下庄铀矿田337矿床成矿流体稀土元素示踪     

张国玉  王正其  梁良 《华东地质学院学报》2006,29(1):27-31

337铀矿床位于下庄矿田东缘,区内发育近EW向、NNE向构造裂隙群及NW向辉绿岩和正长岩脉体,发育以碱性为主的多种围岩蚀变。区内矿床主要赋矿围岩的稀土元素特征属壳源型。矿石内金属矿物以沥青铀矿为主,矿石的LREE/HREE比值为3.25,Sm/Nd比值平均为0.307,Ce/Yb比值为7.127,这些数据都显示出成矿流体具有较深来源。矿石较围岩亏损稀土元素尤其是轻稀土元素,稀土元素分布模式平缓,与幔源辉绿岩特别是与正长岩的稀土元素分布模式相近,负铕异常比围岩更为强烈,反映成矿流体的来源具有幔源性。结合区域地质特征,可以认为337矿床成矿流体来源具有幔源性质。  相似文献   

Continent–ocean transition and voluminous magmatic underplating derived from P-wave velocity modelling of the East Greenland continental margin     

Max Voss  Wilfried Jokat 《Geophysical Journal International》2007,170(2):580-604

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弯曲射线追踪中Dijkstra算法的改进与实现          下载免费PDF全文

王汪根  刘盛东  张平松 《地球物理学进展》2006,21(4):1120-1126

文章针对图论中寻找最短路径的Dijkstra算法内存占用量大，效率低的缺点，对该算法进行了改进，修改后的算法计算效率是原来的四倍，内存使用量和图中节点数呈线性关系.在此基础上，用新算法求出了激发点和接收点的最短走时路径，并由激发接收点的旅行时结合联合迭代法对理论模型和实际场地进行了反演.结果表明：和直射线追踪相比，弯曲射线路径能更好地反演出地质体内部的速度场分布.理论模型和实际探测结果证实改进后的算法是有效的.  相似文献   

地磁台站建设中磁测异常现象分析     

吴乔木 《地震地磁观测与研究》2006,27(4):63-66

地磁台建设磁性跟踪测试工作很重要,通过对跟踪磁测中发现的一个异常现象的分析,计算了不同重量、距离的铁磁性物质对磁房建筑场地磁场的影响,讨论了排除施工现场磁性干扰的一些办法,并得出各种重量铁磁性物质与磁房建筑物的安全距离,还讨论了地磁台部分建筑材料的选择问题。  相似文献   

Composition and applied sedimentology of salt from brines of the Mamfe Basin, Cameroon     

E. Eseme  P.A. Abanda  C.M. Agyingi  J. Foba-Tendo  R.E. Hannigan 《Journal of Geochemical Exploration》2006,91(1-3):41-55

Salts produced using brines of the Mamfe Basin were analysed by XRD for their mineral composition and ICP-MS for minor element composition. Halite (NaCl) and dolomite (CaMg (CO₃)₂) constitute the major minerals with minor impurities from Mo and Cd in the chlorides and Sc and Cu in the carbonates. The mineral composition is evidence of dissolution of evaporites with parent brine of marine origin. Other elements analysed are suggested to be adsorbed to these salts and result from water–rock interaction. The elements partitioned based on their correlation to other elements are suggested to derive from sulphates including barite for Ba, sulphides for Pb, Zn, silicates for Zr, Mn and oxides for V, Cr. The electrical conductance of the brines is related to the salt yield by the equation; M = 9 × 10^− 4E− 3.27, and it can be used to estimate salt yield throughout the year. Over 1200 tons of salt consisting dominantly of grade I halite are lost annually as brines across the basin. Purification is required for some minor elements including Ba, Pb, Hg and Cd for use as a condiment. A genetic relation between the parent brine, sulphide minerals and organic matter-rich sediments is proposed.  相似文献   

Detrital zircon reference for the North China block   总被引：17，自引：0，他引：17  

Brian J. Darby  George Gehrels   《Journal of Asian Earth Sciences》2006,26(6):637-648

U–Pb analyses of 250 single detrital zircons from Upper Proterozoic to Ordovician strata collected from the Zhuozi Shan in north-central China provide a detrital zircon reference for the North China block, a major crustal entity in the Asian tectonic collage. The results, which range in age from 1.72 to 2.97 Ga, shed new light on the age of the crystalline basement in North China, much of which is covered by younger sedimentary units. In addition, this detrital zircon reference can be used to help determine the provenance of clastic sedimentary units and for assessing validity of paleogeographic and regional tectonic models that include the complex history of Asian continental amalgamation, terrane accretion, and subsequent translation that is ongoing today.  相似文献   

Petrofacies, provenance and diagenesis of the dhosa sandstone member (Chari Formation) at Ler, Kachchh sub-basin, Western India     

A.H.M. Ahmad  G.M. Bhat   《Journal of Asian Earth Sciences》2006,27(6):857-872

The sandstones of the Dhosa Sandstone Member of Late Callovian and Early Oxfordian age exposed at Ler have been analyzed for their petrofacies, provenance, tectonic setting and diagenetic history. These sandstones are fine to medium grained and poorly- to well sorted. The constituent mineral grains are subangular to subrounded. These sandstones were derived from a mixed provenance including granites, granite–gneisses, low- and high-grade metamorphic and some basic rocks of the Aravalli Range and Nagarparkar Massif. The petrofacies analysis reveals that these sandstones belong to the continental block-, recycled orogen- and rifted continental margin tectonic regime.The imprints of early and deep burial diagenesis of these sandstones include different stages of compaction, cementation, change in crystal boundaries, cement–cement boundaries, chertification and neomorphism. The sequence of cementation includes precipitation of calcite and its subsequent replacement by Fe calcite and silica cements. The typical intermediate burial (2–3 km depth) diagenetic signatures of these sandstones are reflected in the formation of suture and straight-line boundaries, and triple junctions with straight-line boundaries. The depositional environment, relatively low-energy environment that was below storm wave base but subjected to gentle currents, of the Dhosa Sandstone Member controlled the early diagenesis, which in turn influenced the burial diagenesis of these sandstones.  相似文献   

From source terrains of the Eastern Alps to the Molasse Basin: Detrital record of non-steady-state exhumation   总被引：2，自引：1，他引：2  

J. Kuhlemann  I. Dunkl  A. Brügel  C. Spiegel  W. Frisch 《Tectonophysics》2006,413(3-4):301-316

Fission-track cooling ages of detrital apatite (AFT) in the East Alpine Molasse Basin display age groups corresponding to geodynamic events in the orogen since Jurassic times. These age groups are typical of certain thermotectonic units, which formed a patchwork in the Swiss and Eastern Alps. By a combination of petrographic and thermochronologic data, progressive erosion of source terrains is monitored in different catchments since the Oligocene. The AFT cooling ages show a decrease in lag time until when rapidly cooled debris derived from tectonically exhumed core complexes became exposed. After termination of tectonic exhumation, lag times of debris derived from the core complexes increased. Neither on the scale of the entire Eastern Alps, or on the scale of individual catchments, steady-state exhumation is observed, due to the highly dynamic changes of exhumation rates since Late Eocene collision.  相似文献   

PS转换波界面二次源法射线追踪          下载免费PDF全文

王童奎  张美根  李小凡  李瑞华  龙桂华 《地球物理学进展》2007,22(1):165-170

界面二次源法是最近提出的一种最小走时射线追踪方法，尤其适合层状介质中走时和射线路径的计算.该方法相对于传统的最小走时树方法（如Moser法），仅在物性界面上设置二次源，射线路径的方向只在层界面处发生改变，该方法最大程度地消除了射线路径的锯齿状现象，同时也避免了低变速区的射线路径多值现象，因此，它具有更高的追踪精度和效率.本文采用界面二次源法在各向同性介质中实现了PS转换波射线追踪，理论模型的计算证实了界面二次源法追踪PS转换波的准确性和高效性，同时该方法在各向异性介质中也很好地追踪出分离的PSV波和PSH波，因此该方法有利于横波分裂在地震勘探中的研究和应用  相似文献   

线性体图像自动矢量化算法研究     

李增兵  张晓帆 《测绘与空间地理信息》2006,29(5):22-24

依据线图的结构特点,首先提取节点信息快速抓住图像的总体拓扑结构,然后以节点信息指导进行矢量跟踪,能够有效解决复杂的交叉点问题,提高矢量化的效率和精度。基于节点信息指导和对不同连通体分类跟踪的方法避免了跟踪起始点选取的随意性和跟踪方向选取的盲目性,并具有抗噪性好和适应性强的特点。  相似文献