全文获取类型
收费全文 | 5143篇 |
免费 | 1010篇 |
国内免费 | 1316篇 |
专业分类
测绘学 | 330篇 |
大气科学 | 1193篇 |
地球物理 | 1240篇 |
地质学 | 2801篇 |
海洋学 | 531篇 |
天文学 | 197篇 |
综合类 | 496篇 |
自然地理 | 681篇 |
出版年
2024年 | 17篇 |
2023年 | 69篇 |
2022年 | 251篇 |
2021年 | 302篇 |
2020年 | 207篇 |
2019年 | 282篇 |
2018年 | 346篇 |
2017年 | 308篇 |
2016年 | 314篇 |
2015年 | 266篇 |
2014年 | 299篇 |
2013年 | 280篇 |
2012年 | 301篇 |
2011年 | 346篇 |
2010年 | 336篇 |
2009年 | 284篇 |
2008年 | 220篇 |
2007年 | 249篇 |
2006年 | 233篇 |
2005年 | 197篇 |
2004年 | 133篇 |
2003年 | 124篇 |
2002年 | 151篇 |
2001年 | 129篇 |
2000年 | 167篇 |
1999年 | 238篇 |
1998年 | 161篇 |
1997年 | 183篇 |
1996年 | 167篇 |
1995年 | 164篇 |
1994年 | 133篇 |
1993年 | 166篇 |
1992年 | 100篇 |
1991年 | 78篇 |
1990年 | 56篇 |
1989年 | 49篇 |
1988年 | 41篇 |
1987年 | 33篇 |
1986年 | 20篇 |
1985年 | 14篇 |
1984年 | 5篇 |
1983年 | 8篇 |
1982年 | 12篇 |
1981年 | 3篇 |
1980年 | 4篇 |
1979年 | 4篇 |
1963年 | 1篇 |
1958年 | 14篇 |
1954年 | 1篇 |
1947年 | 1篇 |
排序方式: 共有7469条查询结果,搜索用时 298 毫秒
441.
Land use change in Bohai Rim: a spatial-temporal analysis 总被引:5,自引:0,他引:5
Land use change is one of the important aspects of global change[1-3]. The Bohai Rim is a hot spot of economic development in China, where land use changes remarkably. Analyzing land use change in this area is significant to the research of global change and regional sustainable land use. Although there has been much work undertaken on regional land use change in China, it was mainly on urban land use change[4-11], and few researches integrated remote sensing and GIS method. Based on data f… 相似文献
442.
— Using P and S arrival times, which occurred within the Huabei seismic network, we carried out a tomographic inversion and compared results with the earthquake catalogue of the last 1000?years in the area. The results are as follows:¶1) The hypocenters of most of the strong shocks are distributed in the transitional zones between high- and low-velocity areas in the crust, especially at edges of high-velocity blocks.¶2) Strong shocks predominantly lie above low-velocity blocks, or in transitional zones between low- and high-velocity areas, in the lower crust.¶3) The tectonic settings for the Tangshan and the Sanhe-Pingu earthquakes are similar. Both are not known near large fault belts, and in zones with a sharp lateral velocity gradient.¶4) The Ninghe, Tangshan and Luanxia earthquakes are located in high-velocity blocks that differ in size and depth. This difference can explain the focal depth distribution of the Tangshan earthquake sequence, i.e., earthquakes are shallower in the northeastern Luanxian area but deeper in the southwestern Ninghe area. 相似文献
443.
In our work,ocean ridge granite,i.e., Oytan plagiogranite massif,was discovered in western Qinghai-Xizang plateau.It intruded into the basic lava of the Oytag ophiolite suite and it was formed a little later than the (ultra)mafic rocks of the Oytag ophiolite suite.The Oytang plagiogranite possesses the geochemical characteristics of mantle-source granite and was formed in the “supre-subduction zone”(SSZ)ocean ridge environment,like the ocean ridge granite of Troodos,Cypus. 相似文献
444.
445.
446.
对云龙台的水管倾斜仪观测数据进行了倾斜固体潮的潮汐分析,发现EW和NS两个分量的振幅因子异常变化与地震有较好的对应关系。由于潮汐分析方法本身的科学性和严密性,故振幅因子误差小、精度高;又因为对潮汐谐波波群的选择,避免了以太阳日为基础的周期性干扰,M2、O1波振幅因子的地震异常识别则简易可行,并且可信度高。云龙台的固体潮观测具有较强的地震监测能力。 相似文献
447.
Based on the long period surface wave data recorded by the China Digital Seismograph Network (CDSN), theQ
R
of fundamental mode Rayleigh wave with periods from 10 s to 146 s is determined for the eastern Sino-Korean paraplatform
in this paper. TheQ
β
models of the crust and upper mantle are respectively obtained for the 4 paths, with the aid of stochastic inverse method.
It shows that in the eastern Sino-Korean paraplatform, the average crustalQ
β
is about 200, and that there exists a weak attenuation layer in the middle crust (about 10–20 km deep) which is possibly
related to earthquake-prone layer. A strong attenuation layer (lowQ) of 70 km thick extensively exists in the uppermost mantle, with the buried depth about 80 km. The averageQ
R
of fundamental mode Rayleigh wave is between the value of stable tectonic region and that of active tectonic region, and
much close to the latter.
Contribution No. 96A0001, Institute of Geophysics, SSB, China.
Funded by the Chinese Joint Seismological Science Foundation. 相似文献
448.
Aseismio fault slip and block deformation in North China 总被引:1,自引:0,他引:1
Lanbo Liu Alan T. Linde I. Selwyn Sacks Shihai He 《Pure and Applied Geophysics》1996,146(3-4):717-740
In North China, the tectonic fault-block system enables us to use the Discontinuous Deformation Analysis (DDA) method to simulate the long-term cross-fault survey and other geodetic data related to aseismic tectonic deformation. By the simulation we have found that: (1) Slips on faults with different orientation are generally in agreement with the ENE-WSW tectonic stress field, but the slip pattern of faulting can vary from nearly orthogonal, to pure shear along the strike of the faults, this pattern cannot be explained by simple geometric relation between the strike of the fault and the direction of the tectonic shortening. This phenomenon has been observed at many sites of cross-fault geodetic surveys, and might be caused by the interactions between different blocks and faults. (2) According to the DDA model, if the average aseismic slip rate along major active faults is at the order of several tenths of millimeter per year as observed by the cross-fault geodetic surveys, the typical strain rate inside a block is at the order of 10–8 year–1 or less, so that the rate of 10–6 year–1, as reported by observations in smaller areas, cannot be the representative deformation rate in this region. (3) Between the slips caused by regional compression and block rotation, there is a possibility that the sense of slip caused by rigid body rotation in two adjacent blocks is opposite to the slip caused by the tectonic compression. But the magnitude of slip resulting from the tectonic compression is much larger than that due to the block rotation. Thus, in general, the slip pattern on faults as a whole agrees with the sense of tectonic compression in this region. That is to say, the slip caused by regional compression dominates the entire slip budget. (4) Based on (3), some observed slips in contradiction to ENE tectonic stress field may be caused by more localized sources, and have no tectonic significance. 相似文献
449.
依据地震危险性分析的思路,提出一种场地震害预测的方法。依此方法,给出山东地区50a超越概率为10%的震害预测略图 相似文献
450.
CHARACTERISTICS OF MESOSCALE FLOOD-MAKING TORRENTIAL RAIN SYSTEM SIMULATED BY HIGH RESOLUTION LIMITED AREA MODEL—NUMERICAL SIMULATION OF A HEAVY RAIN PROCESS DURING MEIYU SEASON IN 1991*
下载免费PDF全文
![点击此处可从《Acta Meteorologica Sinica》网站下载免费的PDF全文](/ch/ext_images/free.gif)
An experimental work on the transplant of high resolution limited area model(HIRLAM) isfirstly introduced into China.For the implementation,first of all is to adjust a new geographicalcoordination and to remove the instability caused by the Tibetan Plateau,the roof of the world.Then,we have applied this model to simulate a flood-making torrential rain process which occurredin the Changjiang-Huaihe River Valley in July 1991.That revealed the formation,development andmovement of a mesoseale heavy rain system which had made a disastrous flood event in the middleand lower reaches of Changjiang River Valley.The result encourages us to use the HIRLAM for the researches on the Meiyu belt,the salientfeature of precipitation of East Asia,and the numerical prediction of heavy rains in China. 相似文献