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901.
伽师强震群地震动特点与震源机制关系的研究 总被引:5,自引:0,他引:5
1997年1至4月,新疆维吾尔自治区伽师县境内发生了7次6级以上强震群。在此期间布设了由4个临时台站组成的地面加速度观测台网,共得到6级以上强震记录57条。本文给出这次强震群的烈度分布图和震源机制,研究了这批强震记录的相关谱特性及其与震源机制的关系。此外,还研究了这些地震的地震动与宏观烈度的对应关系以及地震动随震中距的衰减曲线。 相似文献
902.
An M=6.0 earthquake occurred on February 23, 2001 in the western Sichuan Province, China. The macro seismic epicenter situated
in the high mountain-narrow valley region between Yajiang and Kangding counties. According to field investigation in the region,
the intensity of epicentral area reached VIII and the areas with intensity VIII, VII and VI are 180 km2, 1 472 km2 and 3 998 km2, respectively. The isoseismals are generally in elliptic shape with major axis trending near N-S direction. The earthquake
destroyed many buildings and produced some phenomena of ground failure and mountainous disasters in the area with intensity
VIII. This event may be resulted from long-term activities of the Litang fault and Yunongxi fault, two main faults in the
western Sichuan. The movements between the main faults made the crust stress adjusted and concentrated, and finally the earthquake
on a secondary fault in the block released a quite large energy. 相似文献
903.
The 1927 earthquake was the strongestseismic event (M = 6.2) of the 20th centuryin the Holy Land and the first significantone in the region to be recorded worldwideby seismometers. By quoting theseismological station in Ksara, the ISSlocated the epicenter 40 km north of theDead Sea. This location, which wassupported by secondary and tertiarymacroseismic `evidence' and became one ofthe most accepted `facts', was neverquestioned nor reevaluated.We show how an initial mistaken earthquakelocation, supported by questionableevidence, struck roots and eventually becamean accepted fact. This typical `chain oferrors' may serve as a warning regardingtreatment of historical macroseismicsources, as well as historical microseismicdocuments. The conclusions drawn from thisstudy, while focusing on historicaldocumentation, fit well the new epicenterof the 1927 earthquake, recalculated in ourformer study. 相似文献
904.
905.
花岗岩动三轴抗压强度的裂纹模型研究(I):理论基础 总被引:3,自引:0,他引:3
简要地介绍了岩石材料在压应力作用下的裂纹模型。应用虚拟力方法(Pseudo-tractionmethod)考虑2阶虚拟力情形,求解裂纹组应力强度因子表达式,为岩石动三轴抗压强度的裂纹模型研究提供理论基础。 相似文献
906.
907.
908.
LIU Jiyuan LIU Mingliang DENG Xiangzheng Zhuang Dafang ZHANG Zengxiang LUO Di 《地理学报》2002,12(3):275-282
In the mid-1990s, we established the national operative dynamic information serving systems on natural resources and environment. During building the land-use/land-cover change (LUCC) database for the mid-1990s, 520 scenes of remotely sensed images of Landsat Thematic Mapper (TM) were interpreted into land-use/land-cover categories at scale of 1:100,000 under overall digital software environment after being geo-referenced and ortho-rectified. The vector map of land-use/land-cover in China at the scale of 1:100,000 was recently converted into a 1-km raster database that captures all of the high-resolution land-use information by calculating area percentage for each kind of land use category within every cell. Being designed as an operative dynamic information serving system, monitoring the change in land-use/land-cover at national level was executed. We have completed the updating of LUCC database by comparing the TM data in the mid-1990s with new data sources received during 1999-2000 and 1989-1990. The LUCC database has supported greatly the national LUCC research program in China and some relative studies are incompletely reviewed in this paper. 相似文献
909.
岩石边坡裂隙渗流的流形元模拟 总被引:1,自引:0,他引:1
为了能够更好地考虑裂隙渗流在岩石边坡破坏中的作用,在考虑裂纹扩展的数值流形方法程序基础上,从最小势能原理出发,阐述了渗流与变形的耦合作用机理并推导了相应的耦合方程,在程序中实现了对渗流与断裂的模拟。最后利用该程序对含初始裂隙的岩石边坡在渗流作用下的破坏过程进行了模拟。模拟结果很好地再现了边坡在渗流作用下的实际破坏过程。同时通过对裂纹扩展过程中应力强度因子的计算发现,第一应力强度因子始终大于第二应力强度因子,且随着计算时间增加,二者的差值逐渐增大,裂纹扩展以Ⅰ型为主。 相似文献
910.