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971.
972.
The focus of this study is a suite of garnet-bearing mantlexenoliths from Oahu, Hawaii. Clinopyroxene, olivine, and garnetconstitute the bulk of the xenoliths, and orthopyroxene is presentin small amounts. Clinopyroxene has exsolved orthopyroxene,spinel, and garnet. Many xenoliths also contain spinel-coredgarnets. Olivine, clinopyroxene, and garnet are in major elementchemical equilibrium with each other; large, discrete orthopyroxenedoes not appear to be in major-element chemical equilibriumwith the other minerals. Multiple compositions of orthopyroxeneoccur in individual xenoliths. The new data do not support theexisting hypothesis that all the xenoliths formed at 1 6–22GPa, and that the spinel-cored garnets formed as a consequenceof almost isobaric subsolidus cooling of a spinel-bearing assemblage.The lack of olivine or pyroxenes in the spinel–garnetreaction zones and the embayed outline of spinel grains insidegarnet suggest that the spinel-cored garnets grew in the presenceof a melt. The origin of these xenoliths is interpreted on thebasis of liquidus phase relations in the tholeiitic and slightlysilica-poor portion of the CaO–MgO–Al2O3–SiO2(CMAS) system at pressures from 30 to 50 GPa. The phase relationssuggest crystallization from slightly silica-poor melts (ortransitional basaltic melts) in the depth range 110–150km beneath Oahu. This depth estimate puts the formation of thesexenoliths in the asthenosphere. On the basis of this study itis proposed that the pyroxenite xenoliths are high-pressurecumulates related to polybaric magma fractionation in the asthenosphere,thus making Oahu the only locality among the oceanic regionswhere such deep magmatic fractional crystallization processeshave been recognized. KEY WORDS: xenolith; asthenosphere; basalt; CMAS; cumulate; oceanic lithosphere; experimental petrology; mantle; geothermobarometry; magma chamber 相似文献
973.
Halil Murat Algin 《国际地质力学数值与分析法杂志》2000,24(8):681-692
This paper presents a general algebraical formula to determine the vertical stresses resulting from a linearly distributed surface pressure resting on an elastic medium. This problem and its various derivations has received considerable attention because of its applications in foundation engineering [1–5]. The equation presented in this paper has been determined by the integration of the Boussinesq [6] equation with respect to the general surface function of a linearly distributed loading regime. The equation can be applied to the case of an optimally designed rectangular footing subjected to biaxial bending. Unlike the current design formulae [1–7], it provides the flexibility of having various contact pressures at each of the four corners of the rectangular area. This may enable more accurate design procedures for pad foundations in the future. This paper explains the validity of the new formula by comparing its results with those produced by classical methods. It shows how it can be applied to determine the vertical stress distributions resulting from all types of linearly distributed surface pressures which occupy a rectangular area on an elastic mass. Copyright © 2000 John Wiley & Sons, Ltd. 相似文献
974.
In geotechnical engineering designs and safety checks, the number of cycles of repeated loading N is frequently used as a parameter for calculating the response of soil structures under the repeated loading. However, there appears to be a lack of rational methods for calculating N for repeated loadings along general stress paths. A new method for defining N is proposed in this paper, based on the assumption that a yield surface may be identified for the material. It is demonstrated that the proposed method provides a rational and useful means for engineering calculation of soil deformations under repeated loadings. Copyright © 2001 John Wiley & Sons, Ltd. 相似文献
975.
976.
Analytical methods for the axial responses of piles can be classified under three broad categories of (1) simple but approximate analytical solutions, (2) one-dimensional numerical algorithms, (3) full axisymmetric analyses using boundary or finite element approaches. The first two categories rely on the so-called load transfer approach, with interaction between pile and soil determined by independent springs distributed along the pile shaft and at the pile base. The non-linear spring stiffness is related to the elastic–plastic properties of the actual soil partly by empirically based correlations and partly by theoretical arguments based on simplified models of the pile–soil system. This paper presents new closed-form solutions for the axial response of piles in elastic–plastic, non-homogeneous, media. The solutions fall in the first of the three categories above, and have been verified through extensive parametric studies using more rigorous one-dimensional and continuum analyses. The effect of non-homogeneity and partial slip on the load and displacement profiles along the pile shaft is explored, and comparisons are presented with experimental data. © 1997 John Wiley & Sons, Ltd. 相似文献
977.
地图切片技术分析与简单实现 总被引:8,自引:0,他引:8
地图切片(MapTile)技术是目前大多数电子地图网站、3维地图网站使用的预先生成栅格地图,并由客户端接口呈现出无缝拼接地图的浏览技术。地图以链接图片的方式快速定位,访问速度要快于传统的WebGIS,同时,对地图服务器的负载也相应小一些。本文介绍了地图切片技术的相关步骤并对主流电子地图网站做了分析。笔者利用Flash作为地图客户端开发工具,实现了地图切片的实时加载和不同比例尺的漫游。 相似文献
978.
979.
非饱和黏土的结构性能够显著影响其力学特性。基于非饱和土经典模型BBM(Barcelona basic model)和一种可描述循环塑性的硬化法则,引入体积破损率的作为标准土体结构破损的参数,建立了一个描述常吸力下非饱和结构性黏土静态及动态力学特性的弹塑性双面模型。模型在应力空间中包含与重塑非饱和土屈服面几何相似的结构性边界面和加载面,采用径向映射法则和可移动的记忆中心原理,通过结构性边界面和加载面在应力空间中的演化来反映循环加载过程中非饱和结构性黏土的循环塑性特征和结构损伤过程。通过与相关非饱和黏土控制吸力试验数据的比较,表明该模型能够较好地反映静态加载下非饱和结构性黏土的力学特性,而模型预测的循环荷载下的应力?应变特征也具有一定的合理性。 相似文献
980.
利用霍布金森压杆试验装置对灰砂岩试样进行预加静载的循环冲击,使试样产生初始损伤,并分析此过程中试样的损伤演化规律。使用能够施加轴压的霍布金森压杆进行预损伤试样动静组合加载试验,获得试样破坏模式、动态应力-应变关系等指标。基于应变等价原理分析预损伤试样动静组合加载条件下的总损伤变量,建立相应的损伤演化方程及损伤本构关系,并与完整试样进行对比。研究结果表明:循环冲击过程中试样损伤变量分为快速上升、低速发展、高速发展3个阶段,预加轴压越大低速发展阶段损伤变量平均值越小;相同动静组合加载条件下预损伤试样动态强度较小,完整试样应变率增强效应更加显著;循环冲击预损伤变量 、预加静载损伤变量 对于应力-应变关系的影响是较为复杂的, 、 值之和可能为负值;建立的本构关系与试验曲线具有较好的一致性,得到的总损伤变量曲线不仅能够解释试样宏观破坏与细观损伤过程的一致性,并且能够反映循环冲击和预加静载两种因素对岩石总损伤发展的非线性影响。 相似文献