豫西南湍源银多金属矿集区典型矿床（点）——来自地质、流体特征及锆石U-Pb年龄的证据     

李胜利  姚娟  吴清杰  李泳泉  张德会 《中国区域地质》2012,(10):1608-1627

豫西南湍源银多金属矿集区位于秦岭造山带中部,分布有板厂铜多金属矿床、银洞沟银多金属矿床、许窑沟金矿床、银虎曼铅锌矿,以及万人洞沟、铁罗沟、万沟等金银矿点。流体包裹体研究表明,与含矿有关的石英脉流体包裹体组成复杂,特别是富气包裹体十分发育,而不含矿的石英包裹体类型简单,多为水盐包裹体。获得研究区内与成矿关系比较密切的卢家坪岩体和五龙潭岩体的锆石206Pb/238U年龄分别为446Ma±7Ma和424.6Ma±4.9Ma,据此认为该区成矿时间最早可延伸至加里东期。系统总结了矿集区矿床矿点的成矿作用过程,认为湍源银多金属异常区典型矿床可以分为以下几类：①与地层有关的火山喷流沉积及后期热液叠加改造的块状硫化物矿床（VMS-SEDEX）,火山作用提供成矿物质,后期热液改造形成矿床,代表性矿床为银虎曼铅-锌矿床;②与构造有关的蚀变岩-石英脉型金、银多金属矿床,成矿物质来源于深部和围岩,朱-夏断裂带次级构造提供容矿空间,代表性矿床为银洞沟银多金属矿床、许窑沟金矿;③与中酸性侵入岩有关的斑岩型-矽卡岩型矿床,成矿物质来源于深部和围岩,朱阳关-夏馆断裂带提供容矿空间,代表性矿床为板厂铜多金属矿床。  相似文献   

http://www.sciencedirect.com/science/article/pii/S1674987111001046     

C. Casquet  C.W. Rapel  R.J. Pankhurst  E.G. Baldo  C. Galindo  C.M. Fanning  J.A. Dahlquist  J. Saavedra 《地学前缘(英文版)》2012,3(2):137-145

The role played by Paleoproterozoic cratons in southern South America from the Mesoproterozoic to the Early Cambrian is reconsidered here.This period involved protracted continental amalgamation that led to formation of the supercontinent Rodinia.followed by Neoproterozoic continental break-up,with the consequent opening of Clymene and Iapetus oceans,and finally continental re-assembly as Gondwana through complex oblique collisions in the Late Neoproterozoic to Early Cambrian.The evidence for this is based mainly on a combination of precise U-Pb SHRMP dating and radiogenic isotope data for igneous and metamorphic rocks from a large area extending from the Rio de la Plata craton in the east to the Argentine Precordillera in the west and as far north as Arequipa in Peru.Our interpretation of the paleogeographical and geodynamic evolution invokes a hypothetical Paleoproterozoic block(MARA) embracing basement ultimately older than 1.7 Ga in the Western Sierras Pampeanas(Argentina),the Arequipa block(Peru),the Rio Apa block(Brazil),and probably also the Paraguaia block(Bolivia).  相似文献   

Tall building vibration control using a TM‐MR damper assembly: Experimental results and implementation     

Rene Zemp  Juan C. de la Llera  Paul Roschke 《地震工程与结构动力学》2011,40(3):257-271

This paper summarizes the relevant results of the design, construction, testing, and implementation of a nominal 120 kN magnetorheological damper developed to control a free‐plan tall building in Santiago, Chile, equipped with two 160‐ton tuned masses. Cyclic as well as hybrid simulation tests were performed on the prototype damper. Global building responses using measured MR properties showed good correlation with analytical estimations. Also, a proposed physical controller for the MR damper was validated through hybrid and building pull‐back tests. Its performance is essentially equivalent to that of an LQR controller, but the information needed in its implementation is considerably less. Pull‐back tests of 10 cm amplitude were performed on one mass along the flexible edge of the building and its response controlled using the passive and controlled modes of the MR damper. The MR damper was capable of controlling the TM displacements very effectively, as well as the simulated building response for different ground motions and harmonic excitation. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   

Tall building vibration control using a TM‐MR damper assembly     

Rene Zemp  Juan C. de la Llera  José L. Almazán 《地震工程与结构动力学》2011,40(3):339-354

  相似文献   

晚古生代泛大陆聚合过程中板块碰撞的运动学分析   总被引：1，自引：0，他引：1  

李江海  李维波  王洪浩  张华添  毛翔 《地质论评》2013,59(6):1047-1059

本文基于古板块再造方法,通过收集和筛选全球晚古生代古地磁数据,恢复再造泛大陆的构造格局及其聚合过程。晚古生代,全球板块的运动轨迹表明,全球板块整体以顺时针旋转的方式运动,聚合形成泛大陆。通过分析单个板块的运动学特征以及不同板块间的相对运动,表明在泛大陆聚合过程中,至少出现四种碰撞方式：① 追尾式碰撞：不同板块在同向运动过程中,板块运动速度存在差异,如前方板块速度慢于后方板块,则会造成其间洋盆逐渐收敛—关闭,如莱茵洋（海西造山带）、索伦洋（索伦山造山带）等。 ② 侧向式碰撞：两个板块运动轨迹大角度交叉,发生侧向碰撞,如波罗的板块向北运动过程中与向东北运动的西伯利亚板块碰撞,造成乌拉尔洋盆闭合,形成狭长的造山带。③ 错车式碰撞：两个板块,同向或者相向交错运动,在其侧翼发生走滑—斜向式聚合。如塔里木和华北板块转动方向相反,在侧翼斜向对接,以洋盆属性不明和走滑断层系发育为特征。④ 拥堵式碰撞：多个大板块之间汇聚区域的小陆块和地体发生多边汇聚,广泛出现岛弧增生和残余洋盆,如中亚造山带。  相似文献   

Gemstone Mineralization in the Palghat-Cauvery Shear Zone System (Karur-Kangayam Belt), Southern India     

M. Santosh  Alan S. Collins 《Gondwana Research》2003,6(4):911-918

We summarize here the occurrence of a number of semiprecious stones within a major gemstone belt in the Palghat-Cauvery shear zone system close to the northern margin of the Madurai Granulite Block, southern India. The gem mineralization in this belt includes different varieties of corundum (star ruby, sapphire), cordierite (iolite), feldspar (moonstones and sunstone of various hues), beryl (emerald, aquamarine), chrysoberyl (alexandrite), kornerupine, topaz, spinel, crystal quartz and amethyst, among others. Gem mineralisation has not been directly dated, but is associated with pegmatites that crosscut rocks metamorphosed in late Neoproterozoic/Early Cambrian times. Similar aged gem mineralization occurs south of the Achankovil Shear Zone in southern India, as well as in Sri Lanka and Madagascar and strengthen the view of a broad late Neoproterozoic-early Cambrian gemstone province in central Gondwana. The ruby mineralization within this belt can be correlated with similar occurrences in eastern Madagascar, supporting a correlation between the Malagasy Betsimisaraka suture zone and the Palghat-Cauvery shear zone system in southern India.  相似文献   

方形组合式钢丝绳隔震器静刚度试验研究     

卢红标  赵帆  蔡立艮  严东晋 《地震学刊》2009,(5):537-540

作者研制了一种新型方形组合式钢丝绳隔震器。该种隔震器由4个条形夹具夹持16根普通镀锌钢丝绳组合而成,从结构形式上保证了水平刚度对称。经过多次垂直向循环静力加卸载试验,运用Origin 7.0软件对实验数据进行分析处理,绘制出该种隔震器的静力特性曲线,并分别与目前防护工程中采用的条形不锈钢钢丝绳隔震器、鼓形钢丝绳隔震器的静力特性曲线进行了比较。试验结果表明,方形组合式钢丝绳隔震器不但具有初始刚度大、软特性明显、阻尼大、加工简便、性价比高等优点,而且克服了条形不锈钢钢丝绳隔震器价格高、水平刚度不相同和鼓形钢丝绳隔震器加工复杂的不足,在今后的防护工程隔震技术中有良好的应用前景。  相似文献   

辽河盆地荣兴屯地区中生界火山岩储集性能研究   总被引：7，自引：0，他引：7       下载免费PDF全文

梁晓东  赵志刚 《地球科学》2000,25(2):143-146

运用火山岩岩石薄片、铸体薄片、扫描电镜、孔、渗及压汞分析等多种分析测试手段研究了辽河盆地荣兴屯地区中生界火山岩储集性能, 认为: (1) 火山岩储集空间以次生孔缝为主, 原生孔缝大多已被充填; (2) 孔喉狭窄, 平均连通孔喉半径一般在0.100~ 0.500 μm左右.孔喉分布主要有单峰型和平峰型两种; (3) 孔隙组合类型有微裂缝型、微裂缝-孔隙型和孔隙型3种, 并以前两种类型为主; (4) 孔隙度值在1.0 %~ 16.3%之间, 渗透率在0.0 12× 10-3 ~12×10-3 μm2, 属低孔特低渗储集层; (5) 储层非均质性强, 渗透率级差为10 0 0, 突进系数为12.41, 变异系数为2.3.根据上述特点提出了火山岩储集层划分方案; (6) 由于孔/喉比值较小, 火山岩储集层的压汞退出效率较高, 平均达47.9%, 预示了较高的油气产能.   相似文献   

烃源岩评价分析项目的优化组合   总被引：1，自引：0，他引：1  

曹寅  钱志浩  张渠 《海相油气地质》2008,13(3)

在我国石油天然气行业中,对烃源岩评价的实验分析技术已形成一套比较成熟的方法,其中大部分已制订成国家标准或行业标准。但是在实际过程中,或者是全面测试,以致浪费大、收益小,或者是为过度节约而少测样品,造成信息严重丢失。为了分析测试能既节约成本又成果优秀,对各分析项目依据其有效性和局限性,分为基本项目、选择项目和补充项目三大类。针对不同的研究目的,分别提出了烃源岩样品快速筛选分析、烃源岩系统评价分析、下古生界海相烃源岩研究分析等相关实验测试分析项目的优化组合设计方案。  相似文献   

Relics of the Mozambique Ocean in the central East African Orogen: evidence from the Vohibory Block of southern Madagascar   总被引：4，自引：0，他引：4  

N. JÖNS  V. SCHENK 《Journal of Metamorphic Geology》2008,26(1):17-28

The Vohibory Block of south‐western Madagascar is part of the East African Orogen, the formation of which is related to the assembly of the Gondwana supercontinent. It is dominated by metabasic rocks, which have chemical compositions similar to those of recent basalts from a mid‐ocean ridge, back‐arc setting and island‐arc setting. The age of formation of protolith basalts has been dated at 850–700 Ma by U–Pb SHRIMP analysis of magmatic cores in zircon, pointing to an origin related to the Neoproterozoic Mozambique Ocean. The metabasic rocks are interpreted as representing components of an island arc with an associated back‐arc basin. In the early stage of the Pan‐African orogeny, these rocks experienced high‐pressure amphibolite to granulite facies metamorphism (9–12 kbar, 750–880 °C), dated at 612 ± 5 Ma from metamorphic rims in zircon. The metamorphism was most likely related to accretion of the arc terrane to the margin of the Azania microcontinent (Proto‐Madagascar) and closure of the back‐arc basin. The main metamorphism is significantly older than high‐temperature metamorphism in other tectonic units of southern Madagascar, indicating a distinct tectono‐metamorphic history.  相似文献