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   492篇
  免费   103篇
  国内免费   159篇
测绘学   18篇
大气科学   47篇
地球物理   161篇
地质学   447篇
海洋学   24篇
天文学   4篇
综合类   19篇
自然地理   34篇
  2024年   5篇
  2023年   9篇
  2022年   17篇
  2021年   17篇
  2020年   25篇
  2019年   21篇
  2018年   45篇
  2017年   14篇
  2016年   18篇
  2015年   26篇
  2014年   29篇
  2013年   30篇
  2012年   26篇
  2011年   28篇
  2010年   15篇
  2009年   39篇
  2008年   43篇
  2007年   35篇
  2006年   28篇
  2005年   25篇
  2004年   32篇
  2003年   25篇
  2002年   29篇
  2001年   20篇
  2000年   13篇
  1999年   9篇
  1998年   13篇
  1997年   9篇
  1996年   15篇
  1995年   13篇
  1994年   22篇
  1993年   19篇
  1992年   11篇
  1991年   4篇
  1990年   2篇
  1989年   3篇
  1988年   4篇
  1987年   2篇
  1986年   2篇
  1985年   3篇
  1983年   2篇
  1979年   2篇
  1978年   3篇
  1977年   2篇
排序方式: 共有754条查询结果,搜索用时 328 毫秒
91.
武夷山成矿带燕山期岩浆-成矿活动的深部动力学机制一直是学者们研究的热点.已有的研究结果表明,武夷山成矿带及邻区的上地幔存在着显著的低速异常,可能与地表的岩浆-成矿活动存在着密切的联系.本研究利用分布在华夏地块98个固定地震台站以及59个流动地震台站所记录到的278个远震事件,采用远震层析成像方法构建了武夷山成矿带及邻区...  相似文献   
92.
日本9.0级大地震前长波辐射异常研究   总被引:3,自引:1,他引:2       下载免费PDF全文
方颖  张艳梅 《地球物理学报》2012,55(8):2620-2624
应用聚类分析方法对日本Mw9.0地震前长波辐射进行了分析,结果表明2010年8月在大范围的西太平洋海域,出现一个自北向南逐渐增强的季节性高温条带,该条带从日本海沟中北段开始,一直向南延伸到伊豆—小笠原海沟.同时日本海沟的地壳垂直运动自2010年8月份开始出现季节性运动消失的异常现象.这两种现象同时出现是否表明地球物理场在大地震发生前可能出现异常?地震发生前半年时间出现的热异常条带是否与此次地震有关?这些问题有待进一步探索.  相似文献   
93.
The aim of this study is to describe ostracods from freshwater habitats in the Siberian Arctic in order to estimate the present-day relationships between the environmental setting and the geochemical properties of ostracod calcite. A special focus is on the element ratios (Mg/Ca, Sr/Ca), and the stable isotope composition (δ18O, δ13C), in both ambient waters and ostracod calcite. The most common species are Fabaeformiscandona pedata and F. harmsworthi with the highest frequency in all studied waters. Average partition coefficients D(Sr) of F. pedata are 0.33 ± 0.06 (1σ) in females, and 0.32 ± 0.06 (1σ) in males. A near 1:1 relationship of δ18O was found, with a mean shift of Δmean = 2.2‰ ± 0.5 (1σ) to heavier values in ostracod calcite of F. pedata as compared to ambient waters. The shift is not dependent on δ18Owater, and is caused by metabolic (vital) and temperature effects. Temperature-dependence is reflected in the variations of this shift. For ostracod calcite of F. pedata a vital effect as compared to inorganic calcite in equilibrium was quantified with 1.4‰. Results of this study are valuable for the palaeoenvironmental interpretation of geochemical data of fossil ostracods from permafrost deposits.  相似文献   
94.
We use annual GPS observations on the Reykjanes Peninsula (RP) from 2000 to 2006 to generate maps of surface velocities and strain rates across the active plate boundary. We find that the surface deformation on the RP is consistent with oblique plate boundary motion on a regional scale, although considerable temporal and spatial strain rate variations are observed within the plate boundary zone. A small, but consistent increase in eastward velocity is observed at several stations on the southern part of the peninsula, compared to the 1993–1998 time period. The 2000–2006 velocities can be modelled by approximating the plate boundary as a series of vertical dislocations with left-lateral motion and opening. For the RP plate boundary we estimate left-lateral motion  18+4−3 mm yr−1  and opening of  7+3−2 mm yr−1  below a locking depth of  7+1−2 km  . The resulting deep motion of  20+4−3 mm yr−1  in the direction of  N(100+8−6)°E  agrees well with the predicted relative North America–Eurasia rate. We calculate the areal and shear strain rates using velocities from two periods: 1993–1998 and 2000–2006. The deep motion along the plate boundary results in left-lateral shear strain rates, which are perturbed by shallow deformation due to the 1994–1998 inflation and elevated seismicity in the Hengill–Hrómundartindur volcanic system, geothermal fluid extraction at the Svartsengi power plant, and possibly earthquake activity on the central part of the peninsula.  相似文献   
95.
96.
花坤头营子侵入岩是花坤头营子旋卷构造的重要组成部分,共分出4个侵入体,分别为早石炭世辉绿岩、早三叠世闪长岩、中侏罗世二长花岗岩、早白垩世花岗斑岩,最晚还有一期流纹斑岩脉侵入.岩浆来源除早石炭世辉绿岩来自上地幔,余下几个序次来源于下地壳,并熔融了部分陆壳物质.以被动就位机制为特征.  相似文献   
97.
低纬度环球带和环太平洋带大地震的幕式活动分析   总被引:2,自引:0,他引:2       下载免费PDF全文
统计分析低纬度环球带(E带)和环太平洋带(P带)在1900~2008年间MW≥7.5地震的时空分布,进一步证实两者本身和两者之间都存在15~18年的幕式交替活动. 将这两大地震带分别划分为5个地震区,发现这些分区地震幕式活动互不相同, 但E带各区奇数幕与偶数幕年均地震数之比OER均大于1.58, 而P带各区的OER均小于0.93, 显示出前者以奇数幕活跃为特征, 后者以偶数幕活跃为特征. 对这些地震区的组合分析进一步证明,从幕式活动的共性看, 中太平洋地区宜纳入E带. 本文推论:低纬度环球带是另一条全球尺度地震带;大地震幕式活动的成因应归因于板块运动有几十年时间尺度的非平稳幕式运动;未来5~8年, E带的大地震还会比P带多.  相似文献   
98.
It is established that the methodological tools for quantitative measurement of the transport-geographical location is insufficiently advanced. We suggest the algorithm for the technique of its cost assessment based on determining the “economic” distances and adapted to the peculiarities of the transport system of Siberia. We calculated the costs of the transport-geographical location of Siberian microregions (within administrative districts) with respect to the most important year-round sea ports for the current (the year 2005) and future (the year 2030) levels.  相似文献   
99.
This paper examines the role of atmospheric forcing in modifying the pathways of riverine water on the Laptev Sea shelf, using summer-to-winter hydrographic surveys from 2007 to 2009. Over the two consecutive winter seasons of 2007–2008 and 2008–2009 in the area of the winter coastal polynya, our data clearly link winter surface salinity fields to the previous summer conditions, with substantially different winter salinity patterns preconditioned by summer atmospheric forcing. In the summer of 2007, dominant along-shore westerly winds in the cyclonic regime force the Lena River runoff to flow eastward. In contrast, in the summer of 2008, dominant along-shore easterly winds over the East Siberian Sea and on-shore northerly winds over the Laptev Sea in the anticyclonic regime lock the riverine water in the vicinity of the Lena Delta. Over the coastal polynya area in the southeastern Laptev Sea these patterns precondition a surface salinity difference of 8–16 psu between the winters of 2008 and 2009. Overall, this indicates a residence time of at least half a year for riverine water on the Laptev Sea shelf. Future climate change associated with an enhanced summer cyclonicity over the eastern Arctic may turn more riverine water eastward along the eastern Siberian coast, resulting in weaker vertical density stratification over the Laptev Sea shelf, with possible impact on the efficiency of vertical mixing and polynya dense water production.  相似文献   
100.
Based on their Euler poles,we calculated the relative velocities between every two plates in the typical global plate motion models,respectively,and estimated the area change along these boundaries. In our calculations,plates on both sides accommodated area changes depending on the boundary types: extensional, convergent or transform, so we can estimate area change of each plate and then globally. Our preliminary results show that the area of the southern hemisphere increased while that of the northern hemisphere decreased over the past 1 million years,and global area has increased by 26,000km2 to 36,000km2,which corresponds to the 160m~250m increment on the Earth's radius if all these area increments are attributed to Earth's expansion. Taking the NUVEL-1 model as an example,of the 14 plates in this model,11 are decreasing,but the global area has increased because of the larger increment amount from Africa,North America and Antarctica. Finally,we also discussed factors affecting the global area change such as subduction zone retreating and back-arc spreading.  相似文献   
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