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物探与化探  1988, Vol. 12 Issue (2): 81-84    
  论文 本期目录 | 过刊浏览 | 高级检索 |
试论郯—庐“Y”型三叉裂谷
王金星, 史秀琴
浙江地矿局物化探大队
A TENTATlVE DISCUSSION ON TANCHENG-LUJIANGY-SHAPED TRIPURCATE RIFT
Wang Jinxing, Shi Xiuqin
Genphysical and Geochemical Prospecting Party, Bureau of Geology and MineralResources of Zhejiang Province
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摘要 

本文根据卫星重力资料和地面重力资料,研究了地幔对流产生的应力场,并结合地质、地球物理资料的综合分析,对郯—庐裂谷带的具体位置、形成机理及其演化规律都作了探讨。在此基础上提出了郯—庐“Y”型三叉裂谷的看法。

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Abstract

Based on satellite gravity data and ground gravity data, the present paperdeals with the stress field caused by mantle convection and, in combinationwith an integrated analysis of geologic and geophysical data, makes an inves-tigation into the location, formation mechanism and evolutionary regularity ofthe Tancheng-Lijiang rift belt. On such a basis, the view of Tancheng-Lujiang Y-shaped trifurcate rift is presented.

     出版日期: 1988-04-24
引用本文:   
王金星, 史秀琴. 试论郯—庐“Y”型三叉裂谷[J]. 物探与化探, 1988, 12(2): 81-84.
Wang Jinxing, Shi Xiuqin. A TENTATlVE DISCUSSION ON TANCHENG-LUJIANGY-SHAPED TRIPURCATE RIFT. Geophysical and Geochemical Exploration, 1988, 12(2): 81-84.
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https://www.wutanyuhuatan.com/CN/      或      https://www.wutanyuhuatan.com/CN/Y1988/V12/I2/81

[1] A. C. Waguer and F. J. Lerch; Improvement in the Geopotential derived from Satellite and Surface data(GEM7 and 8),Journal of Geoyhysical Research, Vol. 82, No. 5, 1977.
[2] 5. K. Runcorn;Flow in the hfantle Inferred from the Low Degree Harmonics of the Geopotential, Geophysical Journal, 14, 1967.
[3] 黄培华、付容珊:应用卫星重力数据研究全球岩石层下地慢流应力场,中国科技大学学报,12卷,2期,1982.
[4] 黄培华:中国岩石层底面地慢对流状态的探讨,地球物理学报,26卷,1期,1983.
[5] 许志琴:谈谈裂谷,地质评论,26卷,3期,1980.
[6] 荻原幸男:重力异常和地慢对流,测地学会志(日本),1972年,17卷,4号。

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