Resolution assessment of the three-dimensional acquisition geometry of the Anhui experiment in "Geoscience Yangtze Plan" |
| |
| Authors: | Yiqing Li Xiaofeng Tian |
| |
| Institution: | Geophysical Exploration Center, China Earthquake Administration, Zhengzhou450002, China;Geophysical Exploration Center, China Earthquake Administration, Zhengzhou450002, China |
| |
| Abstract: | According to the actual observation conditions of the Yangtze River valley from Anqing city to Maanshan city, we designed the 3D acquisition geometry, and applied the multi-scale checkerboard semblance analysis to assess the preliminary resolution of the designed observation. The checkerboard semblance tests use the refraction and reflection travel-time simultaneous inversion algorithm to quantitatively provide both resolution assessment of velocity structure and Moho topography. The multi-scale checkerboard semblance recovery results show that while the checkerboard semblance threshold value is 0.5, the preliminary resolution of the designed acquisition geometry is better than 10 km in the upper crust (the depth is less than 10 km), around 15 km in the mid-crust (the depth is 10?25 km), and better than 20 km in the lower crust (the depth is 25?33 km). The preliminary tomographic resolution for the Moho topography is about 20 km in the ray-path coverage area beneath the acquisition geometry. While the checkerboard semblance threshold value is 0.75, the preliminary resolution is 20 km in the upper crust, around 20?25 km in the mid-crust and 25 km in the lower crust. And the preliminary tomographic resolution for the Moho topography is better than 30 km in the ray-path coverage area beneath the acquisition geometry. These non-linear checkerboard tests reveal that the designed acquisition geometry is suitable to image the crustal velocity structure of the Yangtze River valley in the Anhui province. |
| |
| Keywords: | artificial seismic source air gun 3D seismic tomography acquisition geometry resolution assessment |
| 本文献已被 万方数据 等数据库收录！ |
| 点击此处可从《Earthquake Science》浏览原始摘要信息 |
| 点击此处可从《Earthquake Science》下载免费的PDF全文 |
|
