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   38193篇
  免费   7259篇
  国内免费   8787篇
测绘学   1199篇
大气科学   1975篇
地球物理   7504篇
地质学   25445篇
海洋学   4228篇
天文学   6928篇
综合类   1885篇
自然地理   5075篇
  2024年   113篇
  2023年   560篇
  2022年   1327篇
  2021年   1504篇
  2020年   1475篇
  2019年   1718篇
  2018年   1538篇
  2017年   1584篇
  2016年   1745篇
  2015年   1766篇
  2014年   2244篇
  2013年   2339篇
  2012年   2443篇
  2011年   2549篇
  2010年   2337篇
  2009年   3073篇
  2008年   2767篇
  2007年   2863篇
  2006年   2706篇
  2005年   2368篇
  2004年   2164篇
  2003年   1938篇
  2002年   1622篇
  2001年   1453篇
  2000年   1342篇
  1999年   1226篇
  1998年   1081篇
  1997年   708篇
  1996年   595篇
  1995年   560篇
  1994年   538篇
  1993年   443篇
  1992年   372篇
  1991年   234篇
  1990年   173篇
  1989年   177篇
  1988年   136篇
  1987年   119篇
  1986年   79篇
  1985年   59篇
  1984年   30篇
  1983年   20篇
  1982年   20篇
  1981年   14篇
  1980年   23篇
  1979年   27篇
  1978年   10篇
  1977年   20篇
  1976年   5篇
  1954年   19篇
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
971.
海洋平台结构振动的AMD主动控制参数优化分析   总被引:5,自引:0,他引:5  
本文针对海洋平台结构的冰激振动和地震反应控制问题,提出了采用AMD主动控制的控制策略,结合JZ20-2MUQ平台结构进行了AMD控制系统的硬参数和软参数的优化分析,并就相应于最优参数下的AMD控制海洋平台结构冰激振动和地震反应的几种代表性工况进行了时程分析,得到了一些定性和定量的结论,为实际工程的控制设计提供了基础。本文提出的AMD主动控制方法对类似的海洋平台结构的控制问题也有参考价值。  相似文献   
972.
我国抗震设计规范(GB50011-2001)规定在6、7、8度区,混凝土小砌块结构分别可以建七、六、五层。由于混凝土小砌块结构的最大优势在于10-20层(与混凝土框架或框架剪力墙结构比)。本文按1/4比例制作了10层混凝土小砌块结构模型,按7度设防要求实施构造措施,通过振动台试验研究模型结构的抗震性能。结果表明,模型结构完全能够满足在7度区“小震不坏,大震不倒”的要求。圈梁、构造柱以及水平拉结筋构成的约束体系抗震作用是明显的。试验利用砌块的非注芯孔灌注铁砂来模拟墙体出平面动力效应。在本模型的构造措施下,平出面反应不对结构破坏起控制作用。  相似文献   
973.
2001年11月14日新疆-青海交界8.1级地震   总被引:3,自引:0,他引:3  
简要介绍了2001年11月14日新疆-青海交界8.1级地震的预测情况,给出了中、美、日等对此次地震的震源参数测定和震源机制,以及余震的分布和加卸载响应比随时间的变化。进而对震区近期地震趋势进行预测。  相似文献   
974.
Abstract. A simple, fast, moment-tensor inversion method using bandpass-filtered P-amplitudes was used to study the moment-tensor statistics of Long Valley caldera microearthquakes. The events were recorded in the summer of 1997, during a swarm in the caldera. The swarm was associated with geodetic extension, uplift, and subsequent moderate earthquake activity. The moment tensor solutions for 1,993 events were calculated using the new method. The majority of the resulting focal mechanisms appear to be explained in terms of double couple mechanisms. Since some events did exhibit considerable deviation from double-couples, the moment data were studied for their statistical significance. The moments of the actual data were compared to the moments of synthetic data with varying degrees of random noise in their spectra. The results of this study suggested that unless data from more than 20 stations are used and the earthquake epicenter is located inside or very close to the network area, moment-tensor inversion does not correctly resolve the non-double-couple components of microearthquakes. Analysis of the inversion residuals shows that the average noise in the P-wave spectra was close to 20%. The fluctuations of the volumetric components of the moment-tensor are in good agreement with those of the synthetic pure double-couples with 20% of added noise. Thus the moment-tensor statistics suggests that little if any volume change is required to explain the observed seismic energy release in the swarm. However, the statistics do show that a significant compensated-linear-vector-dipole component maybe present in the bulk of the seismicity. Given the network used in this study, such a component could not be precisely resolved for individual earthquakes. This possibility deserves further investigation because of its bearing on the nature of fluid-fault-earthquake processes in swarms.  相似文献   
975.
976.
Focal Fault of the 1999 Datong Ms5.6 Earthquake in Shanxi Province   总被引:1,自引:0,他引:1  
Several earthquakes with Ms≥5.0 occurred in the Datong seismic region in 1989,1991 and 1999,The precise focus location of the earthquake sequence was made by the records of the remote sensing seismic station network in Datong.Using that data together with macro-intensity distribution and focal mechanism solutions,we analyze the difference among three subsequences.The results show that the focal fault of the 1999 Ms 5.6 earthquake was a NWW-trending left-lateral strike-slip fault.It is 16km long and 12km wide.It developed at the depth of 5km and is nearly vertical in dip.The two previous earthquake subsequences,however,were generated by activity along NNE-trending right-lateral strike-slip fault.It can be found that the rupture directioin of the 1999 earthquake has changed.It is generally found that a rupture zone has more than two directions and has different strength along these two directions.The complicate degree of focal circumstance is related to the type of earthquake sequences.There is the NE-trending Dawangcun fault and the NW-trending Tuanbu fault in the seismic region,but no proof indicates a connection between focal faults and these two tectonic faults.The feature that focal faults of three subsequences are strike-slip is different from that of the two tectonic faults.It is suggested that the 1999 earthquake subsequence was possibly generated by a new rupture.  相似文献   
977.
为研究钢筋砼摩擦耗能支撑框架结构的动力反应性能 ,对其中的摩擦耗能器单元和框架杆单元的单元刚度和力学模型做了分析。钢筋砼摩擦耗能支撑单元由支撑杆单元和钢板—橡胶摩擦耗能器单元组成 ,支撑单元可取空间杆单元 ,摩擦耗能器单元为平面应力矩形单元。摩擦耗能器单元的剪切恢复力曲线为理想的弹塑性曲线 ,根据耗能器单元的力学模型 ,可确定其在每一时刻的刚度 ;框架结构空间杆单元的恢复力模型采用双线型模型 ,根据杆单元的力学模型 ,可确定其在每一时刻的刚度。并利用所编制的程序对十层单榀两跨空间普通框架和摩擦耗能支撑框架在地震作用下进行了弹塑性反应时程分析 ,结果表明耗能支撑框架的顶层最大位移明显小于普通框架  相似文献   
978.
昆仑山口西8.1级地震的远程地下水动力学效应   总被引:3,自引:2,他引:3  
王道 《内陆地震》2002,16(3):213-223
对新疆北天山地区地下流体的动态观测资料进行分析 ,发现在 2 0 0 1年 11月 14日昆仑山口西 8.1级地震的震时和震后 ,多井水位、水温、流量出现大量异常变化 ,其特征主要表现为地震波的同震振动效应和震后阶跃变化。其中乌鲁木齐 10号井的地震波效应双振幅最大 ,为 185 mm,持续时间达 2个小时 ;0 4井水位阶跃上升幅度较大 ,为 0 .12 5 m,且具有不可逆特征。另外 ,对比了新疆及邻区 7级以上地震北天山地下水的震后效应 ,讨论了地下水远程效应与井震距离的关系以及阶跃异常的幅度等问题  相似文献   
979.
华北板内深部构造   总被引:9,自引:0,他引:9  
华北板块的形成经历了早前寒武纪、燕山期及喜马拉雅期3个主要构造发展期,由于华北板块自身运动及所受应力场的作用,加之上地幔岩石圈的不均一性等因素,在中、新生代形成许多特殊的板内构造块。综合应用地质、地球物理和地球化学的成果,对华北板内深部结构进行了研究。从深部构造角度划分出6个金及金金属成矿带、4个金刚石成矿带,并对华北地区的地震及地热资源与新生事大陆裂谷的关系进行了探讨。  相似文献   
980.
 The non-parametric Mann–Whitney (MW) statistic test has been popularly used to assess the significance of a shift in median or mean of hydro-meteorological time series. It has been considered that the test is more suitable for non-normally distributed data and it may be not sensitive to the distribution type of sample data. However, no evidence has been provided to demonstrate these. This study investigates the power of the test in various circumstances by means of Monte Carlo simulation. Simulation results demonstrate that the power of the test is very sensitive to various properties of sample data. The power depends on the pre-assigned significance level, magnitude of a shift, sample size, and its occurrence position within a time series; and it is also strongly affected by the variation, skewness, and distribution type of a time series. The bigger the magnitude of a shift, the more powerful the test is; the larger the sample size, the more powerful the test is; and the bigger the variation within a time series, the less power the test has. The test has the highest power if a shift occurs at the midpoint of a time series. For the samples with different distribution types, the power of the test is dramatically different. The test has the highest power for time series with the extreme value type III (EV3) distribution while it indicates the lowest power for time series with the lognormal distribution.  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