全文获取类型
收费全文 | 3793篇 |
免费 | 1022篇 |
国内免费 | 1647篇 |
专业分类
测绘学 | 56篇 |
大气科学 | 97篇 |
地球物理 | 774篇 |
地质学 | 4507篇 |
海洋学 | 634篇 |
天文学 | 56篇 |
综合类 | 186篇 |
自然地理 | 152篇 |
出版年
2024年 | 29篇 |
2023年 | 68篇 |
2022年 | 152篇 |
2021年 | 159篇 |
2020年 | 179篇 |
2019年 | 230篇 |
2018年 | 204篇 |
2017年 | 216篇 |
2016年 | 218篇 |
2015年 | 270篇 |
2014年 | 279篇 |
2013年 | 310篇 |
2012年 | 322篇 |
2011年 | 268篇 |
2010年 | 255篇 |
2009年 | 278篇 |
2008年 | 240篇 |
2007年 | 316篇 |
2006年 | 272篇 |
2005年 | 212篇 |
2004年 | 237篇 |
2003年 | 197篇 |
2002年 | 179篇 |
2001年 | 226篇 |
2000年 | 218篇 |
1999年 | 159篇 |
1998年 | 157篇 |
1997年 | 105篇 |
1996年 | 107篇 |
1995年 | 86篇 |
1994年 | 81篇 |
1993年 | 45篇 |
1992年 | 54篇 |
1991年 | 30篇 |
1990年 | 15篇 |
1989年 | 23篇 |
1988年 | 13篇 |
1987年 | 12篇 |
1986年 | 12篇 |
1985年 | 9篇 |
1984年 | 6篇 |
1983年 | 5篇 |
1982年 | 3篇 |
1981年 | 2篇 |
1980年 | 2篇 |
1977年 | 1篇 |
1971年 | 1篇 |
排序方式: 共有6462条查询结果,搜索用时 437 毫秒
971.
972.
针对保德区块中低阶煤储层压裂过程中容易出现砂堵影响储层改造效果的问题,根据研究区块的地质条件,结合水力压裂时裂缝在煤层中的扩展规律,分析了保德区块煤层水力压裂出现砂堵的4类主要原因,分别为煤储层裂隙相对发育造成压裂液滤失量增加、压裂沟通高渗透性的顶底板、煤储层本身有效厚度大滤失量增大及多层合压造缝不充分。在此基础上,提出了相应的技术对策,使用清洁压裂液、适当提高并稳定施工排量及优化压裂施工设计,为现场的水力压裂施工和提高煤储层改造效果提供重要指导。 相似文献
973.
The barium deposits in Ankang and Xunyang counties,Shaanxi Province,China,occur in the northernmost part of the world-class barium metallogenic belt in south Qinling.The deposits are hosted by the Lower Silurian carbonaceous siliceous rocks,with a unique combination of barite and witherite.The homogenization temperatures of fluid inclusions in the barite are mainly concentrated between 135 and 155 ℃,whereas those from the witherite have two peaks of 165-175 ℃,and 215-225℃,respectively.Laser Raman analysis of fluid inclusions indicates that the vapor phase of fluid inclusions in barite is dominated by H_2O,although some contains N_2,H_2S,and CH_4.The compositions of the vapor and liquid phases of fluid inclusions in witherite can be divided into two end-members,one dominated by H_2O without other volatiles,and the other containing CH_4,C_2H_6,C_3H_8,C_2H_4,and C_6H_6 in addition to H_2O.CO_2,H_2S,and some CH_4 are interpreted as products of chemical reactions during mineralization.Organic gases(CH_4,C_2H_6,C_3H_8,C_2H_4,and C_6H_6) in the fluids were critical in the formation of barium sulfate versus carbonate.The δ~(34)S values of barite range from 38.26‰ to54.23‰(CDT),the δ~(34)S values of sulfides coexisting with barium minerals vary from 22.44‰ to25.11‰(CDT),and those in the wall rock from 11.60‰ to 19.06‰(CDT).We propose that the SO_4~(2-)generally experienced bacterial sulfate reduction in seawater before mineralization,and some SO_4~(2-)also experienced thermochemical sulfate reduction in hydrothermal system during mineralization.The δ~(13)C values of witherite range from-27.30‰ to-11.80‰(PDB),suggesting that carbon was sourced from organic substances(like CH_4,C_2H_4,and C_2H_6).The formation of witherite was possibly associated with thermochemical sulfate reduction,which caused the consumption of the organic gases and SO_4~(2-) in the hydrothermal solutions,consequently inhibiting barite formation.The important conditions for forming witherite include high fluid temperatures,high Ba~(2+) concentrations,CO_2 in the fluids,low HS~- concentrations,and the subsequent rapid diffusion of H_2S during thermochemical sulfate reduction of the fluids. 相似文献
974.
使用相关分析方法可以定量地确定地震勘探中检波器组合的组内距,达到更有效地压制各种随机干扰,从而提高地震记录的信噪比的目的,作者在本文中,利用相关分析的思路,给出了用计算机干扰相关半径定量确定组内距的野外工作方法和数据计算方法,在实施地震施工表明,使用本方法可有效地压制各种随机干扰,达到提高地震记录信噪比的目的。 相似文献
975.
IbrahimAA MusaTA 《中国地质大学学报(英文版)》2003,14(2):182-189
With a clear understanding of the drilling fluid techniques and the cutting-taking mechanism, a new advanced model is set up for analyzing field data and quantitative forecast of cutting-taking mechanism. Therefore, a number of values affecting the drilling rate and the hole cleaning are studied over a wide range of parameters. Drilling data obtained under high-borehole-pressure conditions are analyzed to determine the causes of the reduction in rate of penetration (ROP) as the borehole pressure increases, which in some cases is caused by the buildup of rock debris under the bit. The theoretical achievement and testing conclusions can be very instructional for horizontal well drilling. Much higher annular velocities are required for effective hole cleaning in directional wells than in vertical wells. Highviscosity muds are observed to provide better transport than low-viscosity muds. 相似文献
976.
977.
岩浆热液矿床是在地壳浅部形成的,恰好位于浅源地震的震源深度范围.文章将地震机制中的微裂隙群区理论引入到岩浆热液矿床成矿过程中,地震组合模式中闭锁带必须在下一次断裂滑动之前破坏,所以这个带为微裂群区和它相关的震源区的核心.文章认为微裂群区理论不但揭示了孕震机制,同时也揭示了岩浆热液矿床形成过程,岩浆热液侵位与断裂形成过程中微裂群区的形成发展密切相关,成矿期矿体范围内应力场与区域应力场呈共轭关系.微裂群区即为岩浆热液矿床的矿化富集场,控矿的隐爆角砾岩带也与微裂群区密切相关. 相似文献
978.
979.
980.
The Dalradian and Ordovician–Silurian metamorphic basement rocks of southwest Scotland and Northern Ireland host a number of base‐metal sulphide‐bearing vein deposits associated with kilometre‐scale fracture systems. Fluid inclusion microthermometric analysis reveals two distinct fluid types are present at more than half of these deposits. The first is an H2O–CO2–salt fluid, which was probably derived from devolatilization reactions during Caledonian metamorphism. This stage of mineralization in Dalradian rocks was associated with base‐metal deposition and occurred at temperatures between 220 and 360°C and pressures of between 1.6 and 1.9 kbar. Caledonian mineralization in Ordovician–Silurian metamorphic rocks occurred at temperatures between 300 and 360°C and pressures between 0.6 and 1.9 kbar. A later, probably Carboniferous, stage of mineralization was associated with base‐metal sulphide deposition and involved a low to moderate temperature (Th 70 to 240°C), low to moderate salinity (0 to 20 wt% NaCl eq.), H2O–salt fluid. The presence of both fluids at many of the deposits shows that the fractures hosting the deposits acted as long‐term controls for fluid migration and the location of Caledonian metalliferous fluids as well as Carboniferous metalliferous fluids. Copyright © 2004 John Wiley & Sons, Ltd. 相似文献