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81.
A. A. Nikonov 《Natural Hazards》1992,6(1):1-10
This paper relates some facts about abnormal animal behaviour prior to several Armenian earthquakes. The catastrophic Spitak, northern Armenia, earthquake of 7 December 1988, M = 7, I
0 = X, was preceded by extensive occurrences of abnormal animal behaviour. Proof was established by questioning residents in the area and by distributing specially prepared questionnaires shortly after the event. Approximately 200 reports from 50 sites were examined. The raw data recorded included lists of different types and locations of species that have shown abnormal responses to an impending earthquake, distribution of anomalous occurrences over the area, and precursor times. It is concluded that specially conducted observations of animal behaviour as a possible premonitory phenomenon is both useful and necessary. 相似文献
82.
利用福建水氡台网 1 990年以来的水氡资料 ,针对 6次福建及其东南沿海大于 4 5级地震 ,7次台湾及其近海大于 6 8级地震进行分析研究 ,认为地震前异常存在加速性、同步性 ,形态的多样性 ,空间分布的不确定性。运用“九五”攻关软件 ,给出上述两区域地震异常特征的共性和个性 ,并对映震效能进行R值评分 相似文献
83.
本文对近期乌鸦咀泉异常进行宏观和微观分析 ,通过对此次异常和以往异常进行对比分析 ,以及对不同位置水样进行对比观测 ,指出该异常由下水道污水引起 ,且此次污染源同以往不同 ,进而对今后的工作提出几个建设性意见。 相似文献
84.
85.
86.
Four types of disturbances in the seasonal variation in georesistivity are presented in the light of specific circumstances
in China. As the results of theoretic calculation for the models and in comparison of the calculated results with the seasonal
variations observed at 40 georesistivity stations, the following points are found: (1) The seasonal variation in georesistivity
is caused by the change in resistivity of the surface layer, especially by the annual variation of phreatic level when the
sounding depth is too shallow. This is one of the disturbances and thus has no relation to the origin of earthquake. The feature
and amplitude of the seasonal variation depend on the types of disturbance models, geoelectric cross sections and sounding
depth. (2) The seasonal variation in georesistivity usually has the same sign as that of the change in resistivity of shallow
layer and thus the normal seasonal change appears. However, as far as the K or Q types of geoelectric cross sections are concerned,
the abnormal seasonal variation in georesistivity starts to appear with a certain electrode spacing, when the interference
layer is located in the first layer. (3) Both abnormal and normal seasonal variations in georesistivity will be smaller than
2% when the sounding depth is greater than 300 m. Therefore, the seasonal variations can be removed or restrained when the
location of observation has been properly chosen or the electrode spacing is enlarged enough to obtain a sufficient sounding
depth. 相似文献
87.
88.
Grain growth experiments in dunite, clinopyroxenite, and wehrlites with various forsterite/diopside ratios were performed to investigate the effect of modal composition on grain growth kinetics in the Earth's uppermost mantle. The experiments were conducted using a piston-cylinder apparatus at 1200 °C and 1.2 GPa for 2-763 h under dry conditions. Normal grain growth (NGG) occurred in dunite, clinopyroxenite, and relatively forsterite-poor wehrlites (≤70 vol.% of forsterite). Grain growth rates of forsterite and diopside in relatively forsterite-poor wehrlites were much slower than those in dunite and clinopyroxenite. In the forsterite-rich wehrlites (≥80 vol.% of forsterite), NGG of diopside and abnormal grain growth (AGG) of forsterite occurred. The growth rate of diopside was significantly slower than that in clinopyroxenite, while the growth rate of forsterite by AGG was found to be similar to that by NGG in dunite. The presence of ≤20 vol.% diopside had the effect of inhibiting the forsterite grain growth during the initial stage, resulting in AGG of forsterite, thus overtaking the growth rate in dunite. Our experimental results suggest that there would be a significant difference in grain growth rate and consequently in effective viscosity between olivine-rich peridotites (depleted mantle) and relatively olivine-poor peridotites (fertile mantle) in the case of grain size-sensitive creep. Variation of mean grain sizes in the upper mantle would result not only from differences in temperature and phase assemblage, but also from the variation of modal compositions. 相似文献
89.
90.
Two great earthquakes occurred in the sea northwest of Sumatra, Indonesia, on December 26, 2004 and March 29,2005. The observation of water levels in Yunnan yielded abundant information about the two earthquakes. This paper presents the water level response to the two earthquakes in Yunnan and makes a preliminary analysis. It is observed that the large earthquake- induced abnormal water level change could be better recorded by analog recording than by digital recording. The large earthquake-caused water level rise or decline may be attributed to the effect of seismic waves that change the stress in tectonic units, and is correlated with the geological structure where the well is located. The water level response mode in a well is totally the same for earthquakes occurring on the same fault and with the same fracture mode. The only difference is that the response amplitude increases with the growth of the earthquake magnitude. 相似文献