| 大足重力高及其复合成因 |
| |
| 引用本文： | 葛双成,周熙襄.大足重力高及其复合成因[J].物探与化探,1991,15(1):25-30. |
| |
| 作者姓名： | 葛双成 周熙襄 |
| |
| 作者单位： | 浙江省石油地质研究所
(葛双成)，成都地质学院(周熙襄) |
| |
| 摘 要： | 在综合分析大量地质、航磁、重力,大地电磁测深及地震勘探、密度测定等成果的基础上,我们建立了川中地区的地质—地球物理模型.进而利用正演计划方法分析以大足为中心的川中重力异常,最后提出了大足重力高复合成因的新观点.
|
| 关 键 词： | 重力勘探 重力高 大足 复合成因 |
THE DAZU GRAVITY HIGH AND ITS COMPOSITE ORIGIN |
| |
| Institution: | 1. Zhejiang Institute of Petroleum Geology;
2. Chengdu College of Geology |
| |
| Abstract: | Based on an integrated analysis of large quantities of outcomes obtainedin such fields as geology, aeromagnetic survey, gratity, telluric electromagneticsounding, seismic exploration and density determination, we have established a geological-geophysical model for Central Sichuan area. With the direct calculation method, we have analysed the Central Sichuan gravity anomaly centering on Dazu. Finally, a new viewpoint is put forward concerning the composite origin of the Dazu gravity high. |
| |
| Keywords: | |
| 本文献已被 CNKI 维普 等数据库收录！ |
| 点击此处可从《物探与化探》浏览原始摘要信息 |
| 点击此处可从《物探与化探》下载免费的PDF全文 |
|
