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61.
本文基于格林公式,给出了均匀二度体重力异常线积分表达式的严格数学推导过程,其结果与前人推导出的结果完全相同,但我们的方法在数学上更简单,也更严谨.在此基础之上,我们详细讨论了多边形截面二度体重力异常计算公式中所包含的数值不稳定性,并作了适当的修正.新的计算方法在数值上是稳定的,且适用于包括场源内部以及边界上的任意空间位置.为了对新算法进行验证,我们以一个均匀无限长水平圆柱体及其内接正多边形截面棱柱体为模型,分别利用解析公式和本文所提供的算法计算了二者在不同深度的两条水平观测线上所产生的重力异常,其中一条观测线穿过了模型的内部.通过两种途径计算得到的重力异常在两条测线上都是吻合的,这表明新算法是正确的. 相似文献
62.
从Delamerian造山带的碎锆年代看冈瓦纳早古生代太平洋边缘的发育T.R.Ireland等大陆边缘板块的重组通常伴随着强烈侵蚀,继而发生源区不明的单一碎屑物的巨量沉积。然而,沉积物源区地壳要素的重要信息通常记载在碎锆石的年代谱上。这些年代谱对于了... 相似文献
63.
为了深入研究东北地区断裂分布及构造分区,利用全国1∶2 500 000布格重力异常图,分析了泛东北地区(包括东北3省及内蒙古自治区的东北部分地区)的区域重力场特征。利用布格异常变化形态,并参考地质资料,在研究区内划分出岩石圈断裂14条,壳内断裂11条。根据大兴安岭和依兰—伊通两条明显的重力异常梯级带把研究区划分出兴安、松嫩以及张广才岭等三大重力异常区,在划分断裂和分析重力场特征的基础上进行了构造分区。其研究成果为认识和研究泛东北地区油气与矿产分布提供了重力场方面的依据。 相似文献
64.
针对提高重力勘探正反演解释的分辨率问题,提出利用Hilbert变换计算和研究重力归一化总梯度.文中从理论上详细地证明了方法的可行性,给出了适合计算机实现的计算方法.为探讨该方法对油气藏的分辨能力,在模型计算中,分别利用Fourier级数法、Fourier变换法和本文提出的Hilbert变换法计算模型的GH场值,发现当三度体储油球冠模型(模拟似三度贮油气藏背斜模型)油气藏部分(低密度体)厚度减小到低于球冠厚度的十分之一时,Fourier级数及变换法不能分辨出低密度体所产生的异常,而Hilbert变换法仍然可以清晰地识别,这说明用Hilbert变换法计算的GH场对异常识别的分辨率优于其他两种方法. 相似文献
65.
本文利用面积广、勘探深度大的重磁数据通过增强型局部相位边界识别方法和优化欧拉反褶积法获得东海陆架盆地的构造特征,为油气勘探提供基础资料。增强型局部相位边界识别法是重磁数据一阶和二阶水平导数的比值函数,能有效地均衡不同深度地质体的边界响应,从而同时显示不同深度构造的边界,提高对较深层构造的分辨率;优化欧拉反褶积法有效地降低了背景异常的干扰,从而可获得更加准确的构造反演结果。理论模型研究表明,增强型局部相位边界识别法可更加准确和清晰地划分边界信息,优化欧拉反褶积法可获得更加准确和收敛的反演结果。综合利用增强型局部相位边界识别和优化欧拉反褶积法对东海陆架断裂构造分布进行划分,获得了分析区域构造背景和评估油气潜力的基础资料。 相似文献
66.
H- and K-band moderate-resolution and 4 μm high-resolution spectra have been obtained for FMM 362, a bright star in the Quintuplet Cluster near the Galactic center. The spectral features in these bands closely match those of the Pistol Star, a luminous blue variable and one of the most luminous stars known. The new spectra and previously obtained photometry imply a very high luminosity for FMM 362, L>/=106 L middle dot in circle, and a temperature of 10,000-13,000 K. Based on its luminosity, temperature, photometric variability, and similarities to the Pistol Star, we conclude that FMM 362 is a luminous blue variable. 相似文献
67.
Comparing bleaching and mortality responses of hard corals between southern Kenya and the Great Barrier Reef, Australia 总被引:1,自引:0,他引:1
We compared the bleaching and mortality response (BMI) of 19 common scleractinian corals to an anomalous warm-water event in 1998 to determine the degree of variation between depths, sites, and regions. Mombasa corals experienced a greater temperature anomaly than those on the Great Barrier Reef (GBR) sites and this was reflected in the greater BMI response of most taxa. Comparing coral taxa in different sites at the same depth produced high correlation coefficients in the bleaching response in Kenya at 2 m (r=0.86) and GBR at 6 m depth sites (r=0.80) but less in the GBR for shallow 2 m sites (r=0.49). The pattern of taxa susceptibility was remarkably consistent between the regions. Coral taxa explained 52% of the variation in the response of colonies to bleaching between these two regions (Kenya BMI=0.90 GBR BMI+26; F(1,19) - 18.3; p < 0.001; r2 = 0.52). Stylophora and Pocillopora were consistently susceptible while Cyphastrea, Goniopora Galaxea and Pavona were resistant in both regions. Three taxa behaved differently between the two regions; Acropora, and branching Porites were both moderately affected on the GBR but were highly affected in Kenya while the opposite was true for Pavona. These results suggest that a colonies response to bleaching is phylogenetically constrained, emphasizing the importance of features of the host's physiology or morphology in determining the response to thermal stress. 相似文献
68.
Spatial interpolation methods for nonstationary plume data 总被引:1,自引:0,他引:1
Plume interpolation consists of estimating contaminant concentrations at unsampled locations using the available contaminant data surrounding those locations. The goal of ground water plume interpolation is to maximize the accuracy in estimating the spatial distribution of the contaminant plume given the data limitations associated with sparse monitoring networks with irregular geometries. Beyond data limitations, contaminant plume interpolation is a difficult task because contaminant concentration fields are highly heterogeneous, anisotropic, and nonstationary phenomena. This study provides a comprehensive performance analysis of six interpolation methods for scatter-point concentration data, ranging in complexity from intrinsic kriging based on intrinsic random function theory to a traditional implementation of inverse-distance weighting. High resolution simulation data of perchloroethylene (PCE) contamination in a highly heterogeneous alluvial aquifer were used to generate three test cases, which vary in the size and complexity of their contaminant plumes as well as the number of data available to support interpolation. Overall, the variability of PCE samples and preferential sampling controlled how well each of the interpolation schemes performed. Quantile kriging was the most robust of the interpolation methods, showing the least bias from both of these factors. This study provides guidance to practitioners balancing opposing theoretical perspectives, ease-of-implementation, and effectiveness when choosing a plume interpolation method. 相似文献
69.
查明大庆外围中、新生代断陷盆地群的油气潜力,选取有利勘探战略目标区是一个亟待解决的问题。针对漠河盆地内的重力场资料特点和需要解决的地质问题,采用了下列常规处理技术:曲线的圆滑、方向导数的计算;同时,采用了DCT反演技术。通过以上常规及特殊处理方法,得出漠河盆地的结晶基底深度及形态并划分出断裂的位置与断裂深度,经过与地质资料的对比,取得了较好的效果。 相似文献
70.
Arsenic in glacial aquifers: sources and geochemical controls 总被引:1,自引:0,他引:1
A total of 176 wells in sand-and-gravel glacial aquifers in central Illinois were sampled for arsenic (As) and other chemical parameters. The results were combined with archived and published data from several hundred well samples to determine potential sources of As and the potential geochemical controls on its solubility and mobility. There was considerable spatial variability in the As concentrations. High concentrations were confined to areas smaller than 1 km in diameter. Arsenic and well depth were uncorrelated. Arsenic solubility appeared to be controlled by oxidation-reduction (redox) conditions, especially the presence of organic matter. Geochemical conditions in the aquifers are typically reducing, but only in the most reducing water does As accumulate in solution. In wells in which total organic carbon (TOC) was below 2 mg/L and sulfate (SO4(2-)) was present, As concentrations were low or below the detection limit (0.5 microg/L). Arsenic concentrations >10 microg/L were almost always found in wells where TOC was >2 mg/L and SO4(2-) was absent or at low concentrations, indicating post-SO4 (2-)reducing conditions. Iron (Fe) is common in the aquifer sediments, and Fe oxide reduction appears to be occurring throughout the aquifers. Arsenic is likely released from the solid phase as Fe oxide is reduced. 相似文献