A new method to determine the start depth in gravity anomaly inversion
OriginalPaper|Updated:2023-05-16
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A new method to determine the start depth in gravity anomaly inversion
A new method to determine the start depth in gravity anomaly inversion
海洋湖沼学报(英文)1998年16卷第4期 页码:381-384
Affiliations:
Institute of Oceanology
Author bio:
Funds:
Contribution No. 3370 from the Institute of Oceanology, Chinese Academy of Sciences.;Project 49625609 supported by NSFC, and Young Scientist Lab. of Submarine Hydrothermal Activity Research.
A new method to determine the start depth in gravity anomaly inversion[J]. 海洋湖沼学报(英文), 1998,16(4):381-384.
Xi-wu, L. A new method to determine the start depth in gravity anomaly inversion., Chin. J. Ocean. Limnol. 16, 381–384 (1998). https://doi.org/10.1007/BF02844938
A new method to determine the start depth in gravity anomaly inversion[J]. 海洋湖沼学报(英文), 1998,16(4):381-384. DOI: 10.1007/BF02844938.
Xi-wu, L. A new method to determine the start depth in gravity anomaly inversion., Chin. J. Ocean. Limnol. 16, 381–384 (1998). https://doi.org/10.1007/BF02844938DOI:
A new method to determine the start depth in gravity anomaly inversion
摘要
Abstract
The start depth in gravity anomaly inversion is discussed in this paper
and a new method called “test comparing method” is presented to determine the start depth when both boring data and seismic data are not available. Anticline and syncline density interface models are designed to test the method; the calculated result agreed well with the designed value
which proved that the new method can be used to determine the start depth in the gravity anomaly inversion when boring data and seismic data are not available.
关键词
Keywords
references
Wang Xingtai, Li Xiaoqin, Sun Renguo et al., 1996. The inversion of resistivity sounding curve using genetic algorithms.Acta Geophysica Sinica 39(2): 297–285. (in Chinese with English Abstract)
Liu Yuanlong, Wang Qianshen, 1977. Inversion of gravity data by using a method of “compressed mass plane” to estimate crustal structure.Acta Geophysica Sinica 20(1): 69–80. (in Chinese with English Abstract)
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