全文获取类型
收费全文 | 5561篇 |
免费 | 1376篇 |
国内免费 | 1582篇 |
专业分类
测绘学 | 690篇 |
大气科学 | 909篇 |
地球物理 | 1144篇 |
地质学 | 3352篇 |
海洋学 | 888篇 |
天文学 | 168篇 |
综合类 | 560篇 |
自然地理 | 808篇 |
出版年
2024年 | 18篇 |
2023年 | 138篇 |
2022年 | 369篇 |
2021年 | 372篇 |
2020年 | 327篇 |
2019年 | 354篇 |
2018年 | 402篇 |
2017年 | 354篇 |
2016年 | 346篇 |
2015年 | 349篇 |
2014年 | 355篇 |
2013年 | 406篇 |
2012年 | 353篇 |
2011年 | 386篇 |
2010年 | 369篇 |
2009年 | 337篇 |
2008年 | 325篇 |
2007年 | 301篇 |
2006年 | 232篇 |
2005年 | 220篇 |
2004年 | 213篇 |
2003年 | 216篇 |
2002年 | 346篇 |
2001年 | 270篇 |
2000年 | 226篇 |
1999年 | 208篇 |
1998年 | 121篇 |
1997年 | 87篇 |
1996年 | 80篇 |
1995年 | 78篇 |
1994年 | 73篇 |
1993年 | 59篇 |
1992年 | 58篇 |
1991年 | 28篇 |
1990年 | 32篇 |
1989年 | 17篇 |
1988年 | 17篇 |
1987年 | 11篇 |
1986年 | 11篇 |
1985年 | 13篇 |
1984年 | 9篇 |
1983年 | 2篇 |
1982年 | 8篇 |
1981年 | 6篇 |
1980年 | 3篇 |
1978年 | 1篇 |
1977年 | 1篇 |
1958年 | 4篇 |
1957年 | 1篇 |
1954年 | 7篇 |
排序方式: 共有8519条查询结果,搜索用时 125 毫秒
991.
Rare—Earth Element Geochemistry of Elogites from the Ultra—High Pressure Metamorphic Belt in Central China 总被引:2,自引:1,他引:1
Based on their REE contents and REE patterns,eclogites from the ultra-high pressure metamorphic belt in central China may be roughly divided into xis types including LREE-rich.LREE-rich positive Eu anomaly,LREE-rich negative Eu anomaly,REE pattern-smooth,MREE-rich and HREE-rich.The LREE_rich,LREE-rich positive Eu anomaly and LREE-rich negative Eu anomaly types of eclogites are dominant .REE types of eclogites in different areas can be compared and the REE feactures of the same REE type of eclogites in different areas are similar.The results of reconstruction of the primary rocks show that the primary rocks of eclogites possibly are dominated by continental tholeiites which are the product of partial melting of relatively fertile mantle and the rocks of tholeiite crystallization-differentiation.There is perfect evolution relationship among the primary rocks of the LREE-rich, LREE-rich positive Eu anomaly and LREE-rich negative Eu anomaly types of eclogites and among those of the REE pattern smooth and MREE-rich types of eclogites,the former three types were deried from continental settings and the latter two from nearly oceanic settings.Meanwhile,it is concluded that the mantle sources of primary rocks of the eclogites are inhomogeneous and the primary rocks of eclogites in this area appear to have undergone varying degree of crustal contamination. 相似文献
992.
Experimental simulation of dolomite dissolution under burial diagenesis conditions and thermodynamic interpretation 总被引:3,自引:0,他引:3
Simulating experiments on dolomite dissolution by acetic acid were made under burial diagenesis conditions,at temperatures ranging from 75℃to 130℃ and pressures from 20 MPA to 30MPa,The results show that the dissolution rate of dolomite increased rapidly with increasing temperature and prssure,From 75℃/Mpa to 130℃/30 MPa,the total amount of released ca and Mg increased from 32.98mg/L to 337.9mg/L,over one order of magnitude in difference,Thermodynamic calculation indicates that the increment of Gibbs free energy (ΔG) of the chemical reaction decreases with increasing temperature and pressure.This thermodynamic result is consistent with the experimental result.Based on the Experimental results.it is suggested that secondary prosities formed by dolomite dissolution under conditions of deep burial diagenesis should be more common than those under epigenesis and shallow burial conditions,and therefore dolomite reservoires in the formations that have been deeply buried should be more abundant than in the formations that have only been shallowly buried. 相似文献
993.
The Bogda Shan orogenic belt is interpreted to be an Upper Palaeozoic continental rift, which was closed towards the end of the Carboniferous period. Intrusive activities in that belt are represented mainly by a large number of diabasic sills, dykes and stocks with sparse dioritic and granitic bodies. Determinations on a group of samples from the Shangdaheyan intrusion yielded a mineral-rock Rb-Sr isochron with an age of 298.4±0.76 Ma and an initial87Sr/86Sr ratio of 0.7041. In combination with field evidence, these results indicate that most of the intusions of the Bogda Shan orogenic belt were emplaced during the Hercynian cycle as a result of initial extension following rift closure, and that post-Hercynian intrusive activities are not important in that belt. 相似文献
994.
Types of Enclaves and Their Features and Origins in Intermediate-Acid Intrusive Rocks from the Tongling District, Anhui Province, China 总被引:9,自引:0,他引:9
WU Cailai WANG Zhihong QIAO Dewu LI Haibing HAO Meiying SHI Rendeng Institute of Geology Chinese Academy of Geological SciencesXi''an Engineering College Geological Mechanics Institute CAAGS 《《地质学报》英文版》2000,74(1):54-67
Enclaves in intermediate-acid plutons from Tongling can be divided into three types: xenoliths, relics and magmatogenic enclaves. The magmatogenic enclaves consist of cumulates, micrograined dioritite mixtite and dioritic chilled border enclaves. Petrologically, relics with eyed and meta-poikilitic texture are characterized by high content of biotite (>80%) and low content of cordierite and grossular. The cumulates with accumulate texture consist of a great amount of pyroxene, hornblende and minor spinel and phlogopite. The micrograined dioritic mixtite is composed of more hornblendes and feldspar and less needle apatites and an ellipsoid basic core included in plagio-clase. The chilled border enclaves have the same mineral association, but more dark minerals than the host rocks consisting of plagioclase, quartz, alkaline feldspar, hornblende and biotite. Geochemically, the relics exhibit high REE content (455.8×10-6) and high ratio of LREE/HREE, more obvious Eu negative anomaly and are rich in Cr and 相似文献
995.
QIAO Yanxiao LI Miwen Remote Sensing Center of Hebei Province Huaizhong Rd. Shijiazhuang Hebei 《《地质学报》英文版》2000,74(2):334-338
The Taihang Mountains area is an area in North China where serious mudflow hazards take place frequently. The hazards often obstrust traffic and make it difficult to carry out conventional ground investigations of the mudflow hazards. This paper introduces the feasibility study of mudflow hazards by using Landsat-5TM data. The study has achieved a great success through adopting both the faint spectral enhancement technique for mudflow fans (or other depositional areas) and comprehensive study of the environmental background of pregnant mudflows. Thus, remote sensing as a fast, convenient, low-cost and effective technical method can be used to recognise the situation of mudflow hazards so that effective rescue can be provided. 相似文献
996.
内蒙大青山山前活动断裂带西端左旋走滑现象 总被引:10,自引:0,他引:10
位于大青山山前断裂西端约10km的地段,18条冲沟不同程度地发生了左旋扭曲,扭曲量20~300m不等。冲工度与左旋扭曲量显示了较好的正比关系。从山前台地与冲沟的切割关系可以看到,这些上游长度1~5km及小于1km的冲沟形成在晚更新世末期及全新世以后,同时冲沟沟口河流冲洪积相砂砾石层直接与山边黄色亚砂土断层接触,断层下降盘地层年龄早于断层上升盘的地层年龄,显示了断层的走滑活动,由断错的地层年代估算,大青山山前活动断裂西端全新世左旋走滑速率达到5mm/a。此外,本文还讨论了了大青山山前活动断裂的演化机制。 相似文献
997.
Acidic species, such as Nitrate, in polar snow and firn layers are “reversibly” deposited, and are sufficiently volatile to undergo significant postdepositional exchange between snow/firn and the atmosphere. Through comparison of the snowpit and snowpack nitrate concentrations from central East Antarctica and the headwater of ürumqi River, we conclude that the nitrate peaks in the uppermost surface snow layers in central Antarctica are not related to an atmospheric signal and must account for post-depositional effects. Such effects, however, are not found in the surface snowpack nitrate profiles from the headwater of ürumqi River. Two reasons may account for the post-depositional difference. At first, nitrate in the polar snow and firn layers appears to be hydrated ion, which can be taken up by the atmosphere, while at the headwater of ürumqi River it seems mainly as mineral ion, which assembles the behavior of aerosol-derived species that are “irreversibly” deposited and do not undergo significant post-depositional exchange with the atmosphere. Secondly, the chemical features of the snow and ice on the Antarctica are mainly determined by wet deposition, to the contrary, dry deposition is more significant at the headwater of lUrumqi River than that on the East Antarctic Plateau. 相似文献
998.
999.
从地形变资料探讨丽江7.0级地震的前兆特征 总被引:2,自引:0,他引:2
讨论了地震孕育发生的物理机制是“拉疏隆起-压缩凹陷”模式的形成机理及其特征;根据这一理性认识,应用丽江7.0级地震之前滇西地区的地形变资料,较确切出得出了本区有强震发生,并且可以认为孕震体是在丽江至玉龙雪山东麓地区;根据发震前夕所观测到孕震体的“拉疏隆起-压缩凹陷”的区域大小与幅度值及岩层的弹性应变,可近似计算震级的大小。 相似文献
1000.
给出了川- 20 地下水综合观测井井下仪器探头可能存在机械部分相互干扰的现场研究结果。所得结果对于正确区分各种手段今后的异常与干扰具有参考意义。 相似文献