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211.
212.
均衡理论,无论是艾礼模式,还是普拉特模式,都是建立在平面地壳的基础之上,并不考虑重力随高程的变化;这事实上相当于质量的均衡。如果在球面上考察均衡理论,并且考虑重力随高程的变化,则得到的均衡模型为重力的均衡。定量计算表明,质量均衡和重力均衡之间的差别是不可忽略的。这种差别对研究地壳的应力状态意义重大。 相似文献
213.
长江三峡工程坝址西南约10km的狮子口地区,发育一个长约8km、宽约3km的重力滑动构造系统。它由下伏系统、滑动系统和前缘推挤带构成,是一个典型的多层次滑褶型重力滑动构造。它形成时的温、压条件为130.5~193.7℃和180~230MPa;l;形成深度约5~10km;总体岩层收缩量32.2%;总滑移距离1060m;活动时间上限127.65士38.29万年。它是燕山运动期间南北向挤压体制下,在黄陵背斜东、西两侧应力屏蔽区内派生的近东西向拉伸构造应力场的产物。 相似文献
214.
215.
Wang Xingbao 《Acta Meteorologica Sinica》1995,9(4):488-500
Effects of topography on the propagation and development of inertia gravity waves areinvestigated by means of WKBJ method.The equation of wave action conservation is obtained.It isfound that the inertia gravity wave tends to propagate to the higher elevation area,meanwhile theamplitudes of the waves increase.While the inertia gravity waves propagate to a lower elevation area,their amplitudes decrease. 相似文献
216.
研究表明,康滇地轴及其东部地区属均衡补偿平衡区,西部属强烈上升的异常区。上升的原动力为板块碰撞的构造力与均衡调整力的综合。 相似文献
217.
局部重磁场源全方位成像理论概要(续) 总被引:4,自引:4,他引:0
作者近年来首创了"复杂条件下局部重磁场源全方位成像"理论体系。在本文中,概要阐述该理论体系中下延有限二度体复重磁场级数正演通式、复场模值全方位延拓和全方位反演等。 相似文献
218.
泾阳4.8级地震前后重力变化探析 总被引:2,自引:0,他引:2
系统分析了泾阳Ms4.8地震前后陕西关中地区流动重力观测资料,探讨了重力场的时空变化及其映震特征。结果表明:①震前在震中区附近形成较显著地重力负异常区,且与沉降区基本吻合。②泾阳地震震中区既是重力变化梯度带,也是重力异常的正值区到负值区的过度带。③由于震源区应力作用方式是以水平为主的左旋走滑运动,震前局部重力异常不显著。 相似文献
219.
Inference of mantle viscosity from GRACE and relative sea level data 总被引:12,自引:0,他引:12
Gravity Recovery And Climate Experiment (GRACE) satellite observations of secular changes in gravity near Hudson Bay, and geological measurements of relative sea level (RSL) changes over the last 10 000 yr in the same region, are used in a Monte Carlo inversion to infer-mantle viscosity structure. The GRACE secular change in gravity shows a significant positive anomaly over a broad region (>3000 km) near Hudson Bay with a maximum of ∼2.5 μGal yr−1 slightly west of Hudson Bay. The pattern of this anomaly is remarkably consistent with that predicted for postglacial rebound using the ICE-5G deglaciation history, strongly suggesting a postglacial rebound origin for the gravity change. We find that the GRACE and RSL data are insensitive to mantle viscosity below 1800 km depth, a conclusion similar to that from previous studies that used only RSL data. For a mantle with homogeneous viscosity, the GRACE and RSL data require a viscosity between 1.4 × 1021 and 2.3 × 1021 Pa s. An inversion for two mantle viscosity layers separated at a depth of 670 km, shows an ensemble of viscosity structures compatible with the data. While the lowest misfit occurs for upper- and lower-mantle viscosities of 5.3 × 1020 and 2.3 × 1021 Pa s, respectively, a weaker upper mantle may be compensated by a stronger lower mantle, such that there exist other models that also provide a reasonable fit to the data. We find that the GRACE and RSL data used in this study cannot resolve more than two layers in the upper 1800 km of the mantle. 相似文献
220.
A. M. Marotta R. Barzaghi A. Borghi E. Spelta 《Geophysical Journal International》2007,171(3):977-985
The thermomechanic evolution of the lithosphere–upper mantle system during Calabrian subduction is analysed using a 2-D finite element approach, in which the lithosphere is compositionally stratified into crust and mantle. Gravity and topography predictions are cross-checked with observed gravity and topography patterns of the Calabrian region. Modelling results indicate that the gravity pattern in the arc-trench region is shaped by the sinking of light material, belonging to both the overriding and subduction plates. The sinking of light crustal material, up to depths of the order of 100–150 km is the ultimate responsible for the peculiar gravity signature of subduction, characterized by a minimum of gravity anomaly located at the trench, bounded by two highs located on the overriding and subducting plates, with a variation in magnitude of the order of 200 mGal along a wavelength of 200 km, in agreement with the isostatically compensated component of gravity anomaly observed along a transect crossing the Calabrian Arc, from the Tyrrhenian to the Ionian Seas. The striking agreement between the geodetic retrieved profiles and the modelled ones in the trench region confirms the crucial role of compositional stratification of the lithosphere in the subduction process and the correctness of the kinematic hypotheses considered in our modelling, that the present-day configuration of crust–mantle system below the Calabrian arc results from trench's retreat at a rate of about 3 cm yr−1 , followed by gravitational sinking of the subducted slab in the last 5 Myr. 相似文献