Review:
Magnetotellurics
overall review score: 4.2
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score is between 0 and 5
Magnetotellurics is a geophysical method that uses natural electric and magnetic fields to determine the electrical resistivity structure of the Earth's subsurface.
Key Features
- Non-invasive geophysical method
- Provides information on subsurface resistivity
- Used for mapping structures such as faults, mineral deposits, and groundwater
Pros
- Non-destructive imaging of subsurface structures
- Can be used in remote or inaccessible areas
- Useful for mineral exploration and hydrogeological studies
Cons
- Requires specialized equipment and expertise
- Data interpretation can be complex
- Limited resolution at shallow depths