全文获取类型
收费全文 | 91篇 |
免费 | 68篇 |
国内免费 | 7篇 |
专业分类
测绘学 | 10篇 |
大气科学 | 7篇 |
地球物理 | 112篇 |
地质学 | 23篇 |
海洋学 | 9篇 |
天文学 | 1篇 |
综合类 | 3篇 |
自然地理 | 1篇 |
出版年
2024年 | 1篇 |
2023年 | 6篇 |
2022年 | 5篇 |
2021年 | 9篇 |
2020年 | 9篇 |
2019年 | 5篇 |
2018年 | 7篇 |
2017年 | 6篇 |
2016年 | 7篇 |
2015年 | 4篇 |
2014年 | 10篇 |
2013年 | 12篇 |
2012年 | 8篇 |
2011年 | 7篇 |
2010年 | 10篇 |
2009年 | 4篇 |
2007年 | 6篇 |
2006年 | 6篇 |
2005年 | 2篇 |
2004年 | 2篇 |
2003年 | 3篇 |
2002年 | 4篇 |
2001年 | 2篇 |
2000年 | 2篇 |
1999年 | 4篇 |
1998年 | 5篇 |
1996年 | 4篇 |
1994年 | 4篇 |
1993年 | 4篇 |
1992年 | 2篇 |
1991年 | 2篇 |
1989年 | 3篇 |
1954年 | 1篇 |
排序方式: 共有166条查询结果,搜索用时 15 毫秒
31.
推导出频率域有限元声波正演方程,为了消除边界反射,将Clayton-Engquist旁轴波动方程吸收边界条件引入频率域,并对有限元刚度矩阵和质量矩阵进行压缩存储,利用广义共轭梯度法求解有限元方程获得正演解.在此基础上,推导出在某一频率下波场数据残差δU与单元物性参数修改量δλ之间关系的Jacobi矩阵,反演方法允许利用地面二维炮集全波场资料与给出初始模型参数的正演值的差值δU,迭代求得δλ.由于计算机内存的限制,方法计算不允许有过多数目的未知数个数,因此还提出了对同一介质物性单元的Jacobi矩阵元素进行压缩组装的措施,从而使反演的未知量个数减少,结合采用共轭梯度迭代法,使得只需利用有效波频段的少数一些频率即可进行迭代反演.正演和反演理论模型的数值模拟结果表明方法是有效的. 相似文献
32.
低序级断层是复杂断块油藏勘探开发的重要研究内容,对油田开发后期落实剩余油分布、解决注采矛盾具有重要意义.本文采用声波方程有限差分正演模拟,对以下几种情形进行了研究:(1)低序级断层与埋深、主频以及信噪比之间的关系;(2)观测系统对断层的影响;(3)物性差异产生的假断层问题;(4)大断层衍生出小断层的正演问题;(5)断层破碎带的影响以及断层封堵带含流体的影响.在上述理论模型正演分析的基础上,根据胜利油田典型构造带的地震剖面建立速度模型,研究了不同组合模式的低序级断层的识别能力,最后分析了波动方程正演模拟和褶积合成地震记录的区别.通过对低序级断层正演模拟特征的分析,得出了不同资料质量、不同地质情况以及不同组合模式下,能够准确识别的断层的极限.理论上能够识别的断层最小断距为7 m左右,最小可能会达到5 m,子波主频适当提高,数据采集时炮点和检波点越密集,道间距越小,多个断层的横向或纵向间隔越大,断层的落差越大时,越能够准确地定位断点并确定断层位置.本文研究成果对油田科研生产中低序级断层的正确判别以及提高断层检测方法的可信度方面具有重要意义. 相似文献
33.
34.
E.H. Timothy Whitten 《Proceedings of the Geologists' Association. Geologists' Association》2010,121(3):249-251
The special significance of unanticipated extreme data (in space and time), especially for both genetic and economic predictions, is emphasised with reference to numerous dissimilar geological examples. However, commonly, data for measured variables falling near, or beyond, the tails of unimodal distribution curves have not been incorporated in inverse or forward models used previously in the earth sciences. 相似文献
35.
Kui Xiang Kjersti Solberg Eikrem Morten Jakobsen Geir Nvdal 《Geophysical Prospecting》2022,70(1):3-18
We have derived a convergent scattering series solution for the frequency-domain wave equation in acoustic media with variable density and velocity. The convergent scattering series solution is based on the homotopy analysis of a vectorial integral equation of the Lippmann–Schwinger type. By using the Green's function and partial integration, we have derived the vectorial integral equation of the Lippmann–Schwinger type that involves the pressure gradient field as well as the pressure field from the wave equation. The vectorial Lippmann–Schwinger equation can in principle be solved via matrix inversion, but the computational cost of matrix inversion scales like , where is the number of grid blocks. The computational cost can be significantly reduced if one solves the vectorial Lippmann–Schwinger equation iteratively. A simple iterative solution is the Born series, but it is only convergent when the scattering potential is sufficiently small. In this study, we have used the so-called homotopy analysis method to derive an iterative solution for the vectorial Lippmann–Schwinger equation which can be made convergent even in strongly scattering media. The computational cost of our convergent scattering series scales as . Our algorithm, which is based on the homotopy analysis method, involves a convergence control operator that we select using hierarchical matrices. We use a three-layer model and a resampled version of the SEG/EAGE salt model to show the performance of the developed convergent scattering series. 相似文献
36.
37.
38.
In order to investigate the ability of numerical techniques in computing seismic displacement fields, a forward problem of dislocation theory is first solved by both analytical and numerical techniques. Convergency of the numerical solution and a comparison with the results of a well-known analytical solution are presented for a particular problem. The results are then used when the numerical technique is applied to the same problem without any information on the dislocation source. The latter results may be applied in an inverse dislocation problem. Numerical techniques are in particular expected to be flexible enough to (1) include internal discontinuities, (2) apply geodetic observations as boundary conditions and (3) model lateral, in addition to radial, material heterogeneities. A model with lateral variation of elastic parameters is considered in the last problem.
Acknowledgments.The authors are most grateful to Y. Okada, National Research Institute for Earth Science and Disaster Prevention, Japan, for providing the Fortran code of his analytical solution. 相似文献
39.
40.