全文获取类型
收费全文 | 10226篇 |
免费 | 2069篇 |
国内免费 | 3080篇 |
专业分类
测绘学 | 238篇 |
大气科学 | 426篇 |
地球物理 | 2244篇 |
地质学 | 10288篇 |
海洋学 | 705篇 |
天文学 | 56篇 |
综合类 | 464篇 |
自然地理 | 954篇 |
出版年
2024年 | 71篇 |
2023年 | 169篇 |
2022年 | 304篇 |
2021年 | 412篇 |
2020年 | 523篇 |
2019年 | 510篇 |
2018年 | 492篇 |
2017年 | 610篇 |
2016年 | 545篇 |
2015年 | 572篇 |
2014年 | 740篇 |
2013年 | 1018篇 |
2012年 | 838篇 |
2011年 | 667篇 |
2010年 | 516篇 |
2009年 | 655篇 |
2008年 | 616篇 |
2007年 | 654篇 |
2006年 | 696篇 |
2005年 | 528篇 |
2004年 | 583篇 |
2003年 | 494篇 |
2002年 | 467篇 |
2001年 | 392篇 |
2000年 | 434篇 |
1999年 | 342篇 |
1998年 | 253篇 |
1997年 | 278篇 |
1996年 | 230篇 |
1995年 | 202篇 |
1994年 | 147篇 |
1993年 | 107篇 |
1992年 | 84篇 |
1991年 | 52篇 |
1990年 | 47篇 |
1989年 | 36篇 |
1988年 | 29篇 |
1987年 | 16篇 |
1986年 | 14篇 |
1985年 | 5篇 |
1984年 | 4篇 |
1983年 | 3篇 |
1982年 | 2篇 |
1981年 | 2篇 |
1980年 | 1篇 |
1979年 | 6篇 |
1978年 | 4篇 |
1977年 | 1篇 |
1976年 | 1篇 |
1954年 | 3篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
671.
花垣县李梅地区早寒武世清虚洞期碳酸盐岩中的风暴沉积 总被引:4,自引:0,他引:4
扬子地台东南缘的花垣李梅地区,早寒武世晚期清虚洞组钙质风暴岩分布广泛,表现为层数众多,剖面类型丰富,识别标志清楚,颇具特色。风暴作用强度和侵蚀力按地层层序自下而上有由弱到强的规律性变化,与本区清虚洞期陆棚浅滩化演变过程相对应。早寒武世晚期的风暴事件与本区岩相、岩性的分布,均有密切联系。 相似文献
672.
The Hikurangi Margin is a region of oblique subduction with northwest-dipping intermediate depth seismicity extending southwest from the Kermadec system to about 42°S. The current episode of subduction is at least 16–20 Ma old. The plate convergence rate varies along the margin from about 60 mm/a at the south end of the Kermadec Trench to about 45 mm/a at 42°S. The age of the Pacific lithosphere adjacent to the Hikurangi Trench is not known.The margin divides at about latitude 39°S into two quite dissimilar parts. The northern part has experienced andesitic volcanism for about 18 Ma, and back-arc extension in the last 4 Ma that has produced a back-arc basin onshore with high heaflow, thin crust and low upper-mantle seismic velocities. The extension appears to have arisen from a seawards migration of the Hikurangi Trench north of 39°S. Here the plate interface is thought to be currently uncoupled, as geodetic data indicate extension of the fore-arc basin, and historic earthquakes have not exceededM
s=7.South of 39°S there is no volcanism and a back-arc basin has been produced by downward flexure of the lithosphere due to strong coupling with the subducting plate. Heatflow in the basin is normal. Evidence for strong coupling comes from historic earthquakes of up to aboutM
s=8 and high rates of uplift on the southeast coast of the North Island.The reason for this division of the margin is not known but may be related to an inferred increase, from northeast to southwest, in the buoyancy of the Pacific lithosphere. 相似文献
673.
Guy R. Cochrane Brian T. R. Lewis Kevin J. McClain 《Pure and Applied Geophysics》1988,128(3-4):767-800
Seismic reflection and refraction data off Washington and Oregon are used to determine the style of sediment deformation and to infer the physical properties of accreted sediments on the lower slope. Onshore-offshore seismic refraction data off Washington are used to determine the location of the trench, or where the plate bending starts.We find that off Washington the subduction zone is characterized by a trench whose physiographic expression is buried under several kilometers of sediments and is tens of kilometers landward of the lower slope, which is accreting seaward as the result of the offscraping of sediments.Seismic reflection data support previous observations that offscraping occurs along seaward and landward dipping thrust faults. Refraction data indicate that a sediment package thrust up along a seaward dipping fault (off Washington) was not measurably changed in velocity with respect to a Cascadia basin section. However a package uplifted by thrusting along a landward dipping fault (off Oregon) did have increased velocity. It is suggested that the increased velocities off Oregon could be the result of erosion and exposure of more deeply buried and compacted sediments, rather than the result of dewatering due to tectonic stress. Off Washington the sensitivity of velocity to porosity and resolution of the seismic method does not preclude dewatering due to tectonic stress, but it does limit the degree of dewatering.In the deeper parts of the lower slope section off Washington and Oregon velocities as high as 3 to 4 km/sec are found. Heat flow data indicate that the temperatures in this high velocity regime are greater than 100°C. It is hypothesized that lithification related to clay diagenesis may be partly responsible for the high velocities, rather than simply compaction. It also appears that the high velocity sediments are subducted while the unlithified low velocity sediments are offscraped. 相似文献
674.
675.
The determination of uranium series disequilibria in fluvial environments is proposed as a method of calculating catchment mass balances. The technique is based on two main principles. Firstly, 234U is more mobile than 238U, especially during the early stages of weathering. Secondly, uranium is far more mobile than either thorium or protactinium. Consequently, teaching during weathering results in the loss of the uranium found in the fresh rock, leaving the two immobile daughters behind. The ratio of uranium carried by sediment to that dissolved, US/UW can, therefore, be determined from river water and sediment isotopic activity ratios. Fluxes of uranium can then be calculated from average concentrations in the water and the associated sediment, from which a sediment yield can be inferred. The Witham catchment in Lincolnshire has been used to test the proposed method. A US/UW ratio of between 5 and 7 is determined and a sediment yield of 2.51 ± 2.12 tonnes yr?1 km?2 is proposed. Although some problems concerning environmental chemistry have arisen, the validity of the approach is confirmed by the close correspondence between the results obtained and those inferred by earlier workers using more conventional methods. 相似文献
676.
The C and H isotopic compositions of the methane in more than 160 gas samples from 10 basins in China are presented in this paper.The natural gases are classified as four types: biogenic gas ,bio-thermocatalytic transitional gas, gas associated with condensate oil ,and coal-type gas. The isotopic compositions of these gases closely related to the depositional basins, the types of organic matter,the stages of thermal evolution and the genetic characteristics of different gas reservoirs.Studies of the C and H isotopic compositions of terrigenous natural gases will provide valua-ble information on the prospecting and development of natural gases of different genetic types. 相似文献
678.
贵州长顺代化石炭系中间界线的沉积相研究 总被引:3,自引:3,他引:3
在碳酸盐微相的详细研究基础上,贵州长顺代化下、上石炭统剖面由下至上可分出5个主要沉积相:盆地相、开阔海陆架相、下斜坡相、中斜坡相和上斜坡相,下、上石炭统界线处于连续沉积的中斜坡相内。 相似文献
679.
大别山前寒武纪变质地体基本组成 总被引:5,自引:0,他引:5
本文以新城-圻春断裂为界将大别山前寒武纪变质地体划分为华北陆块南缘和场子陆块北缘两个次级变质地体,两个次级地体不仅在地球物理,构造变形方面明显不同,而且在物质成分上有显著差异,它们有各自独立的变质地层系统,遭受了不同类型的变质作用,有完全不同的岩浆活动图象,上述差异均可指示华北,扬子两古陆碰掸对接时扬子陆块北缘向北俯冲至华北陆块南缘之下,这可能包括两次合作用,从元古代开始至中生代最终结束的长期复杂 相似文献
680.
Structural Styles of the Longmenshan Thrust Belt and Evolution of the Foreland Basin in Western Sichuan Province, China 总被引:7,自引:0,他引:7
Liu Hefu Liang Huishe Cai Liguo Shen Fei China University of Geosciences Beijing Jiang Minxi 《《地质学报》英文版》1994,68(4):351-372
The Longmenshan thrust system consists of two major groups of structural styles according to the depth of their involvement: basement thrusts-compressional fault blocks; fold-thrust system in the cover. In cross-section, the Longmenshan structural belt is divided into 5 zones. The propagation of the Longmenshan thrust system is piggy-back due to pushing at the early stage and overstep due to gravity sliding at the late stage. Balanced cross-sections and palinspastic reconstruction reveal that the total sliding displacement of the thrust system amounts to 120 km. The tectonic evolution of the Tethys domain in western Sichuan has experienced 5 stages: continental break-up; ocean-continent subduction ; continent-arc collision; orogenic thrusting; uplift of western Sichuan. 相似文献