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211.
Jian Cao Zhijun Jin Wenxuan Hu Yijie Zhang Suping Yao Xulong Wang Yueqian Zhang Yong Tang 《Marine and Petroleum Geology》2010
Calcite veins and cements occur widely in Carboniferous and Permian reservoirs of the Hongche fault zone, northwestern Junggar Basin in northwest China. The calcites were investigated by fluid inclusion and trace-element analyses, providing an improved understanding of the petroleum migration history. It is indicated that the Hongche fault behaved as a migration pathway before the Early Cretaceous, allowing two oil charges to migrate into the hanging-wall, fault-core and footwall reservoirs across the fault. Since the Late Cretaceous, the Hongche fault has been sealed. As a consequence, meteoric water flowed down only into the hanging-wall and fault-core reservoirs. The meteoric-water incursion is likely an important cause for degradation of reservoir oils. In contrast, the footwall reservoirs received gas charge (the third hydrocarbon event) following the Late Cretaceous. This helps explain the distribution of petroleum across the fault. This study provides an example of how a fault may evolve as pathway and seal over time, and how reservoir diagenetic minerals can provide clues to complex petroleum migration histories. 相似文献
212.
对海莲(Brugiera sexangula)幼苗进行不同浓度的铝盐处理,采用微波消解和电感耦合等离子体质谱法(ICP-MS)测定了海莲幼苗叶片,茎和根组分的Na、Mg、K、Ca、Mn、Fe、Cu、Zn和Al金属元素含量。结果显示,随培养液Al浓度的增加,海莲叶片、茎和根部Al的积累增加,其中根组分增加尤为显著。Al胁迫下,海莲根部对Na的吸收增强,但在叶和茎中的变化不显著;10 mmol/L的Al处理促进了根对K的吸收;Al显著抑制了Mn和Fe在海莲中的积累;Cu、Zn含量在海莲各器官中的变化不一致。此外,25 mmol/L和50 mmol/L Al处理的海莲幼苗根部对Ca的积累显著增加,有利于Al毒害的缓解作用。 相似文献
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214.
该文探讨了马超营断裂带内各地层的成矿元素丰度特征,阐述了该带内成矿元素的分布特征及分布规律,总结了Au及有关元素Ag、Pb、Zn、Mo、Co、Ni、Mn、Ba、Sr、As、Sb、Bi等异常的特征及其分布规律。研究成果表明:马超营断裂带的韧性—韧脆性剪切带是本区Au及与其相关的Ag、Pb、Zn等成矿元素异常规模、形态和空间分布的控制因素。 相似文献
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217.
E. A. Belousova S. Walters W. L. Griffin S. Y. O'Reilly 《Australian Journal of Earth Sciences》2013,60(4):603-619
The concentrations of trace elements in apatite from granitoid rocks of the Mt Isa Inlier have been investigated using the laser‐ablation inductively coupled plasma‐mass spectrometry (ICP‐MS) microprobe. The results indicate that the distribution of trace elements (especially rare‐earth elements (REE), Sr, Y, Mn and Th) in apatite strongly reflects the chemical characteristics of the parental rock. The variations in the trace‐element concentrations of apatite are correlated with parameters such as the SiO2 content, oxidation state of iron, total alkalis and the aluminium saturation index (ASI). The relative enrichment of Y, HREE and Mn and the relative depletion of Sr in the apatites studied reflect the degree of fractionation of the host granite. Apatites from strongly oxidised plutons tend to have higher concentrations of LREE relative to MREE. Manganese concentrations are higher in apatite from reduced granitoids because Mn2+substitutes directly for Ca2+. The La/Ce ratio of apatite is well‐correlated with the whole‐rock K2O and Na2O contents, as well as with the oxidation state and ASI. Because apatite trace‐element composition reflects the chemistry of the whole rock, it can be a useful indicator mineral for the recognition of mineralised granite suites, where particular mineralisation styles are associated with granitoids that have specific geochemical fingerprints. 相似文献
218.
Qingli Dai 《国际地质力学数值与分析法杂志》2010,34(13):1321-1345
This paper presents parallel and serial viscoelasto‐plastic models to simulate the rate‐independent and the rate‐dependent permanent deformation of stone‐based materials, respectively. The generalized Maxwell viscoelastic and Chaboche's plastic models were employed to formulate the proposed parallel and serial viscoelasto‐plastic constitutive laws. The finite element (FE) implementation of the parallel model used a displacement‐based incremental formulation for the viscoelastic part and an elastic predictor—plastic corrector scheme for the elastoplastic component. The FE framework of the serial viscoelasto‐plastic model employed a viscoelastic predictor—plastic corrector algorithm. The stone‐based materials are consisted of irregular aggregates, matrix and air voids. This study used asphalt mixtures as an example. A digital sample was generated with imaging analysis from an optically scanned surface image of an asphalt mixture specimen. The modeling scheme employed continuum elements to mesh the effective matrix, and rigid bodies for aggregates. The ABAQUS user material subroutines defined with the proposed viscoelasto‐plastic matrix models were employed. The micromechanical FE simulations were conducted on the digital mixture sample with the viscoelasto‐plastic matrix models. The simulation results showed that the serial viscoelasto‐plastic matrix model generated more permanent deformation than the parallel one by using the identical material parameters and displacement loadings. The effect of loading rates on the material viscoelastic and viscoelasto‐plastic mixture behaviors was investigated. Permanent deformations under cyclic loadings were determined with FE simulations. The comparison studies showed that the simulation results correctly predicted the rate‐independent and rate‐dependent viscoelasto‐plastic constitutive properties of the proposed matrix models. Overall, these studies indicated that the developed micromechanical FE models have the abilities to predict the global viscoelasto‐plastic behaviors of the stone‐based materials. Copyright © 2009 John Wiley & Sons, Ltd. 相似文献
219.
本文以西北一个铀矿床为例,介绍了一种进行矿床断裂构造地球化学研究的方法,包括了以断裂构造的倾角和倾向为座标的微量元素含量的等值线圆形曲线图;断裂构造的元素频数分布图;断裂构造中元素的多元统计分析。据此,讨论了热液作用和其它地质作用有关的断裂构造中微量元素的相互关系,并进而讨论了它们的铀成矿作用过程以及对找矿勘探的意义。 相似文献
220.
Chai Sheli 《吉林大学学报(地球科学版)》1989,(3)
本文从地质地球化学角度对峪耳崖金矿床进行了详细研究,认为该金矿是典型的岩浆热浪型脉状金矿床,金矿与峪耳崖花岗岩(即矿床的主要围岩)为同源岩浆作用的产物,而其源岩物质可能来自深部地壳。黄铁矿中Co/Ni比为1.58,石英中La/Yb比为2.95,δ~(34)S_∑为+2.6‰,δ~(13)O水为+7.03‰,δD为-88.4‰,δ~(13)C为-4.18‰,成矿温度为305~343℃,pH为6.2~6.8,石英包裹体成分中Cl~->F~-、Na~+>K~+,金可能是以Na[AuCl_2],Na[Aucl_4]或Na[AuS]等络合物形式迁移。 相似文献