俄罗斯乌多坎砂岩型铜矿的成矿特征与找矿标志

乌多坎砂岩型铜矿是世界知名的超大型砂岩型铜矿之一。总结了该矿床形成的区域地质背景和矿床地质特征,建立了乌多坎砂岩型铜矿的找矿模型与找矿标志,对比了乌多坎砂岩型铜矿床与世界主要著名砂岩型铜矿床的特征,分析了它们之间成矿及赋矿的共同点。结果表明,世界著名的大型-超大型砂岩型铜矿均形成于后造山盆地或地台边缘的盆地(坳陷)中;矿体的规模与形态取决于岩性-岩相条件;矿化类型均具有Cu-Ag矿化特征;均具有干旱的古气候条件及滨海相、三角洲相、海湾-泻湖相的岩相-古地理环境。     

http://www.sciencedirect.com/science/article/pii/S1674987114000668

Microbial diversity in the hydrate-containing (sites SH3B and SH7B) and-free (sites SH1B, SH5B, SH5C) sediments collected from the Shenhu area of the South China Sea (SCS) was investigated using 16S rR...     

A maximum-entropy compound distribution model for extreme wave heights of typhoon-affected sea areas

A new compound distribution model for extreme wave heights of typhoon-affected sea areas is proposed on the basis of the maximum-entropy principle.The new model is formed by nesting a discrete distribution in a continuous one,having eight parameters which can be determined in terms of observed data of typhoon occurrence-frequency and extreme wave heights by numerically solving two sets of equations derived in this paper.The model is examined by using it to predict the N-year return-period wave height at two hydrology stations in the Yellow Sea,and the predicted results are compared with those predicted by use of some other compound distribution models.Examinations and comparisons show that the model has some advantages for predicting the N-year return-period wave height in typhoon-affected sea areas.     

The deep and shallow structure,composition and its relation to earthquakes in Chaoyang — Yixian seismic region

This paper describes synthetically the seismic activity, deep and shallow structures and rock dynamic features in and near Chaoyang—Yixian region. It is supposed that there is a low velocity layer in middle crust and the three-layered crustal velocities are all lower than that in both sides of the region. There exists uplifts of upper mantle and asthenosphere-low resistance layer. It is also studied the composition of matter of three-layered crust, low velocity layer, upper mantle and asthenosphere. In the end the direct relations between the deep and shallow structure, composition and the seismic activity and new activities of faults in this region are discussed.     

PBO钻孔应变同震响应分析

以2017-09-08墨西哥8.1 级地震为例,分析14个PBO综合钻孔应变仪和地震仪同址记录的地震波信号,结果表明,应变仪记录的地震波符合射线传播规律。对不同震中距的站点进行基于S变换的应变仪与地震仪的同震响应特征分析,二者同震响应一致性较好,应变仪频段主要在0.25 Hz以下。取震后1 h应变数据进行分析发现,同震阶段应变主方向指向震中。     

Effects of nutritional factors on the growth and heterotrophic eicosapentaenoic acid production of diatom <Emphasis Type="Italic">Nitzschia laevis</Emphasis>

The effects of several nutritional factors on the growth and eicosapentaenoic acid (EPA) production of diatom Nitzschia laevis were studied. 4 LDM (quadrupled concentration of the nutrient salt) was the optimal concentration of nutrient salt for the growth and EPA production of N. laevis. The growth of N. laevis was inhibited when the glucose concentration was either lower than 10 gL⁻¹ or higher than 15 gL⁻¹. Both sodium nitrate and urea were good nitrogen sources for the growth and EPA production, while ammonium chloride seriously decreased the dry cell weight (DW) and the EPA content. Silicate seriously influenced the growth of N. laevis. The maximum DW of 2.34 gL⁻¹ was obtained in the presence of 150 mgL⁻¹ Na₂SiO₃·9H₂O. The EPA content remained almost the same when the silicate concentration was lower than 150 mgL⁻¹; however, higher silicate concentrations resulted in a steady decrease of EPA content. Low medium salinity (⩽29) did not seem to influence the DW of N. laevis, and high salinity resulted in a decrease of DW. The highest EPA content (4.08%) and yield (110 mgL⁻¹) were observed at the salinity of 36 and 29, respectively.     

因子克里格分析支持的重金属元素空间多尺度变化特征——以北部湾东北部海域为例

将因子克里格分析方法应用于海底沉积物重金属元素空间多尺度变化的研究中,分析了北部湾东北部表层沉积物中7种重金属元素,Ni、Cu、Zn、Pb、Cr、As和Cd的空间多尺度结构特征,识别并分离了重金属元素不同尺度的空间变化,并探讨了各个尺度上重金属的物源及控制因素。结果显示,研究区重金属存在块金效应、变程为30km的球状结构(短变程尺度)和变程为140km的球状结构(长变程尺度)等三种尺度的空间结构,并拟合了研究区7种重金属元素的线性协同区域化模型。短变程尺度上,7种重金属元素的空间分布表现为"点状"或"条带状"的局部尺度的空间变化特征;长变程尺度上,7种重金属元素的空间分布反映出"片状"的区域尺度的空间变化特征。局部尺度上,Zn、Cr、Ni、Cu、Pb和Cd等元素主要源于海南岛、雷州半岛、广西大陆等陆地母岩物质,其空间分布特征受到了沉积物粒度的控制作用;而As主要受到海南岛、雷州半岛的人为污染成分的影响。区域尺度上,Zn、Cr、Ni和Cu主要来源于雷州半岛、海南岛的母岩物质,其次为广西大陆;As主要来源于海南岛的母岩物质,其次为雷州半岛、广西大陆。这些重金属元素在北部湾终年逆时针大环流的控制下,进行搬运、迁移并沉积在"汇聚中心",形成了研究区重金属元素区域尺度上NWW-NNW向的分布格局;而As不同于其他元素的亲陆的NNW向分布特征,主要源于其不同的地球化学行为。     

江苏省主要湖泊的降水量与湖泊的降水效应

本文分析了江苏境内主要湖泊的降水量特征,揭示了长江是江苏各湖泊不同降水量特征的一条十分明显的天然界线;估算了太湖的降水效应,并据此推估出江苏主要湖泊的降水效应不太明显;江苏各湖泊的降水量与其水位年过程趋势相似,只是后者位相滞后于前者而已。     

郯庐断裂北带地区主要构造单元壳幔结构特征与地震活动性.

以东北地区的地学断面及其相关资料为基础,分析了郯庐断裂北带地区的地壳-上地幔结构特征与不同地壳构造单元地震活动性之间的关系．结果表明：郯庐断裂北带两侧的壳幔结构存在明显差异,断裂带本身的发育与壳幔结构变异带关系密切;断裂的活动特点及分段明显受到地壳介质力学特性影响;郯庐断裂北带地区软流层的起伏与地貌形态呈明显的镜像关系,前者还制约着不同地壳构造单元的构造活动性及变形方式;郯庐断裂北带地区南、北两端地震较为活跃地段均与壳内低速 高导层发育地段相对应的事实,证明了刚性地块中壳幔结构较为复杂的活动断裂段是构成中强地震的主要控震构造．