全文获取类型
收费全文 | 8015篇 |
免费 | 1932篇 |
国内免费 | 1881篇 |
专业分类
测绘学 | 826篇 |
大气科学 | 476篇 |
地球物理 | 2265篇 |
地质学 | 6398篇 |
海洋学 | 962篇 |
天文学 | 124篇 |
综合类 | 412篇 |
自然地理 | 365篇 |
出版年
2024年 | 26篇 |
2023年 | 106篇 |
2022年 | 277篇 |
2021年 | 305篇 |
2020年 | 318篇 |
2019年 | 395篇 |
2018年 | 334篇 |
2017年 | 387篇 |
2016年 | 473篇 |
2015年 | 443篇 |
2014年 | 593篇 |
2013年 | 586篇 |
2012年 | 564篇 |
2011年 | 617篇 |
2010年 | 459篇 |
2009年 | 562篇 |
2008年 | 528篇 |
2007年 | 525篇 |
2006年 | 527篇 |
2005年 | 500篇 |
2004年 | 403篇 |
2003年 | 405篇 |
2002年 | 349篇 |
2001年 | 296篇 |
2000年 | 292篇 |
1999年 | 214篇 |
1998年 | 229篇 |
1997年 | 190篇 |
1996年 | 180篇 |
1995年 | 155篇 |
1994年 | 139篇 |
1993年 | 100篇 |
1992年 | 80篇 |
1991年 | 46篇 |
1990年 | 40篇 |
1989年 | 29篇 |
1988年 | 48篇 |
1987年 | 21篇 |
1986年 | 21篇 |
1985年 | 13篇 |
1984年 | 16篇 |
1983年 | 6篇 |
1982年 | 1篇 |
1981年 | 2篇 |
1979年 | 16篇 |
1978年 | 7篇 |
1977年 | 2篇 |
1954年 | 3篇 |
排序方式: 共有10000条查询结果,搜索用时 31 毫秒
101.
102.
Although it has been shown that the potential of tight‐sand gas resources is large, the research into the mechanisms of hydrocarbon charging of tight sandstone reservoirs has been relatively sparse. Researchers have found that there is a force balance during hydrocarbon charging, but discriminant models still have not been established. Based on the force balance conditions observed during gas migration from source rocks to tight sandstone reservoirs, a calculation formula was established. A formula for identifying effective source rocks was developed with the gas expulsion intensity as the discrimination parameter. The critical gas expulsion intensity under conditions of various burial depths, temperatures, and pressures can be obtained using the calculation formula. This method was applied in the Jurassic tight sandstone reservoirs of the eastern Kuqa Depression, Tarim Basin, and it was calculated that the critical expulsion intensity range from 6.05 × 108 m3/km2 to 10.07 × 108 m3/km2. The critical gas charging force first increases with depth and later decreases with greater depths. The distribution range of effective gas source rocks and total expelled gas volume can be determined based on this threshold. This method provides new insight into and method for predicting favourable tight‐sand gas‐bearing regions and estimating their resource potentials. Copyright © 2014 John Wiley & Sons, Ltd. 相似文献
103.
南海神狐海域天然气水合物注热降压开采数值模拟研究 总被引:2,自引:0,他引:2
针对南海神狐海域天然气水合物成藏条件,利用pT+H软件和水平井技术对天然气水合物的注热和注热降压开采效果进行了模拟分析。重点讨论了注入热水温度为30、60、90℃时水合物饱和度以及CH4气体饱和度、CH4产气率、累积CH4产气量和产水量的变化规律,发现两种开采模式下水合物低饱和度分布范围随时间增长和温度升高而增大;CH4产气率在开采10 d内升高较快,之后逐渐减小。模拟结果表明:注热降压开采模式比单纯注热模式的效果有较大改善,而且温度对于提高CH4产气量效果不明显,但因为天然气水合物藏的低渗透性,神狐海域的天然气水合物的CH4产气量不大。研究结果可为南海神狐海域和类似地区天然气水合物开采提供参考。 相似文献
104.
鄂尔多斯盆地靖边气田现今构造面貌为一区域性西倾大单斜,其下古生界奥陶系主力气层为马五段马五31小层,该小层顶面构造是在极其平缓的构造背景上发育的小幅度褶皱,且局部小幅度构造与产能关系密切,是寻找高产区的有利指向。应用地震解释成果和测井、钻井资料,研究J井区主力气层马五31顶面的小幅度构造分布特征;分析马五31顶面与本溪组9号煤顶、马家沟组标志层(K1、K2)构造的相关性;总结鼻状构造的组合类型;研究鼻隆构造与天然气富集的关系;总结构造圈闭与复合圈闭类型;分析小幅度构造成因动力学特征。这些认识对该井区井位部署、扩边挖潜及水平井动态调整,提高气田开发钻井成功率有着重要的现实意义。 相似文献
105.
针对石南31井区储层岩性多变、油气水关系复杂等问题,按不同岩性识别油气层、水层和干层,据油气不同测井响应特征进一步识别油层和气层.将储层划分为细砂岩、中粗砂岩和砂砾岩3类,识别储层流体性质,分析油藏分布特征,指出油层、隔夹层平面分布特征,探讨油气水层分布规律.结果表明,石南31井区主要有4个油藏.储层所含流体有油、水和气,中北部细砂岩储层为纯油层,南部中粗砂岩储层为水层.气层从南到北分布于全区,主要位于油藏北部和东部局部区域,为今后解释工作具很好指导意义. 相似文献
106.
The age-accumulation effect of 40Ar in hydrocarbon source rocks was discussed in accordance with the decay law of radioactive elements. In terms of the mean values of 40Ar/36Ar, the old Sinian gas reservoirs (mean values of 40Ar/36Ar: 7009) were definitely distinguished from the Permian gas reservoirs (mean values of 40Ar/36Ar: 1017) in Weiyuan, Sichuan Province, and the gas source of the Permian gas reservoir (mean values of 40Ar/36Ar: 5222) in well Wei-7 with the Weiyuan structure is defined as the Sinian system. Based on the values of 40Ar/36Ar, the coal-type gases (The source rocks are of the C-P system; mean values of 40Ar/36Ar: 1125) are definitely distinguished from the oil-type gases (The source rocks are of the Tertiary system; mean values of 40Ar/36Ar: 590) in the Tertiary reservoirs of the Zhongyuan Oilfield. Besides, 40Ar/36Ar values also have a positive effect on the oil-source correlation of oil reservoirs in ancient hidden mountains. According to the crust-mantle interchange information reflected by 3He/4He values, petroliferous provinces in China can be divided into three major tectonic regions. (1) The eastern active region: The crust-mantle volatile matter exchanges actively, and the 3He/4He values are mainly around 10-6, partly around 10-7. (2) The central stable region: The 3He/4He values are all around 10-8. (3) The western sub-stable region: The 3He/4He values are mainly around 10-8, and around 10-7 on the edges of the basins. Helium contents of some gas wells in China’s eastern petroliferous region reach the industrial abundance (He≈0.05%–0.1%), the 3He/4He values reach 10-6, and the equivalent values for the mantle-source components in helium gas can reach 30%–50%. As viewed from this, a new type of crust-mantle composite helium resources has been proposed. Geneses of some CO2 gas reservoirs in the east of China and some issues concerning mantle-source methane were discussed in the light of the helium and carbon isotopes of CO2 and CH4 in natural gases. In the discussion on helium isotopic characteristics of inclusions in the reservoirs, it was discovered that the 3He/4He values are close to those in natural gases. That is to say, this phenomenon is related to regional tectonism. The 3He/4He, CO2/3He and CH4/3He data were used to discuss the tectonic activities of fault zones in a certain number of regions in China. 相似文献
107.
108.
109.
LI Jijun LU Shuangfang WU Wei XUE Haitao XU Qingxi GENG Jie YU Yinghua 《《地质学报》英文版》2011,85(5):1203-1210
In order to discuss the role and influence of water during the generation of natural gas, the participation mechanism of water during the evolution of organic matter and its influences were summarized. In addition, we carried out an anhydrous cracking experiment of oil extracted from the Feixianguan Formation source rock in a closed system, which led to the establishment of the kinetic models for describing carbon and hydrogen isotopic fractionation during gas generation from organic matter. The models were calibrated and then applied to the northeastern Sichuan Basin. By combining a series of gas generation experiments from octadecane pyrolysis without water or with distilled water in varying mass proportions, several results were proved: (1) the hydrogen isotopic composition of natural gas becomes lighter with the participation of formation water; (2) we can quantitatively study the hydrogen isotopic fractionation with the kinetic model for describing carbon isotopic fractionation; (3) more abundant and reliable geological information can be obtained through the combined application of carbon and hydrogen isotopic indices. 相似文献
110.
In order to recognize the impact of aqueous medium on gas yields and the kinetic behaviors of hydrogen isotope fractionation during organic matter thermal degradation, the gold tube apparatus was used to conduct thermal simulation experiments by mixing the nC18 with the water of different properties and proportions. The yields of natural gas components, the relation among hydrogen isotope composition of each component and the experimental temperatures vs. heating rates have been obtained, and the results indicate that under the higher temperature conditions, the hydrous experiment has obvious impact on gas yields, such as when more water is added, higher amounts of hydrocarbon gas and H2 are yielded, and the existence of water obviously prolongs the temperature interval with the existence of heavy hydrocarbon gas. It also shows that the hydrogen isotope of hydrocarbon gas generated by the hydrous experiment is obviously lighter than that generated by the anhydrous experiment, and with the increasing amount of added water, the δD value of hydrocarbon gas gradually decreases. Compared with gas yields, the variation of δD value is more sensitive to aqueous medium in the thermal simulation experiment. However, compared with the amount of the added water, the aqueous medium property has smaller impact on the gas yields, which still shows the inherit effect on hydrogen isotope composition of aqueous medium. Through the model simulation and the isotope fractionation behavior analysis, it is validated that the hydrogen isotope fractionation process can be well described by the chemical kinetic model. The difference of reaction fraction of normal methane and D-containing methane is large, corresponding to the same activation energy. The content of normal methane is obviously higher in the part with lower activation energy, while the content of D-containing methane is higher in the part with higher activation energy. Therefore, it will result in larger hydrogen isotope fractionation amplitude, and the δD values will be more sensitive to the variation of maturity. Meanwhile, the average activation energy of methane generation from nC18 in the hydrous experiment is higher than that in the anhydrous experiment, and the greater amount of added water, the larger the average activation energy of methane generation reaction. This has laid foundation for its exploratory application in the study of gas reservoir forming history and the gas-source correlation, which indicates the research and application prospects in this orientation. 相似文献