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981.
982.
本论文对交城花岗岩体的地质环境、工程力学和理化特征作了初步研究。认为交城岗花岩体的地质构造稳定、水文地质条件良好,岩性均匀,故选择交城花岗岩作为研究主岩,并对典型核素在填隙物和花岗岩上的吸附性能进行了试验。 相似文献
983.
湘中断裂体系分维与锑矿分布 总被引:18,自引:3,他引:15
笔者将分形几何学的原理和方法,应用于湘中地区断裂体系的二维平面分布特征研究,发现在研究的标度范围内(r约2~80km)不仅具有统计自相似性,并且同一地区,不同分区具有不同的分维值D,分维值分布特征为东南区分维值高于西北区分维值,将本区断裂体系的这种分维值分布特征与锑矿床分布特征对比,可发现锑矿床(点)产出较多,矿床规模较大的地区,其分维值较大。 相似文献
984.
P. Goovaerts 《Mathematical Geology》1998,30(5):511-534
This paper presents both estimation and simulation as optimization problems that differ in the optimization criteria, minimization of a local expected loss for estimation and reproduction of global statistics (semivariogram, histogram) for simulation. An intermediate approach is proposed whereby an initial random image is gradually modified using simulated annealing so as to better match both local and global constraints. The relative weights of the different constraints in the objective function allow the user to strike a balance between smoothness of the estimated map and reproduction of spatial variability by simulated maps. The procedure is illustrated using a synthetic dataset. The proposed approach is shown to enhance the influence of observations on neighboring simulated values, hence the final realizations appear to be better conditioned to the sample information. It also produces maps that are more accurate (smaller prediction error) than stochastic simulation ignoring local constraints, but not as accurate as E-type estimation. Flow simulation results show that accounting for local constraints yields, on average, smaller errors in production forecast than a smooth estimated map or a simulated map that reproduces only the histogram and semivariogram. The approach thus reduces the risk associated with the use of a single realization for forecasting and planning. 相似文献
985.
青藏高原积雪分布与变化特征 总被引:45,自引:1,他引:44
本文对青藏高原SMMR修积雪深度、NOAA周积雪面积、地面台站积雪深度进行了分析。结果表明青藏高原东西两侧多雪与腹地少雪形成鲜明对比,高原东部是高原积雪年际变化最显著的地区,它主导了整个高原积雪的年际变化,并且与西部多雪区年际波动呈反位相关系。从60年代到80年代积雪年际波动幅度有明显增加趋势,积雪变化具有3年左右准周期。随着全球变暖,青藏高原积雪将会有所增加。 相似文献
986.
黄河故道的环境特征与整体开发 总被引:4,自引:0,他引:4
从区域开发的角度,对黄河故道的形成发展与环境的关系进行了分析,提出了开发构想,为黄河故道生态农业的开发提供依据。 相似文献
987.
在分析区域地震活动和构造环境及利用GDSN的宽频带波形资料分析震源破裂特征的基础上,结合余震资料,讨论了1988~1990年发生在四川和青海的9次强震的震源破裂和余震分布特征,分析了四川、青海、西藏相邻区域内的地震能量迁移,并用单键群分析方法对1970年以来的地震活动总体图象进行了研究。结果表明,这些地震的震源性质与构造应力环境相符,但青海地震的震源都具有较大的逆掩分量,与过去的走滑震源性质不同,而四川地震的震源P轴不接近水平方向与当地的“Y”字形复杂构造有关 相似文献
988.
Kai-Wu Li 《地震学报(英文版)》1998,11(5):637-644
Studies by many scientists show that Hebei, China is an area with strong correlation between the tidal force and the occurrences
of major earthquakes, the Xingtai earthquake of 1966, the Hejian earthquake of 1967 and the Tangshan earthquake of 1976 were
triggered by the tidal force, in this paper the study on the common characteristics of their occurrence times confirms these
facts. The computed times of maximum horizontal of the semi diurnal solid tide tidal force show that the occurrence times
of the above mentioned earthquakes were close to the times of maximum horizontal tidal force of the semi diurnal solid tide
at new moon or full moon. The Longyao earthquake of M=6.8, the Ningjin earthquake of M=7.2 and the Hejian earthquake of M=6.3 occurred tens of minutes after the maximum horizontal tidal force of the semi diurnal solid tides, and the Tangshan earthquake
of M=7.8 occurred 16 minutes before the maximum horizontal tidal force. The tidal forces were directed to the west. This is their
temporal characteristic. It is generally accepted that the 1969 Bohai earthquake of M=7.4 and the 1975 Haicheng earthquake were not triggered by the tidal force. These events did not show such characteristics.
The temporal characteristics of the earthquakes indicate that the occurrences of these events were not random, but were controlled
by the tidal force from the sun and the moon, and triggered by the tidal force. These facts agree with the triggering mechanism
of the tidal force, are evidences of earthquakes triggered by tidal force. 相似文献
989.
A nonlinear magnitude frequency equation has been derived in this paper on the assumption that all seismicity systems hold
fractal characteristics, and according to the differences of relevant coefficients in the equation, seismicity systems are
classified into two types: type I, the whole earthquake activity is controlled by only one great unified system; type II,
the whole earthquake activity is controlled by more than one great system. One type of seismicity system may convert to the
other type, generally. For example, a type I system will change to a type II system prior to the occurrence of a strong earthquake
in North China. This change can be regarded as an index for earthquake trend estimation. In addition, the difference between
b value in nonlinear magnitude frequency equation and that in linear equation and the term dΔM related to the coefficients of nonlinear terms obtained in this paper are proved to be a pair of available parameters for
medium short term earthquake prediction. 相似文献
990.