全文获取类型
收费全文 | 917篇 |
免费 | 208篇 |
国内免费 | 87篇 |
专业分类
测绘学 | 66篇 |
大气科学 | 20篇 |
地球物理 | 586篇 |
地质学 | 270篇 |
海洋学 | 77篇 |
天文学 | 15篇 |
综合类 | 46篇 |
自然地理 | 132篇 |
出版年
2024年 | 3篇 |
2023年 | 6篇 |
2022年 | 9篇 |
2021年 | 14篇 |
2020年 | 21篇 |
2019年 | 31篇 |
2018年 | 28篇 |
2017年 | 46篇 |
2016年 | 43篇 |
2015年 | 41篇 |
2014年 | 57篇 |
2013年 | 54篇 |
2012年 | 49篇 |
2011年 | 38篇 |
2010年 | 41篇 |
2009年 | 48篇 |
2008年 | 47篇 |
2007年 | 69篇 |
2006年 | 75篇 |
2005年 | 59篇 |
2004年 | 54篇 |
2003年 | 34篇 |
2002年 | 44篇 |
2001年 | 25篇 |
2000年 | 28篇 |
1999年 | 34篇 |
1998年 | 27篇 |
1997年 | 27篇 |
1996年 | 27篇 |
1995年 | 20篇 |
1994年 | 27篇 |
1993年 | 16篇 |
1992年 | 14篇 |
1991年 | 15篇 |
1990年 | 8篇 |
1989年 | 9篇 |
1988年 | 8篇 |
1987年 | 1篇 |
1986年 | 5篇 |
1985年 | 2篇 |
1981年 | 1篇 |
1980年 | 2篇 |
1979年 | 1篇 |
1954年 | 4篇 |
排序方式: 共有1212条查询结果,搜索用时 15 毫秒
91.
92.
93.
Moment tensors of eleven major earthquakes in the Tibetan Plateau and its surrounding region from 1966 to 1980 are estimated
by generalized inverse technique. The seismic source time function and focal depth are immediately determined in the inversion.
The results show that moment tensors of some events differ significantly from double couple, the deviation increases with
decreasing plunge angle of null axis. All these events occurred in the upper crust, much shallower than those reported so
far, for example, in NEIS Bulletin. Focal mechanism solution obtained from the moment tensors are consistent with the idea
that the Indian plate collides northwards with the Eurasian plate and that an eastward spreading exists in the crust of the
Tibetan Plateau. The stress drops for earthquakes of intraplate are systematically higher than those of earthquakes in suture
zone. The source process duration becomes longer with seismic moment, but for the same seismic moment, the process duration
for earthquakes in suture zone is about 1.4 times of those for intraplate event, these results suggest that the earthquakes
near suture zone may be of a special characteristics in source process differently from those in intraplate.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,14, 423 – 434, 1992. 相似文献
94.
Abstract Focal mechanisms of intermediate-depth earthquakes within the subducted Ryukyu slab indicate a systematic pattern of down-dip extension in the northern part under Kyushu. These mechanisms switch rapidly around the Tokara channel to down-dip compression in the southern part toward Taiwan. This intriguing pattern of strain segmentation, together with the differences between the slab geometry of the northern and southern parts, has raised the question of whether stress segmentation, as defined possibly by a tear fault, might exist in the slab. However the Ryukyu trench has a concave oceanward shape in the northern segment while it is convex in the southern oceanward part toward Taiwan. The inflection zone is located around the Tokara channel. The concept of Gaussian curvature of a curved surface suggests that the along-arc variation of the geometric configuration of a subducted slab is related to the shape of the trench. This is in order to accommodate the lateral membrane deformation of the slab as the oceanic lithosphere subducts from a spherical shell to the geometry delineated by the Wadati-Benioff zone. The membrane deformation regime of the subducted Ryukyu slab and its relation with the trench geometry was examined by assuming that the subduction be modelled by the flow field of a thin viscous sheet. A projection operator was utilized to compute the membrane strain-rate tensor of an arbitrary non-Euclidean surface. Numerical experiments indicated that the northern segment of the slab was dominated by lateral compression and down-dip extension and the southern part by lateral extension and down-dip compression. This transition is sharply located near the Tokara channel. These patterns were compatible with what had been observed from studies of focal mechanisms, suggesting that the strain segmentation might be controlled, at least in part, by the lateral membrane deformation within the slab due to the trench shape in this subduction zone. The slab geometry was predicted by minimizing the integrated total dissipation power; this revealed distinct features that were consistent with observations. This implies that the slab geometry may also be affected by the membrane deformation in a systematic fashion. 相似文献
95.
2011年日本MW9.0地震(简称日本地震)后沂沭断裂带及其两侧地区地震活动显著增强,研究日本地震对该地区地壳运动及地震潜势的影响十分必要.为此,本文通过112个连续GPS观测站获取了研究区高空间分辨率的日本地震同震形变场并得到如下认识:(1)8个定点地球物理观测的同震响应验证了本文同震形变场的可靠性;日本地震的东向拉张使研究区整体上处于张性同震应变状态,但存在局部挤压区域,其中莱州湾至海州湾的挤压条带穿过沂沭断裂带并对断裂带南北两段产生了不同的同震作用,对南段具有拉张作用,对北段产生挤压作用;(2)同震形变场在鲁东隆起和鲁西断块产生了显著的剪应变,地震b值显示上述区域的构造应力在日本地震后增强,因此同震形变场可能改变了这些区域的应力特征;(3)地震矩张量叠加分析显示,同震形变场短期内对鲁西断块、鲁东隆起区和沂沭断裂带南段累积了地震矩,可能有助于上述区域在日本地震以后的地震活动增强;日本地震对沂沭断裂带北段的地震矩具有释放作用,或许是该区域地震活动减弱的原因. 相似文献
96.
IntroductionAfteramoderateorstronger(Ms25.0)earthquake,themosturgentworkofthedivisionforearthquakemonitoringandpredictionistodetermineitstimeoforigin,hypocentrallocation(longitude,latitudeanddepth)andmagnitudeandtojudgethetrendofseismicregimedevelopmentassoonaspossible.Ingeneralcases,whenanearthquakewithMS25.0insideChinaoraonewithMS26.0inneighboringareasofChinahasoccurred,theEarthquakeBulletinofChineseSeismologicalNetworkcanprovidedeterminationoftheorigintime,hypocentrallocation(longitude,… 相似文献
97.
Relationships between moment magnitude and fault parameters: theoretical and semi-empirical relationships 总被引:1,自引:0,他引:1
Fault parameters are important in earthquake hazard analysis. In this paper, theoretical relationships between moment magnitude and fault parameters including subsurface rupture length, downdip rupture width, rupture area, and average slip over the fault surface are deduced based on seismological theory. These theoretical relationships are further simplified by applying similarity conditions and an unique form is established. Then, combining thc simplified theoretical relationships between moment magnitude and fault parameters with seismic source data selected in this study, a practical semi-empirical relationship is established. The seismic source data selected is also to used to derive empirical relationships between moment magnitude and fault parameters by the ordinary least square regression method. Comparisons between semi-empirical relationships and empirical relationships show that the former depict distribution trends of data better than the latter. It is also observed that downdip rupture widths of strike slip faults are saturated when moment magnitude is more than 7.0, but downdip rupture widths of dip slip faults are not saturated in the moment magnitude ranges of this study. 相似文献
98.
引力向量和引力梯度张量在局部和全局坐标系间的转换过程是对卫星重力梯度测量进行模拟研究的主要手段和重要步骤.提出了利用计算机符号运算辅助推导该转换过程的新思想.首先通过对该过程进行分析,指出其运算繁琐复杂;然后通过对理论推导过程的分解,确定了引力向量和引力梯度张量在局部和全局坐标系之间转换的各关键步骤;并借助于计算机符号运算实现了这一转换过程的计算机推演,成功地得到了完整的符号公式结果.所编写的符号推演程序在多台计算机的多种平台上获得了一致的结果.实验结果表明,计算机符号运算对于公式体系繁杂的卫星重力学理论研究来说具有极大的增效作用. 相似文献
99.
用不变矩从机载激光扫描测高点云数据中重建规则房屋 总被引:4,自引:0,他引:4
介绍了不变矩的概念,结合实例,基于机载激光扫描测高的三雏点云数据,用不变矩实现了规则房屋的模型重建。对不变矩重建房屋模型的精度进行了讨论和分析.得出了一些有益的结论。 相似文献
100.