的结果。晚中生代以来,在西太平洋构造域,特提斯构造域西段（印度）及东段（澳大利亚）先后发生了朝欧亚大陆的,不同方向和速度的会聚。在这三大作用的复合和竞争的动力学背景下,东亚陆缘发生了有地幔参加传动的“超级剪切”,其应力场经历了左行压扭体制和右行张扭体制交替的阶段性变化,正是在特提斯构造域西段的会聚起主导作用的阶段,东亚陆缘在右行张扭应力场作用下发生裂解,形成了南海和其他内带边缘海。  相似文献   

REGRESSION ON MULTIVARIATE IMAGES:PRINCIPAL COMPONENT REGRESSION FOR MODELING,PREDICTION AND VISUAL DIAGNOSTIC TOOLS     

PAUL GELADI Research Group for Chemometries  University of Ume  S- Ume  Sweden  Center for Peat Research Box  S- Ume  SwedenKIM ESBENSEN Norwegian Computing Center  PB  Blindern  N- Oslo  Norway 《地理学报(英文版)》1991,(2)

Regression between two blocks(usually called‘dependent’or Y and‘independent’or X)of data is a veryimportant scientific and data-analytical tool.Regression on multivariate images is possible and constitutesa meaningful addition to existing univariate and multivariate techniques of image analysis.The regressioncan be used as a modeling tool or for prediction.The form of the regression equation chosen is dependentupon problem specification and information at hand.This paper describes the use of principal componentregression(PCR).Both model building and prediction are presented for continuous Y-variables.The finalgoal is to supply new image material that can be used for visual inspection on a screen.Also,visual toolsfor diagnosis of model and prediction are provided,often based on derived image material.Examplesof modeling and prediction are given for six channels in a seven-channel satellite image  相似文献   

Characteristics of Arctic synoptic activity, 1952–1989     

M. C. Serreze  J. E. Box  R. G. Barry  J. E. Walsh 《Meteorology and Atmospheric Physics》1993,51(3-4):147-164

Summary Synoptic activity for the Arctic is examined for the period 1952–1989 using the National Meteorological Center sea level pressure data set. Winter cyclone activity is most common near Iceland, between Svalbard and Scandinavia, the Norwegian and Kara seas, Baffin Bay and the eastern Canadian Arctic Archipelago; the strongest systems are found in the Iceland and Norwegian seas. Mean cyclone tracks, prepared for 1975–1989, confirm that winter cyclones most frequently enter the Arctic from the Norwegian and Barents seas. Winter anticyclones are most frequent and strongest over Siberia and Alaska/Yukon, with additional frequency maxima of weaker systems found over the central Arctic Ocean and Greenland.During summer, cyclonic activity remains common in the same regions as observed for winter, but increases over Siberia, the Canadian Arctic Archipelago and the Central Aretic, related to cyclogenesis over northern parts of Eurasia and North America. Eurasian cyclones tend to enter the Aretic Ocean from the Laptev Sea eastward to the Chukchi Sea, augmenting the influx of systems from the Norwegian and Barents seas. The Siberian and Alaska/Yukon anticyclone centers disappear, with anticyclone maxima forming over the Kara, Laptev, East Siberian and Beaufort seas, and southeastward across Canada. Summer cyclones and anticyclones exhibit little regional variability in mean central pressure, and are typically 5–10 mb weaker than their winter counterparts.North of 65°N, cyclone and anticyclone activity peaks curing summer, and is at a minimum during winter. Trends in cyclone and anticyclone activity north of 65°N are examined through least squares regression. Since 1952, significant positive trends are found for cyclone numbers during winter, spring and summer, and for anticyclone numbers during spring, summer and autumn.With 11 Figures  相似文献   

Mineralization at the Wallah Wallah Silver Mine,Rye Park,New South Wales and its metallogenic significance     

Dr. K. G. McQueen  Ms Sara Box 《Mineralogy and Petrology》1988,39(3-4):289-305

Summary The Wallah Wallah lead-zinc-silver deposit near Rye Park, New South Wales, Australia, consists of epigenetic, vein-type mineralization developed in deformed Ordovician host rocks by deposition from medium temperature (280–380°C), low salinity fluids. In addition to dominant sphalerite, galena and arsenopyrite, the ores contain Ag-rich tetrahedrite, Ag-bearing stannite, teallite and trace cassiterite. The mineralogy and geochemistry of the ores, together with features of the geological setting and the regional metallogeny indicate that the oreforming fluids and metals were largely derived from a fractionated granitoid source, in or along the western margin of the Wyangala Batholith. The deposit appears to be part of a wider, but sporadically developed, magmatic-hydrothermal mineralising system, not previously recognised in this area.With 5 Figures  相似文献   

SCOUR RATE FORMULA     

Zhaoyin WANGProf Dr.  International Research  Training Center on Erosion  Sedimentation. P.O.Box  Beijing  China Jinchi HUANG Dr. Senior Engineer  China Institute of Water Resources  Hydro-Power Research  P.O.Box  Beijing . Chi 《国际泥沙研究》1997,(3)

I.INTRODUCTIONhiverchannelsaresubjecttocontinuouschangeingeometryduetoillteraCtionbetWeentheflowanderodibleboundaries.Ofconcerntothedesignersofoilpipelinesacrossariver,bridgesandhydraulicworksistheproblemofscourwhichcanunderminetheStructures.Scouratsiteofbridgesandhydraulicworksoccursduetoconstrictedflowandexistenceofbridgepiers.SuchatabOfscouroccursonlyinashortsection,usuallyillthesameorderofthelengthofthehydraulicworksorbridges.Therefore,thispatternofscouriscalledlocalscour.Man}rresea…  相似文献   

川滇菱形块体顺时针转动的构造学与古地磁学证据   总被引：22，自引：3，他引：22       下载免费PDF全文

徐锡伟  程国良  于贵华  宋方敏  向宏发  张兰凤  Hagai Ron  王洋龙  闻学泽 《地震地质》2003,25(1):61-70

川滇菱形块体内部受NE向丽江 -小金河断裂的切割 ,可进一步划分为川西北次级块体和滇中次级块体等南北 2个部分 ;各次级块体东边界断裂有规律地左旋滑动、西边界断裂的右旋滑动及其滑动速率值的差异 ,反映出新生代时期各次级块体作向SE的水平滑移叠加绕垂直轴顺时针转动的复合运动。其中 ,川西北次级块体SE向的水平滑移速率 5mm/a ,顺时针转动角速度 1 4°/Ma ;滇中次级块体SE向的水平滑移速率 3 5mm/a ,顺时针转动角速度约 1 5°/Ma。在滇中次级块体内部姚安、大姚、永仁、昆明北马街等地采集到约 90个古新世地层的定向样品 ,通过交变退磁和热退磁获得了它们各自的剩磁矢量 (实验磁偏角和磁倾角 ) ,由实测磁偏角与期望磁偏角相比可知川滇地区滇中次级块体中新世早期以来的顺时针转动累积量可达 30°～ 4 8°。次级块体的整体转动与块边活动断裂的左旋滑动符合左旋走滑断裂作用区块体作顺时针转动的运动学模式  相似文献   

Experimental Study on Hysucat Vessels     

M.S.Seif M.Askari 《中国海洋工程》2004,18(3):477-484

The paper contains the results of an experimental study on a planing catamaran. The aim of this study is resistance reduction with application of foils. Experiments are performed in different conditions and the results are compared with each other. The foils are used in different configurations and it is concluded that unsuitable design may result in larger resistance. But, it is also shown that, for a good design, the resistance may be reduced considerably.  相似文献   

Predicted Effects of Climatic Change on Distribution of Ecologically Important Native Tree and Shrub Species in Florida   总被引：3，自引：0，他引：3  

Elgene O. Box  David W. Crumpacker  E. Dennis Hardin 《Climatic change》1999,41(2):213-248

A previously developed plant species-climatic envelope model was evaluated further and used to predict effects of hypothesized climatic change on the potential distribution of 124 native woody plant species in Florida, U.S.A. Twelve scenarios were investigated. These included mean annual temperature increases of 1 °C or 2 °C, achieved either by equal 1 °C or 2 °C increases on a monthly basis throughout the year, or by disproportionately larger seasonal increases in winter and smaller ones in summer. The various temperature increases were then combined with each of several precipitation changes, ranging from +10% to –20%, to produce the final set of scenarios. More detailed analysis involving six of the scenarios and a subset of 28 representative, ecologically important species suggested that (1) large decreases in the Florida range of many temperate species would result if 1 °C warming occurs predominantly in winter or with a 20% decrease in annual precipitation, or (2) if 2 °C warming occurs, with or without decrease in annual precipitation, and regardless of whether there is a uniform monthly warming pattern or one that is higher in winter than in summer. Available information concerning other factors that might also affect climatic-change responses suggests that these large predicted impacts on temperate Florida species may be underestimates. Subtropical Florida species will tend to move north and inland with warming but extensive human assistance may be needed, if they are to realize their newly expanded, potential natural ranges.  相似文献