1D inversion and resolution analysis of marine CSEM data

被引:28
|
作者
Christensen, Niels B. [1 ]
Dodds, Kevin
机构
[1] Univ Aarhus, Dept Earth Sci, Aarhus, Denmark
[2] CSIRO Petr, Kensington, NSW, Australia
关键词
D O I
10.1190/1.2437092
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present results from an investigation into I D inversion of controlled-source electromagnetic (CSEM) data. Based on inspection of a data set, we formulate a simple empirical noise model described by a few pragmatically determined parameters. We also investigate the effects of transmitter height above the seafloor and include the data uncertainty resulting from varying transmitter height in our noise model. Based on the noise model and assumptions about the available data, we analyze model parameter uncertainty estimates derived from the a posteriori model covariance matrix for a resistive layer buried at depth. We find that the layer parameters uncertainty primarily depends on the depth of burial and the thickness of the layer. We then formulate quantitative bounds for these parameters, within which we have a small uncertainty of the parameters of the resistive layer. The depth of burial and the transverse resistance of the layer become better determined the higher its resistance. We invert a field data set with multilayer and four-layer models and find a resistive layer at a depth of 1500-1600 In below the seafloor. Seismic results from the area indicate a depth of 2000 m.
引用
收藏
页码:WA27 / WA38
页数:12
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