全文获取类型
收费全文 | 1094篇 |
免费 | 184篇 |
国内免费 | 223篇 |
专业分类
测绘学 | 45篇 |
大气科学 | 31篇 |
地球物理 | 247篇 |
地质学 | 724篇 |
海洋学 | 199篇 |
天文学 | 21篇 |
综合类 | 40篇 |
自然地理 | 194篇 |
出版年
2024年 | 1篇 |
2023年 | 6篇 |
2022年 | 30篇 |
2021年 | 19篇 |
2020年 | 41篇 |
2019年 | 46篇 |
2018年 | 42篇 |
2017年 | 41篇 |
2016年 | 55篇 |
2015年 | 53篇 |
2014年 | 66篇 |
2013年 | 55篇 |
2012年 | 62篇 |
2011年 | 78篇 |
2010年 | 58篇 |
2009年 | 76篇 |
2008年 | 80篇 |
2007年 | 76篇 |
2006年 | 70篇 |
2005年 | 58篇 |
2004年 | 65篇 |
2003年 | 55篇 |
2002年 | 38篇 |
2001年 | 38篇 |
2000年 | 38篇 |
1999年 | 39篇 |
1998年 | 39篇 |
1997年 | 30篇 |
1996年 | 25篇 |
1995年 | 21篇 |
1994年 | 23篇 |
1993年 | 15篇 |
1992年 | 10篇 |
1991年 | 10篇 |
1990年 | 7篇 |
1989年 | 5篇 |
1988年 | 5篇 |
1987年 | 1篇 |
1986年 | 5篇 |
1985年 | 7篇 |
1984年 | 7篇 |
1982年 | 1篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有1501条查询结果,搜索用时 15 毫秒
411.
412.
重庆市南岸区土地利用变化及原因分析 总被引:2,自引:0,他引:2
利用重庆市南岸区1996—2004年土地利用现状年度变更调查数据,分析其土地利用变化的过程及引起土地利用变化的原因。分析结果显示:人口增长、经济发展、农业结构调整、政策等因素是南岸区土地利用变化的主要驱动因子。并提出土地可持续利用的建议。 相似文献
413.
在分析1996~2004年福州市城市化发展和土地利用动态变化的基础上,探求城市化与土地利用变化之间的内在关系,然后选取代表性指标对建设用地和耕地数量与各自的驱动变量进行相关性分析,最后构建了驱动模型。结果表明:(1)1996-2004年,福州市土地利用结构变化明显,土地利用空间变化较大;(2)地均GDP的提高、GDP总量和全社会固定资产投资额的增长是建设用地拓展的主要驱动力;(3)耕地变化的最主要驱动力则是建设用地占用、粮食播种面积和耕地保护政策强度。 相似文献
414.
The cylindrical coal samples were subjected to three successive cycles of sorption–desorption processes of a single gas (CO2, CH4). Acoustic emission (AE) and strains were simultaneously recorded during the sorption and desorption processes.Tests were conducted on medium-rank coal from the Upper Silesia Basin, Poland. Follow-up tests for gas sorption–desorption consistently showed significant changes of AE characteristics for re-runs on the same sample. The AE level decreased in each successive test. The most spectacular differences were observed between AE generated during the first cycle of gas sorption and the subsequent cycle. This phenomenon could be due to structural changes in the coal taking place substantially on its first exposure to the sorbate. The AE results indicate, that each cycle of gas sorption–desorption was run on the same coal though with a somewhat different structure.In those tests, the swelling of coal by CO2 or/and CH4 was anisotropic (greater in the direction perpendicular to the bedding plane than parallel) in each cycle of the gas sorption–desorption process. 相似文献
415.
The Rio das Velhas greenstone belt is located in the Quadrilátero Ferrífero region, in the southern extremity of the São Francisco Craton, central-southern part of the State of Minas Gerais, SE Brazil. The metavolcano–sedimentary rocks of the Rio das Velhas Supergroup in this region are subdivided into the Nova Lima and Maquiné Groups. The former occurs at the base of the sequence, and contains the major Au deposits of the region. New geochronological data, along with a review of geochemical data for volcanic and sedimentary rocks, suggest at least two generations of greenstone belts, dated at 2900 and 2780 Ma. Seven lithofacies associations are identified, from bottom to top, encompassing (1) mafic–ultramafic volcanic; (2) volcano–chemical–sedimentary; (3) clastic–chemical–sedimentary, (4) volcaniclastic association with four lithofacies: monomictic and polymictic breccias, conglomerate–graywacke, graywacke–sandstone, graywacke–argillite; (5) resedimented association, including three sequences of graywacke–argillite, in the north and eastern, at greenschist facies and in the south, at amphibolite metamorphic facies; (6) coastal association with four lithofacies: sandstone with medium- to large-scale cross-bedding, sandstone with ripple marks, sandstone with herringbone cross-bedding, sandstone–siltstone; (7) non-marine association with the lithofacies: conglomerate–sandstone, coarse-grained sandstone, fine- to medium-grained sandstone. Four generations of structures are recognized: the first and second are Archean and compressional, driven from NNE to SSW; the third is extensional and attributed to the Paleoproterozoic Transamazonian Orogenic Cycle; and the fourth is compressional, driven from E to W, is related to the Neoproterozoic Brasiliano Orogenic Cycle. Gold deposits in the Rio das Velhas greenstone belt are structurally controlled and occur associated with hydrothermal alterations along Archean thrust shear zones of the second generation of structures.Sedimentation occurred during four episodes. Cycle 1 is interpreted to have occurred between 2800 and 2780 Ma, based on the ages of the mafic and felsic volcanism, and comprises predominantly chemical sedimentary rocks intercalated with mafic–ultramafic volcanic flows. It includes the volcano–chemical–sedimentary lithofacies association and part of the mafic–ultramafic volcanic association. The cycle is related to the initial extensional stage of the greenstone belt formation, with the deposition of sediments contemporaneous with volcanic flows that formed the submarine mafic plains. Cycle 2 encompasses the clastic–chemical–sedimentary association and distal turbidites of the resedimented association, in the eastern sector of the Quadrilátero Ferrífero. It was deposited in the initial stages of the felsic volcanism. Cycle 2 includes the coastal and resedimented associations in the southern sector, in advanced stages of subduction. In this southern sedimentary cycle it is also possible to recognize a stable shelf environment. Following the felsic volcanism, Cycle 3 comprises sedimentary rocks of the volcaniclastic and resedimented lithofacies associations, largely in the northern sector of the area. The characteristics of both associations indicate a submarine fan environment transitional to non-marine successions related to felsic volcanic edifices and related to the formation of island arcs. Cycle 4 is made up of clastic sedimentary rocks belonging to the non-marine lithofacies association. They are interpreted as braided plain and alluvial fan deposits in a retroarc foreland basin with the supply of debris from the previous cycles. 相似文献
416.
Clive E. Willman 《Mineralium Deposita》2007,42(5):449-463
The Bendigo and Castlemaine goldfields are classic examples of structurally controlled orogenic gold deposits in the Bendigo
Zone of central Victoria, SE Australia. Detailed mapping and biostratigraphic interpretation has led to a better understanding
of the regional structural controls of this type of gold-quartz mineralisation. Mineralised quartz veins are hosted by the
Castlemaine Group, an Early-to-Middle Ordovician turbidite succession at least 3,000 m thick. Gold deposits are controlled
by low-displacement faults that are clustered into several belts (the goldfields) indicating a regional structural control.
The timing of mineralisation overlapped with that of the major period of deformation including folding, cleavage development
and regional faulting. The Bendigo and Castlemaine goldfields are located in an area termed the Whitelaw thrust sheet bounded
by two unmineralised, high-displacement, regional-scale faults. Mapping has revealed an interrelationship between the regional-scale
faults, regional structural style and goldfield location. The goldfields lie immediately west of the boundary between the
upper and lower portions of the thrust sheet and are characterised by symmetric folds with sub-horizontal to synclinal enveloping
surfaces, relatively low co-axial strains and moderate cleavage development. The non-gold-bearing areas immediately east of
each goldfield correspond with the lower part of the Whitelaw thrust sheet and are characterised by higher non-coaxial strains,
stronger cleavage and folds with wide west-dipping limbs giving rise to easterly vergent sections and steeply west-dipping
enveloping surfaces. That mineralisation was an integral part of the thin-skinned style of deformation in the central Bendigo
Zone is indicated by timing relationships and the interrelationship between local-scale mineralised structures and regional-scale
features such as large-displacement unmineralised faults, regional variations in fold style and overall thrust sheet geometry.
The work supports previous models that suggest mineralised fluids were focussed along a linked system of deep-seated faults.
The primary conduits may have been major regional-scale ‘intrazone’ faults, which are inferred to sole into detachments near
the base of the Castlemaine Group. It is proposed that these structures linked with minor intrazone faults and then with networks
of low-displacement mineralised faults that were strongly controlled by folds. The location of minor intrazone faults was
probably controlled by internal thrust sheet geometry. The distribution of gold deposits and of gold production suggests that
maximum fluid flow was concentrated along the eastern margins of networks of low-displacement faults. 相似文献
417.
418.
蒙山地区平水组细碧岩角班岩系经岩石化学、微量元素及稀土元素特征和构造变形特征研究表明,形成于岛弧环境,岩浆物质来源为幔源型,来源深度约为19Km±,是扬子古板块活动陆缘增生阶段的产物;依据其构造变形特征,探讨多期变形构造叠加型式和变质作用,并确定其构造变化序列,同时显示出与双溪坞群不同的成岩构造背景. 相似文献
419.
A. R. Brown 《Boundary-Layer Meteorology》2005,114(1):233-239
Numerical simulations are presented of flow over small-scale three-dimensional hills embedded within the stable boundary layer. Large surface forces are associated with internal gravity waves excited by Fourier modes aligned with the ridge axes closely parallel to the wind. Even moderate anisotropy of the topography may then lead to the surface forces (in a frame aligned with the wind) being strongly sensitive to wind direction. However, the impact of the waves on forces in the direction of the geostrophic wind is relatively minor.The British Crowns right to retain a non-exclusive royalty-free license in and to any copyright is acknowledged. 相似文献
420.