首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   2137篇
  免费   58篇
  国内免费   80篇
测绘学   82篇
大气科学   232篇
地球物理   434篇
地质学   750篇
海洋学   145篇
天文学   474篇
综合类   9篇
自然地理   149篇
  2023年   21篇
  2022年   20篇
  2021年   10篇
  2020年   16篇
  2019年   18篇
  2018年   68篇
  2017年   59篇
  2016年   101篇
  2015年   64篇
  2014年   75篇
  2013年   122篇
  2012年   90篇
  2011年   114篇
  2010年   100篇
  2009年   157篇
  2008年   117篇
  2007年   108篇
  2006年   101篇
  2005年   84篇
  2004年   86篇
  2003年   96篇
  2002年   63篇
  2001年   82篇
  2000年   64篇
  1999年   48篇
  1998年   56篇
  1997年   47篇
  1996年   50篇
  1995年   30篇
  1994年   43篇
  1993年   27篇
  1992年   28篇
  1991年   13篇
  1990年   10篇
  1989年   7篇
  1988年   12篇
  1987年   7篇
  1986年   7篇
  1985年   5篇
  1984年   10篇
  1983年   6篇
  1982年   6篇
  1980年   3篇
  1979年   3篇
  1978年   2篇
  1976年   2篇
  1973年   2篇
  1972年   3篇
  1921年   1篇
  1915年   1篇
排序方式: 共有2275条查询结果,搜索用时 15 毫秒
101.
The Gorgon Platform is located on the southeastern edge of the Exmouth Plateau in the North Carnarvon Basin, North West Shelf, Australia. A structural analysis using three-dimensional (3D) seismic data has revealed four major sets of extensional faults, namely, (1) the Exmouth Plateau extensional fault system, (2) the basin bounding fault system (Exmouth Plateau–Gorgon Platform Boundary Fault), (3) an intra-rift fault system in the graben between the Exmouth Plateau and the Gorgon Platform and (4) an intra-rift fault system within the graben between the Exmouth Plateau and the Exmouth Sub-basin. Fault throw-length analyses imply that the initial fault segments, which formed the Exmouth Plateau–Gorgon Platform Boundary Fault (EG Boundary Fault), were subsequently connected vertically and laterally by both soft- and hard-linked structures. These major extensional fault systems were controlled by three different extensional events during the Early and Middle Jurassic, Late Jurassic and Early Cretaceous, and illustrate the strong role of structural inheritance in determining fault orientation and linkage. The Lower and Middle Jurassic and Upper Jurassic to Lower Cretaceous syn-kinematic sequences are separated by unconformities.  相似文献   
102.
103.
104.
105.
106.
In this paper, the CPT-based predicted ultimate pile resistances (Rp) were compared with the measured pile resistances (Rm) at different elapsed time for the piles driven into saturated soft clays where piles displayed significant set-up effect. The measured pile resistances were based on 115 restrike records collected from 95 production piles, and 74 records of 9 tested piles. The predicted ultimate pile resistances were calculated from the LCPC, the Schmertmann, and the de Ruiter–Beringen methods, respectively. With the significant pile set-up effect taken into account, the relationship between measured resistances and predicted capacities at different times after pile installation were investigated. The ratios of the measured pile resistances to the predicted capacities scattered in a large spectrum. The ratios fluctuated and stayed within a range of 0.6–1.6 for different CPT methods since end of initial driving until more than 2 months after pile installation. Plots of the ratios versus the predicted pile capacities using different CPT methods have revealed that the ratio (Rm/Rp) presented a strong dependence on the predicted capacities. Great research efforts have been devoted to the analyses of the ratios of the 24-h measured resistance to the predicted capacity based on different CPT methods, in an attempt to find a feasible empirical correlation. It is found that a simple linear relationship exists between the quad root of the ratio and the predicted capacity. The developed empirical equations will give pile foundation engineers an insight into the ultimate resistances of driven piles demonstrating significant pile set-up effects. Pile set-up makes pile resistances grow with time, and it might be one of the reasons that cause the frequently reported large discrepancy between calculated static capacity and measured resistance at a certain time after pile installation.  相似文献   
107.
This study has reviewed the distribution and pedogenesis of late Mesozoic A-Type granitoids in SE China. These A-Type granitoids belong to four belts ( S Jiangxi-SW Fujian belt, Xiang-Gui-Yue belt, Can-Hang belt and coastal belt) due to their temporal-spatial distribution. Based on the comparative analysis of chronology, geochemistry and magmatic association, this study has discussed the formation of A-Type granitoids and the subduction and slab rollback process of paleo-Pacific plate beneath SE China.  相似文献   
108.
109.
110.
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号