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Improved controlled source audio‐frequency magnetotelluric method apparent resistivity pseudo‐sections based on the frequency and frequency–spatial gradients of electromagnetic fields
Author(s) -
Zhang Ming,
Farquharson Colin G.,
Liu Changsheng
Publication year - 2021
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1111/1365-2478.13059
Subject(s) - magnetotellurics , electrical resistivity and conductivity , geology , economic geology , regional geology , field (mathematics) , instrumentation (computer programming) , frequency domain , audio frequency , geophysics , electrical resistivity tomography , environmental geology , gemology , electromagnetic field , acoustics , engineering geology , hydrogeology , computer science , seismology , physics , mathematics , tectonics , geotechnical engineering , volcanism , metamorphic petrology , quantum mechanics , pure mathematics , computer vision , operating system , sound pressure
Although most electromagnetic data can be inverted to actual resistivity, ways of quickly getting a real‐time interpretation of a data set are still valuable. Such methods are useful when we are testing instrumentation or assessing data quality during a survey, or when we need to get a general understanding of the geological structure during a field survey. Apparent resistivity is a good way to satisfy these desires. However, one of the disadvantages of apparent resistivities is that the traditional apparent resistivity formulations are poor at recognizing boundaries, mainly because abnormal responses get stretched into deeper parts of the image (a shadow effect). In order to improve the recognition ability of boundaries, we propose improved apparent resistivity pseudo‐sections based on the formulae for the frequency and frequency–spatial gradients of the fields in the far‐field region of frequency‐domain controlled‐source audio‐frequency magnetotelluric surveys. The new pseudo‐sections are found to be better than those produced from a traditional method when applied to a number of 3‐D examples. The performance of this apparent resistivity method is closely related to using an appropriate transmitter–receiver distance: when a proper value is used, good results can be obtained in which the horizontal locations of vertical boundaries and the positions of top and bottom boundaries can be identified clearly. Finally, the usefulness of the proposed method for practical applications is evaluated with a field‐data example, for which the results of the proposed apparent resistivity imaging method are compared with traditional apparent resistivities, as well as with the results from a 2‐D inversion of DC resistivity data from the same survey line and with what is known about the geology of the area. This comparison demonstrates the improved capabilities of the new apparent resistivities over traditional approaches, including an improved capability to accurately reveal the bottoms of targets.