The importance of using geometrical constraints in marine controlled source electromagnetic data inversion

2005 ◽  
Author(s):  
Paolo Dell'Aversana
Keyword(s):  
Controlled Source ◽  
Electromagnetic Data ◽  
Data Inversion ◽  
Geometrical Constraints

Inversion of frequency-domain marine-controlled-source electromagnetic data using genetic algorithm

2017 ◽  
Author(s):  
Mohit Ayani ◽  
Subhashis Mallick ◽  
Jürg Hunziker ◽  
Lucy MacGregor
Keyword(s):  
Genetic Algorithm ◽  
Frequency Domain ◽  
Controlled Source ◽  
Electromagnetic Data

Interpretation of controlled-source electromagnetic data from iron ores under rough topography

2016 ◽  
Vol 124 ◽  
pp. 106-116 ◽  
Author(s):  
Seokmin Oh ◽  
Kyubo Noh ◽  
Soon Jee Seol ◽  
Joongmoo Byun ◽  
Myeong-Jong Yi
Keyword(s):  
Iron Ores ◽  
Controlled Source ◽  
Electromagnetic Data

Seismic wave propagation concepts applied to the interpretation of marine controlled-source electromagnetics

Geophysics ◽  
2015 ◽  
Vol 80 (2) ◽  
pp. E63-E81 ◽  
Author(s):  
Rune Mittet
Keyword(s):  
Seismic Data ◽  
Maxwell Equations ◽  
Seismic Wave Propagation ◽  
Finite Difference Schemes ◽  
Data Types ◽  
Controlled Source ◽  
Electromagnetic Data ◽  
Inverse Transform ◽  
Refraction Seismic ◽  
Marine Csem

Concepts such as reflections, refractions, diffractions, and transmissions are very useful for the interpretation of seismic data. Moreover, these concepts play a key role in the design of processing algorithms for seismic data. Currently, however, the same concepts are not widely used for the analysis and interpretation of marine controlled-source electromagnetic (CSEM) data. Connections between seismic and marine CSEM data are established by analytically transforming the diffusive Maxwell equations to wave-domain Maxwell equations. Seismic data and wave-domain electromagnetic data are simulated with 3D finite-difference schemes. The two data types are similar; however, the wave-domain electromagnetic data must be transformed back to the diffusive domain to properly describe realistic field propagation in the earth. We analyzed the inverse transform from the wave domain to the diffusive domain. Concepts like reflections, refractions, diffractions and transmissions were found to be valid also for marine CSEM data but the properties of the inverse transform favored refracted and guided events over reflected and diffracted events. In this sense, marine CSEM data were found to be similar to refraction seismic data.

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