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物探与化探  1991, Vol. 15 Issue (1): 25-30    
  论文 本期目录 | 过刊浏览 | 高级检索 |
大足重力高及其复合成因
葛双成1, 周熙襄2
1. 浙江省石油地质研究所;
2. 成都地质学院
THE DAZU GRAVITY HIGH AND ITS COMPOSITE ORIGIN
Ge Shuangcheng1, Zhou Xixiang2
1. Zhejiang Institute of Petroleum Geology;
2. Chengdu College of Geology
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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.

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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.

     出版日期: 1991-02-24
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.
Ge Shuangcheng, Zhou Xixiang. THE DAZU GRAVITY HIGH AND ITS COMPOSITE ORIGIN. Geophysical and Geochemical Exploration, 1991, 15(1): 25-30.
链接本文:  
https://www.wutanyuhuatan.com/CN/      或      https://www.wutanyuhuatan.com/CN/Y1991/V15/I1/25

[1] 李立、金国元:1987,物探与化探,No. 3.
[2] 赵珠、张润生:1987,地震研究,No. 2.
[3] 康义昌,1986,石油实脸地质,No. 3.

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