全文获取类型
收费全文 | 1031篇 |
免费 | 197篇 |
国内免费 | 192篇 |
专业分类
测绘学 | 71篇 |
大气科学 | 160篇 |
地球物理 | 497篇 |
地质学 | 413篇 |
海洋学 | 123篇 |
天文学 | 7篇 |
综合类 | 85篇 |
自然地理 | 64篇 |
出版年
2024年 | 2篇 |
2023年 | 12篇 |
2022年 | 35篇 |
2021年 | 53篇 |
2020年 | 40篇 |
2019年 | 63篇 |
2018年 | 46篇 |
2017年 | 39篇 |
2016年 | 33篇 |
2015年 | 56篇 |
2014年 | 47篇 |
2013年 | 57篇 |
2012年 | 68篇 |
2011年 | 74篇 |
2010年 | 65篇 |
2009年 | 74篇 |
2008年 | 50篇 |
2007年 | 82篇 |
2006年 | 65篇 |
2005年 | 56篇 |
2004年 | 64篇 |
2003年 | 38篇 |
2002年 | 40篇 |
2001年 | 34篇 |
2000年 | 26篇 |
1999年 | 25篇 |
1998年 | 24篇 |
1997年 | 20篇 |
1996年 | 23篇 |
1995年 | 16篇 |
1994年 | 23篇 |
1993年 | 13篇 |
1992年 | 16篇 |
1991年 | 12篇 |
1990年 | 7篇 |
1989年 | 5篇 |
1988年 | 7篇 |
1987年 | 4篇 |
1986年 | 5篇 |
1981年 | 1篇 |
排序方式: 共有1420条查询结果,搜索用时 0 毫秒
91.
采用不同的方法研究了河北万全水位异常与区域中强地震活动的关系,发现万全深井水位在1989年10月18日山西大同-阳高6.1级地震前及1998年1月10日河北张北6.2级地震前有趋势性变化,水位有大于50mm的瞬时突升突降的变化。指出,万全深水井水位的形态变化和瞬间突升突降变化似可作为晋冀蒙三省交界区地震趋势判断的依据。 相似文献
92.
研究了1995年10月24日云南省武定6.5级强震前的地震活动性参数、空间分布图象、距震中135km的巧家台振幅比、波速比演化特征,结果表明武定6.5级地震孕育发生有明显的阶段性变化,经历了早期(1988年4月-1992年7月),中期(1992年8月-1995年3月),晚期(1995年4月-1995年10月)阶段的发展,最终发生了强震。最后应用岩石破裂实验结果,分析了武定6.5级地震孕震过程。 相似文献
93.
94.
滞回曲线对应力振幅和频率的响应 总被引:2,自引:0,他引:2
基于疲劳载荷对应力-应变滞回曲线的影响,作者研究了滞回曲线对应力振幅和频率的影响,获得了载荷超过屈服点后应力振幅增大,滞回曲线趋于稳定,应变硬化效应增强的结果,随着正弦波频率增加岩石的滞回圈频散效应增强,饱和液体加强了这种频散作用,随孔隙液体的粘滞系数增大,滞回曲线的频散效应更强。 相似文献
95.
TheQvaluevariationsinthepreparingpro┐cesofrockruptureBINWANG1)(王彬),ZHAO-YONGXU1)(许昭永),JIN-MINGZHAO1)(赵晋明)YI-LIHU2)(胡毅力)1)Sei... 相似文献
96.
青藏块体北缘跨断层测量资料宏观分析 总被引:1,自引:1,他引:1
本文在系统整理青藏块体北缘跨断层测量资料的基础上,进行了形变类型的划分,探讨了不同类型形变所反映的断层运动性能。 相似文献
97.
Using the data set of about 1 Hz Lg amplitudes from 80 stations in the six eastern provinces of China, the ratios of horizontal
to vertical amplitude of Lg waves,H/Z are determined. The mean lg(H/Z)-value is equal to 0.13. For the station bases of soft deposit,granite and sedimentary rock, lg(H/Z)-values average 0.55, 0.04 and 0.10, respectively. For the three kinds of station bases, the station terms of horizontal
amplitude,C
h
average 0.65, −0.09 and 0.00; that of vertical amplitude,C
z
average 0.32, −0.04 and 0.00, respectively. There are the relations betweenC
h
,C
z
and lg(H/Z):C
h
=0.01+2.10C
z
andC
h
=−0.15+1.46 lg(H/Z).
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,13, 281–286, 1991.
Project sponsored by the Chinese Joint Seismological Science Foundation. 相似文献
98.
Yuru Zhuo 《地震学报(英文版)》1992,5(1):33-43
Using the WKBJ approximation method we calculate the synthetic teleseismograms of P and PP waves to match the observed ones
of six large Chinese earthquakes with known focal mechanisms: Tibet earthquake of July 14, 1973; Haicheng earthquake of February
4, 1975; Songpan earthquakes of August 16, 1976, August 21, 1976 and August 23, 1976 and Nignhe earthquake of November 15,
1976. The focal mechanism of the Tibet earthquake is discussed to examine the technique used in the calculation.
We note that the amplitude ratios of PP and P waves (A
PP/A
P) have different characteristics for dip—slip events and strike—slip events within certain epicentral distances. We calculate
the synthetic teleseismograms of P and PP waves for the strike—slip and dip—slip events with fault angles of 330°, 240° and
0°, focal depths of 8 km, 17 km and 24 km, at the assumed station with an azimuth of 310° and epicentral distances from 40°;
to 80°. The diagrams of maximum amplitude ratios of PP and P waves (A
PP/A
P) versus distances are given. The possibility to use the (A
PP/A
P) values to give an approximate estimation for the focal mechanism type is discussed. This work may be useful for determining
the focal mechanism type for those earthquakes which have only few records such as the Chinese earthquakes from the 1930s
to 1960s.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,13, 150–160, 1991. 相似文献
99.
A mathematical model for compaction in sedimentary basins 总被引:4,自引:0,他引:4
100.
The three-dimensional nonlinear quasi-geostrophic potential vorticity equation is reduced to a linear form in the stream function in spherical coordinates for the permanent wave solutions consisting of zonal wavenumbers from 0 to n and rn vertical components with a given degree n. This equation is solved by treating the coefficient of the Coriolis parameter square in the equation as the eigenvalue both for sinusoidal and hyperbolic variations in vertical direction. It is found that these solutions can represent the observed long term flow patterns at the surface and aloft over the globe closely. In addition, the sinusoidal vertical solutions with large eigenvalue G are trapped in low latitude, and the scales of these trapped modes are longer than 10 deg. lat. even for the top layer of the ocean and hence they are much larger than that given by the equatorial β-plane solutions. Therefore such baroclinic disturb-ances in the ocean can easily interact with those in the atmosphere.Solutions of the shallow water potential vorticity equation are treated in a similar manner but with the effective depth H = RT / g taken as limited within a small range for the atmosphere.The propagation of the flow energy of the wave packet consisting of more than one degree is found to be along the great circle around the globe both for barotropic and for baroclinic flows in the atmosphere. 相似文献