全文获取类型
收费全文 | 305篇 |
免费 | 18篇 |
国内免费 | 8篇 |
专业分类
测绘学 | 17篇 |
大气科学 | 11篇 |
地球物理 | 72篇 |
地质学 | 161篇 |
海洋学 | 10篇 |
天文学 | 28篇 |
综合类 | 5篇 |
自然地理 | 27篇 |
出版年
2024年 | 1篇 |
2023年 | 2篇 |
2022年 | 11篇 |
2021年 | 16篇 |
2020年 | 17篇 |
2019年 | 13篇 |
2018年 | 21篇 |
2017年 | 19篇 |
2016年 | 25篇 |
2015年 | 20篇 |
2014年 | 21篇 |
2013年 | 38篇 |
2012年 | 18篇 |
2011年 | 21篇 |
2010年 | 12篇 |
2009年 | 19篇 |
2008年 | 12篇 |
2007年 | 6篇 |
2006年 | 7篇 |
2005年 | 4篇 |
2004年 | 2篇 |
2003年 | 2篇 |
2002年 | 3篇 |
2001年 | 5篇 |
2000年 | 2篇 |
1999年 | 3篇 |
1998年 | 2篇 |
1997年 | 1篇 |
1995年 | 2篇 |
1994年 | 1篇 |
1984年 | 2篇 |
1974年 | 2篇 |
1971年 | 1篇 |
排序方式: 共有331条查询结果,搜索用时 15 毫秒
71.
72.
73.
74.
75.
Emadullah KHAN Abbas Ali NASEEM Suleman KHAN Bilal WADOOD Faisal REHMAN Maryam SALEEM Mubashir MEHMOOD Waqar AHMAD Zubair AHMED Tahir AZEEM 《《地质学报》英文版》2022,96(5):1673-1692
The present study deals with the depositional facies, diagenetic processes and sequence stratigraphy of the shallow marine carbonates of the Samana Suk Formation, Kohat Basin, in order to elucidate its reservoir quality. The Samana Suk Formation consists of thin to thick-bedded, oolitic, bioclastic, dolomitic and fractured limestone. Based on the integration of outcrop, petrographic and biofacies analyses, the unit is thought to have been deposited on a gentle homoclinal ramp in peritidal, lagoonal and carbonate shoal settings. Frequent variations in microfacies based sea-level curve have revealed seven Transgressive Systems Tracts (TSTs) and six Regressive Systems Tracts (RSTs). The unit has undergone various stages of diagenetic processes, including mechanical and chemical compaction, cementation, micritization, dissolution and dolomitization. The petrographic analyses show the evolution of porosity in various depositional and diagenetic phases. The fenestral porosity was mainly developed in peritidal carbonates during deposition, while the burial dissolution and diagenetic dolomitization have greatly enhanced the reservoir potential of the rock unit, as is further confirmed by the plug porosity and permeability analyses. The porosities and permeabilities were higher in shoal facies deposited in TSTs, as compared to lagoonal and peritidal facies, except for the dolomite in mudstone, deposited during RSTs. Hence good, moderate and poor reservoir potential is suggested for shoal, lagoonal and peritidal facies, respectively. 相似文献
76.
Acta Geotechnica - In general, there are two classical solutions in soil mechanics to predict the shear band orientation in dense granular materials: the Coulomb and Roscoe theories. The present... 相似文献
77.
地震液化条件下重力式码头的变形破坏机理 总被引:3,自引:0,他引:3
现场调查发现在神户地震期间重力式码头破坏时都发生了相当大的侧向位移,因此,阐明挡土墙有变形机理对于改善抗震设计具有十分重要的意义。为此,根据相似原理设计了重力式码头的地基模型,进行了一系列的振动台试验。试验结果表明:基底土的强度降低和局部液化是挡土墙变形破坏的主导因素。墙后动土压力的增加为挡土墙的运动提供了条件。在液化条件下重力式码头地基的运动以侧向位移为主。重力作用是地基侧向运动的主要影响因素。减少作用于挡土墙上的动土压力和充分填实基底下的砂土是增加重力式码头抗震稳定性的重要措施。 相似文献
78.
Mohsen Jalali 《Environmental Geology》2005,47(6):763-772
Hydrochemical investigations were carried out in Bahar area, Hamadan, western Iran, to assess the chemical composition of groundwater. The area falls in a semi-arid type of climate. In this area, groundwater has been exploited over the past century mainly for irrigation and water supply. A total of 135 representative groundwater samples were collected from different wells to monitor the water chemistry of various ions. Chemical analysis of the groundwater shows that the mean concentration of the cations is of the order Ca2+>Mg 2+>Na+>K+, while that for anions is SO42–>HCO3–>Cl–>NO3–. Statistical analyses indicate positive correlation between the following pairs of parameters Cl– and Mg 2+ (r=0.71), Cl– and Na+ (r=0.76), HCO3– and Na+ (r=0.56), SO42– and Mg2+ (r=0.76), SO42– and Na+ (r=0.69). Water presents a large spatial variability of the chemical facies (Ca-HCO3, Ca-SO4, Mg-HCO3, Mg-SO4, Na-HCO3) which is in relation to their interaction with the geological formations of the basin (carbonates, dolomite and various silicates) and evaporation. The hydrochemical types Ca-HCO3 and Ca-SO4 dominate the largest part of the studied area. The dissolution of halite, calcite, dolomite, and gypsum explains part of the contained Na +, Ca2+, Mg2+, Cl–, SO42– and HCO3–, but other processes, such as cation exchange and weathering of aluminosilicates also contribute to the water composition. 相似文献
79.
80.
Kashiri Razieh Kalantariasl Azim Parsaei Rafat Zeinijahromi Abbas 《Natural Resources Research》2021,30(5):3695-3716
Natural Resources Research - Low salinity water flooding (LSWF) has been recognized as one of the promising methods for enhanced oil recovery (EOR) in sandstone reservoirs. Both the positive... 相似文献