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991.
新疆库车坳陷逆掩断裂在油气运聚中的作用 总被引:4,自引:0,他引:4
在研究新疆库车坳陷逆掩断裂、源岩和盖层空间发育特征的基础上,研究了逆掩断裂与源岩、盖层的空间匹配关系.认为断穿源岩、盖层的逆掩断裂则是油气散失的通道;勾通源岩,但未断穿盖层的逆掩断裂则是油气聚集的输导通道,它们控制着库车坳陷油气的聚散及其在空间上的分布.在研究库车坳陷逆掩断裂活动史和源岩排烃史、盖层封闭能力形成史的基础上,研究了逆掩断裂与源岩、盖层的时间匹配关系,认为盖层与源岩的时间匹配关系控制着可供运移的油气量;逆掩断裂与源岩的时间匹配关系控制着可供聚集的油气量,盖层与逆掩断裂的时间匹配关系控制着油气的富集量. 相似文献
992.
P. S. Negi 《Monthly notices of the Royal Astronomical Society》2008,388(3):1161-1170
We show that the mass–radius ( M – R ) relation corresponding to the stiffest equation of state (EOS) does not provide the necessary and sufficient condition of dynamical stability for equilibrium configurations, because such configurations cannot satisfy the 'compatibility criterion'. In this regard, we construct sequences composed of core–envelope models such that, like the central condition belonging to the stiffest EOS, each member of these sequences satisfies the extreme case of the causality condition, v = c = 1 , at the centre. We thereafter show that the M – R relation corresponding to the said core–envelope model sequences can provide the necessary and sufficient condition of dynamical stability only when the 'compatibility criterion' for these sequences is 'appropriately' satisfied. However, the 'compatibility criterion' can remain satisfied even when the M – R relation does not provide the necessary and sufficient condition of dynamical stability for the equilibrium configurations. In continuation of the results of a previous study, these results explicitly show that the 'compatibility criterion' independently provides, in general, the necessary and sufficient condition of hydrostatic equilibrium for any regular sequence. In addition to its fundamental result, this study can explain simultaneously the higher and the lower values of the glitch healing parameter observed for the Crab-like and Vela-like pulsars respectively, on the basis of the starquake model of glitch generation. 相似文献
993.
I. C. Kroon B.-L. Nguyen P. A. Fokker A. G. Muntendam-Bos G. de Lange 《Mathematical Geosciences》2009,41(5):571-584
Understanding and predicting surface movement is important both technically and for social reasons. The shallow processes
contributing to subsidence include construction works, peat oxidation, clay compaction, and groundwater withdrawal; deep causes
are hydrocarbon and salt production. We describe an inversion procedure we have devised to disentangle the deep and shallow
causes of surface movement. It employs a Bayesian inversion scheme, using forward models and other ‘a priori’ information
about shallow and deep compaction. Parameter estimation thus takes place at two different depths, thereby disentangling the
deep and shallow compaction processes responsible for surface movement. The uncertainty in the surface measurements and ‘a
priori’ estimates is naturally incorporated. Furthermore, spatial and temporal correlations can be taken into account through
inclusion of the covariance matrix. The inversion scheme is demonstrated for two synthetic cases. The first combines a compacting
gas field and a compacting shallow peat layer. We demonstrate that assumptions on the shape of the subsidence bowl are not
necessary. We also show how neglecting either deep or shallow causes of subsidence can produce spurious results. The advantage
of using the ‘a priori’ estimates of the compaction and the covariance matrix obtained by Monte Carlo simulations is demonstrated
with a second synthetic example involving two polders and different depths of their water table. A robust solution is obtained
for each polder unit, while a simpler (and faster) ‘a priori’ estimate based on the expected average clay thickness fails
to reproduce the actual compaction. Monte Carlo simulations can also be applied to compaction in depleting gas reservoirs.
Information on spatial correlations is often available, even when the absolute values of the ‘a priori’ compaction data are
quite uncertain. Explicitly incorporating such ‘a priori’ known spatial correlations improves the result significantly. 相似文献
994.
A Blocking Markov Chain Monte Carlo Method for Inverse Stochastic Hydrogeological Modeling 总被引:3,自引:2,他引:1
An adequate representation of the detailed spatial variation of subsurface parameters for underground flow and mass transport
simulation entails heterogeneous models. Uncertainty characterization generally calls for a Monte Carlo analysis of many equally
likely realizations that honor both direct information (e.g., conductivity data) and information about the state of the system
(e.g., piezometric head or concentration data). Thus, the problems faced is how to generate multiple realizations conditioned
to parameter data, and inverse-conditioned to dependent state data. We propose using Markov chain Monte Carlo approach (MCMC)
with block updating and combined with upscaling to achieve this purpose. Our proposal presents an alternative block updating
scheme that permits the application of MCMC to inverse stochastic simulation of heterogeneous fields and incorporates upscaling
in a multi-grid approach to speed up the generation of the realizations. The main advantage of MCMC, compared to other methods
capable of generating inverse-conditioned realizations (such as the self-calibrating or the pilot point methods), is that
it does not require the solution of a complex optimization inverse problem, although it requires the solution of the direct
problem many times. 相似文献
995.
996.
基于小波变换的分层影像匹配 总被引:6,自引:0,他引:6
提出一种小波变换支持的基于灰度和基于特征相结合的分层匹配方案用于DEM自动生成,利用航空与航天影像(MOMS-02,SPOT)进行的试验表明,该方案具有基于灰度、基于特征和分层影像匹配的优点,能以较少的代价获得高精度、高可靠性的匹配结果. 相似文献
997.
998.
999.
1000.
地形起伏对雷达景象实际匹配影响初探 总被引:1,自引:0,他引:1
雷达景象匹配由于具有全天候的特征,在飞行器导航与定位中受到重视,但因为地形起伏影响,实际地物在雷达景象上的成像会发生变形与移位,这将影响实时雷达景象与参考基准图匹配的精度。根据实时雷达景象的成像方式,利用参考基准图模拟出地面平坦条件下的模拟雷达图一;并利用DEM数据,采用纠正方法,在该模拟雷达图上引入地面起伏因素的影响,得到地面起伏情况下的实际成像——模拟雷达图二。试验中,将同一地区的两类模拟雷达实时图分别与参考基准图影像进行匹配,比较匹配的结果,针对其匹配差异分析地面起伏对雷达景象匹配的实际影响,最后得出结论——实际地面在雷达图上的成像特征是影响匹配的最主要因素,地形起伏对匹配的影响与地面特征的分布有关,只有起伏区域存在明显地物特征时才会对匹配产生影响。 相似文献