| ??????ж??????????????????? |
| |
| 引用本文： | 柯小平,王勇,许厚泽.??????ж???????????????????[J].大地测量与地球动力学,2009,29(2):19-23. |
| |
| 作者姓名： | 柯小平 王勇 许厚泽 |
| |
| 作者单位： | 中国科学院测量与地球物理研究所,武汉,430077 |
| |
| 基金项目： | 国家自然科学基金，地球空间环境与大地测量教育部重点实验室测绘基础研究基金 |
| |
| 摘 要： | ?????????????????????????????????????????????IGMAS????????????????????????????????????????????о????????????ж?????????????????????????????????????????????????????????????ж??????????????????????????????μ????????????????????????????и?????????仯??????????????е?????μ???????????????????????е??????????????????????????????С?????????????μ????????????????????????
|
| 关 键 词： | ??????? ??? ????? ???? ???? |
FORWARD SIMULATION OF GEOID IN MIDDLE-SHORT WAVELENGTH IN TIBETAN PLATEAU |
| |
| Ke Xiaoping,Wang Yong,Xu Houze.FORWARD SIMULATION OF GEOID IN MIDDLE-SHORT WAVELENGTH IN TIBETAN PLATEAU[J].Journal of Geodesy and Geodynamics,2009,29(2):19-23. |
| |
| Authors: | Ke Xiaoping Wang Yong Xu Houze |
| |
| Institution: | Institute of Geodesy and Geophysics;CAS;Wuhan 430077 |
| |
| Abstract: | On the basis of the three-dimensional(3D) layered models of crustal structures from the 3D forward simulation of gravity in Tibetan plateau and by use of the software of IGMAS the geoidal undulations caused by the inhomogeneity of three-dimensional crustal structures in Tibetan plateau are simulated.The study shows that,the geoid in middle-short wavelength is produced by the inhomogeneity of density between each layer within the crust in Tibetan plateau,it means that the interface undulation is the main mec... |
| |
| Keywords: | geoid simulation Tibetan plateau gravity crustal structure |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
| 点击此处可从《大地测量与地球动力学》浏览原始摘要信息 |
| 点击此处可从《大地测量与地球动力学》下载免费的PDF全文 |
