Transdimensional Bayesian inversion of time-domain airborne EM data

2018 ◽  
Vol 15 (2) ◽  
pp. 318-331
Author(s):  
Zong-Hui Gao ◽  
Chang-Chun Yin ◽  
Yan-Fu Qi ◽  
Bo Zhang ◽  
Xiu-Yan Ren ◽  
...  
Author(s):  
Yanfu Qi ◽  
Xiu Li ◽  
Changchun Yin ◽  
Huaiyuan Li ◽  
Zhipeng Qi ◽  
...  
Keyword(s):  

2021 ◽  
pp. 104317
Author(s):  
Mengli Tao ◽  
Changchun Yin ◽  
Yunhe Liu ◽  
Yang Su ◽  
Bin Xiong

2016 ◽  
Vol 13 (4) ◽  
pp. 701-711 ◽  
Author(s):  
Yun-He Liu ◽  
Chang-Chun Yin ◽  
Xiu-Yan Ren ◽  
Chang-Kai Qiu
Keyword(s):  

2019 ◽  
Author(s):  
Yanfu Qi* ◽  
Xiu Li ◽  
Changchun Yin ◽  
Zhipeng Qi ◽  
Naiquan Sun ◽  
...  

Author(s):  
M.S. McMillan ◽  
D.W. Oldenburg ◽  
E. Haber ◽  
C. Schwarzbach ◽  
E. Holtham

Geophysics ◽  
2021 ◽  
pp. 1-45
Author(s):  
Hai Li ◽  
Guoqiang Xue ◽  
Wen Chen

The Bayesian method is a powerful tool to estimate the resistivity distribution and associate uncertainty from time-domain electromagnetic (TDEM) data. As the forward simulation of the TDEM method is computationally expensive and a large number of samples are needed to globally explore the model space, the full Bayesian inversion of TDEM data is limited to layered models. To make high-dimensional Bayesian inversion tractable, we propose a divide-and-conquer strategy to speed up the Bayesian inversion of TDEM data. First, the full datasets and model spaces are divided into disjoint batches based on the coverage of the sources so that independent and highly efficient Bayesian subsampling can be conducted. Then, the samples from each subsampling procedure are combined to get the full posterior. To obtain an asymptotically unbiased approximation to the full posterior, a kernel density product method is used to reintegrate samples from each subposterior. The model parameters and their uncertainty are estimated from the full posterior. The proposed method is tested on synthetic examples and applied to a field dataset acquired with a large fixed-loop configuration. The 2D section from the Bayesian inversion revealed several mineralized zones, one of which matches well with the information from a nearby drill hole. The field example shows the ability of Bayesian inversion to infer reliable resistivity and uncertainty.


1998 ◽  
Vol 29 (1-2) ◽  
pp. 16-23 ◽  
Author(s):  
Richard Lane ◽  
Caleb Plunkett ◽  
Antony Price ◽  
Andy Green ◽  
Hu Yiding
Keyword(s):  

Geophysics ◽  
1969 ◽  
Vol 34 (5) ◽  
pp. 729-738 ◽  
Author(s):  
P. H. Nelson ◽  
D. B. Morris

The secondary magnetic field induced by a time‐domain, airborne EM system is calculated by transforming the tabulated mutual impedances of two magnetic dipoles above an earth of homogeneous or layered resistivity structure. The computational procedure is extended to produce response curves useful in interpreting data from a particular system, the Barringer Input system. It is demonstrated that the apparent resistivity can be estimated through use of the receiver channel ratios, a method which is independent of absolute system calibration. Layered earth calculations indicate to what extent conductive overburden cases can be readily distinguished, in terms of the conductivity‐thickness parameter, but separate interpretation of layer resistivity and thickness will require an amplitude‐calibrated flight system.


2016 ◽  
Vol 134 ◽  
pp. 11-22 ◽  
Author(s):  
Changchun Yin ◽  
Yanfu Qi ◽  
Yunhe Liu ◽  
Jing Cai

2021 ◽  
pp. 104357
Author(s):  
Wang Haoman ◽  
Liu Yunhe ◽  
Yin Changchun ◽  
Ren Xiuyan ◽  
Cao Jin ◽  
...  

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