四川盆地及邻区下寒武统龙王庙组颗粒滩沉积特征与空间分布

通过对区域地质调查剖面资料和钻井资料的研究,结合对部分野外剖面与钻井岩心的系统观察和取样分析,发现四川盆地及邻区下寒武统龙王庙组的颗粒滩主要由颗粒石灰岩(白云岩)和晶粒白云岩构成;颗粒滩以未暴露浅滩为主,发育向上变浅和向上变深2类垂向序列。川中古隆起和黔中古隆起北部地区的颗粒滩的横向规模大、层位稳定性和连续性最好,其余地区颗粒滩多表现为点滩且规模较小。研究区龙王庙期总体上为西浅东深,西南缘、西北缘和北缘为古陆环抱,盆内呈“一隆两坳”的古地理格局。颗粒岩在古地貌高地具有广覆式“五线一带”的平面分布样式。川中古隆起、黔中古隆起北部地区是颗粒滩发育最有利的地区,东北部和东南部的水下岛链区是优质颗粒滩带发育的潜在区。古隆起发育演化对颗粒滩和有利储集相带具有明显的控制效应,次一级海平面升降变化影响滩体的垂向叠置样式和横向连续性。     

Evolution of the Late Triassic Paleo-uplift in the Southwestern Upper Yangtze Region and its Tectonic SignificanceEI北大核心CSCD

Based on field geological survey and stratigraphic analysis, a Late Triassic Paleo-uplift is identified in the southwestern upper Yangtze region. The tectonic features, evolution history and tectonic significance of this paleo-uplift are discussed in detail in this paper. The results suggest that the hiatus of the Upper Triassic in the southwestern upper Yangtze region was resulted from the paleo-uplift that roughly parallel to the southwest margin of the upper Yangtze region. The formation of the paleo-uplift is related to the closure of the Jinshajiang-Ailaoshan-Songma-Babu and Ganzi-Litang Oceans and their subsequent collisional orogenesis along the southwest margin of the upper Yangtze region. The forebulges of the Youjiang and Chuxiong Foreland Basins were formed by the closure of the Jinshajiang-Ailaoshan-Songma-Babu Ocean, comprising the paleo-uplift at the end of the Early Triassic. Then the forebulge of the Xichang Foreland Basin was developed by the closure of the Ganzi-Litang Ocean in the Norian, and became a new part of the paleo-uplift. Owing to the termination of the Youjiang Foreland Basin at the end of the Rhaetian, the paleo-uplift was composed only of the forebulges of the Chuxiong and Xichang Foreland Basins. The discovery of the paleo-uplift will help us to better understand the prototype of the Sichuan Basin and the tectonic evolution of the southwestern upper Yangtze region during the Late Triassic. © 2017, Science Press. All right reserved.     

甘肃西和县金崖沟金锑矿特征浅析

甘肃西和县金崖沟金、锑矿位于南秦岭北部的岷县鹿儿坝—西和崖湾—两当广金坝金、汞、锑成矿亚带上。矿带长约1 km,由一条NE向高角度断层F1控制,矿(化)体主要处于断层的下盘即南东盘,矿体产状280°~315°∠67°~80°,不连续,呈透镜状、扁豆状,在纵向上及垂向上矿体产状均变化较大,形态主要随断层错动形成的虚脱空间形态的变化而变化。金矿呈透镜状、板状、长条状,品位1.05~3×10~(-6),厚度0.78~3.20 m不等,锑品位1.14%~3.41%,平均厚度1.26 m。金矿对岩石有一定的选择性,主要以铅锌铜硫化矿物包裹金形式赋存于断层破碎带中的硅化角砾岩中。锑矿不具规模,多分布于两断层交汇处呈鸡窝状产出,即在构造复杂流体流通较好且有利的容矿空间成矿,呈浸染状、放射状、针状,锑矿与金矿局部伴生,局部独立存在。     

GPS软件接收机捕获方法研究

为解决GPS软件接收机中频信号的捕获问题,首先基于FFT的并行码捕获实现了对基带信号的粗捕,对粗捕的捕获判决进行改进,采用自适应门限值调整方法,即基于次高峰判决,同时对次高峰的寻找采用开窗原理;然后利用FFT的频域分析方法进行精捕。与传统相位差分精捕不同,利用FFT频域内对中频信号进行精捕,通过增大FFT变换的点数来提高精捕频率的分辨率,同时具体给出了粗捕和精捕的具体捕获步骤以及主要的技术问题;最后利用一组GPS实测数据对上述分析进行了计算,实验结果表明：基于FFT的GPS信号的粗捕与利用FFT的频域精捕方法非常有效,捕获快速准确,可以满足GPS软件接收机的要求。     

武汉城市圈空间演变的社会经济机制分析

城市化是城市圈社会经济发展和地域空间演变的主要原动力。以武汉城市圈为例,构建城市圈空间演变的动力模型和评价指标体系,运用SPSS12.0软件,通过回归分析,以城市化变量表征城市圈空间演变过程,分析武汉城市圈空间演变的相关动力机制,得出城市圈空间演变表现为动态螺旋跳跃式上升曲线,是城市化、工业化、服务产业化、信息化、运输化等经济社会要素相互作用、共同耦合的结果,同时,各影响因子在城市化的不同发展阶段对城市圈空间发育发挥着不同的作用,主导因子表现为工业化(1949—1965年)—第三产业化(1966—1979年)—市场化与制度化(1980—1989年)—多因素(1990—2008年)推动作用的变化过程。     

An overview of the spatial patterns of land surface processes over arid and semiarid regions

With data from the project Collaborative Observation of Semi-arid/Arid Regions in North China, collected during July and September 2008, the spatial patterns of land surface processes over arid and semiarid regions have been investigated based on the ordinary Kriging interpolation approach. Generally, for the radiation processes, downward and upward short-wave radiation have a uniformly increasing trend with latitude, but the spatial patterns of long-wave radiation present notable regional differences: both upward and downward long-wave radiation increase with latitude in the west of North China, while in the east they vary inversely with latitude, suggesting surface temperature and clouds respectively have feedbacks to the long-wave radiation in the west and east of North China. The surface net radiation basically has a negative latitudinal trend. Long-wave radiation budget plays an important role in the spatial pattern of surface net radiation, particularly in the east of North China, although short-wave radiation budget largely determines the magnitude of surface net radiation. For the energy processes, latent and sensible heat flux varies conversely with latitude: more available land surface energy is consumed by evaporating soil water at lower latitudes while more is used for heating the atmosphere at higher latitudes. A soil heat flux maximum and minimum are found in Loess Plateau and Qinghai Plateau respectively, and a maximum is seen in the northeast China.     

基于小波变换与小波包变换的降噪方法比较

在模拟地震记录信号中加入信噪比为17的高斯白噪声,然后分别采用小波降噪和小波包降噪方法,对含噪信号进行降噪处理。在不同降噪阈值下,比较降噪后信号的信噪比。结果表明:在同一降噪阈值下,小波包降噪后信号的信噪比高于小波降噪后信号的信噪比,而且采用wbmpen方法给定的阈值明显可以提高降噪后信号的信噪比。     

JCZ-1T超宽频带地震计LP垂直通道记录的固体潮特征

JCZ-1T超宽频带地震计具有全频带覆盖特性,其低频端输出延伸到固体潮汐,利用地震计LP通道的垂直分向观测数据,经过处理获得有关的固体潮资料,通过对记录信号的频谱分析对其有了初步的认知。JCZ-1T超宽频地震计LP加速度垂直通道记录的观测信号以固体潮汐信息为主,用该仪器观测可以获取与地震相关的综合观测数据,分析JCZ-1T记录波形叠加的的固体潮信息有着重要的实际意义,通过对资料处理运用,可以与传统前兆仪器结合观测,拓展其研究应用领域,更好的服务于地震科学研究。     

Residual curvature migration velocity analysis for angle domain common imaging gathers

Pre-stack depth migration velocity analysis is one of the keys to influencing the imaging quality of pre-stack migration. In this paper we cover a residual curvature velocity analysis method on angle-domain common image gathers (ADCIGs) which can depict the relationship between incident angle and migration depth at imaging points and update the migration velocity. Differing from offset-domain common image gathers (ODCIGs), ADCIGs are not disturbed by the multi-path problem which contributes to imaging artifacts, thus influencing the velocity analysis. On the basis of horizontal layers, we derive the residual depth equation and also propose a velocity analysis workflow for velocity scanning. The tests to synthetic and field data prove the velocity analysis methods adopted in this paper are robust and valid.     

Anti-proliferative activity of phlorotannin extracts from brown algae Laminaria japonica Aresch

In this study, we evaluated the anti-proliferative activity of phlorotannins derived from brown algae Laminaria japonica Aresch extracts on the human hepatocellular carcinoma cell (BEL-7402) and on murine leukemic cells (P388) by MTT assay. Cells were incubated with 100 μg/mL of the phlorotannin extract (PE) for 48 h. The inhibitory rate of PE on BEL-7402 and P388 cells was 30.20±1.16% and 43.44±1.86%, respectively, and the half-inhibitory concentration of PE (IC₅₀) on P388 and BEL-7402 cells was 120 μg/mL and >200 μg/mL, respectively. Microscopic observation shows that the morphologic features of tumor cells treated with PE and 5-fluorouracil are markedly different from the normal control group. The inhibitory rate of fraction A₂ isolated from PE by sephadex LH-20 for BEL-7402 and P388 cells at the sample concentration of 70.42 μg/mL was 61.96±7.02% and 40.47±8.70%, respectively. The apoptosis peak for fraction A₂ was the most profound of all fractions used in the flow cytometry assay. The results indicate that the anti-proliferative of this algal extract is associated with the total phlorotannin content.