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APPLIED GEOPHYSICS  2021, Vol. 18 Issue (2): 145-158    DOI: 10.1007/s11770-021-0890-6
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Efficient modeling of the gravity anomaly caused by a sedimentary basin with lateral variable density contrast and its application in basement relief estimation
Feng Xu-Liang♦1,2, Liu Sheng-Rong 3, and Shen Hong-Yan 1,2
1. School of Earth Sciences and Engineering, Xi’an Shiyou University, Xi’an 710065, China.
2. Shaanxi Key Laboratory of Petroleum Accumulation Geology, Xi’an Shiyou University, Xi’an 710065, China.
3. Xi’an Center of Geological Survey (Northwest China Center for Geoscience Innovation), Xi’an 710054, China.
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Abstract The forward calculation of gravity anomalies is a non-negligible aspect contributing to the time consumption of the entire process of basement relief estimation. In this study, we develop a fast hybrid computing scheme to compute the gravity anomaly of a basement. We use the vertical prism source equation in a given region R centered at a certain gravity observation point and the vertical line source equation outside R to derive the gravity anomaly. We observe that the computation with the vertical line source equation is much faster than that of the vertical prism source equation, but the former is slightly inaccurate. Therefore,our method is highly efficient and able to avoid the errors caused by the low accuracy of the vertical line source equation near the observation point. We then derive the general principle of choosing the size of R via a series of prism model tests. Our tests on the gravity anomaly over the Los Angeles Basin confirm the correctness of our proposed forward strategy. We modify Bott’s method with an accelerating factor to expedite the inversion procedure and presume that the density contrast between the sediments and the basement in a sedimentary basin varies laterally and can be obtained using the equivalent equation. Synthetic data and real data applications in the Weihe Basin illustrate that our proposed method can accurately and effi ciently estimate the basement relief of sedimentary basins.
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Key wordsgravity anomaly   basement relief   fast forward   inversion   lateral variable density contrast     
Received: 2020-05-08;
Fund:

This work is supported by the National Natural Science Foundation of China (41904115).

Corresponding Authors: Feng Xu-Liang (Email: fxlchd@163.com)   
 E-mail: fengxl@xsyu.edu.cn
About author: Feng Xu-Liang obtained a Bachelor ’s degree i n Prospect in g Technology and Engineering from Chang’an University i n 2011and a Ph.D . degreei n Earth Exploration and Information Technology from Chang’an University in 2016. He works as a lecturer and Master’s Supervisor in the School of Earth Sciences and Engineering at Xi’an Shiyou University. His main research interests include gravitational and magnetic exploration and tectonic geophysics.Email: fxlchd@163.com, fengxl@xsyu.edu.cn
Cite this article:   
. Efficient modeling of the gravity anomaly caused by a sedimentary basin with lateral variable density contrast and its application in basement relief estimation[J]. APPLIED GEOPHYSICS, 2021, 18(2): 145-158.
 
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