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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Arctic Ocean
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Primary terms
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Arctic Ocean
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Barents Sea (4)
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Arctic region (1)
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Atlantic Ocean
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North Atlantic
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Gulf of Mexico (2)
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North Sea
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Troll Field (1)
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Australasia
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Australia
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Queensland Australia
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Cannington Deposit (1)
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South Australia
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Gawler Craton (1)
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Canada
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Eastern Canada
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Newfoundland and Labrador
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Labrador
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Voisey's Bay Deposit (1)
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Newfoundland (1)
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Ontario (1)
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ground water (1)
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mineral exploration (6)
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North America
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Canadian Shield
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Superior Province
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Abitibi Belt (1)
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oil and gas fields (2)
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petroleum (6)
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Precambrian
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upper Precambrian
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United States
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sedimentary rocks
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sedimentary rocks
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chemically precipitated rocks
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evaporites
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salt (1)
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Recovering 3D salt dome by gravity data inversion using ResU-Net++
Joint focusing inversion of marine controlled-source electromagnetic and full tensor gravity gradiometry data
Adaptive multinary inversion of gravity and gravity gradiometry data
A hybrid finite-difference and integral-equation method for modeling and inversion of marine controlled-source electromagnetic data
Anisotropic 3D inversion of towed-streamer electromagnetic data: Case study from the Troll West Oil Province
3D joint inversion of geophysical data with Gramian constraints: A case study from the Carrapateena IOCG deposit, South Australia
3D inversion of airborne electromagnetic data
3D migration for rapid imaging of total-magnetic-intensity data
Inverting airborne geophysical data for mega-cell and giga-cell 3D Earth models
Large-scale 3D inversion of marine magnetotelluric data: Case study from the Gemini prospect, Gulf of Mexico
Electromagnetic geophysics: Notes from the past and the road ahead
Electrical and Electromagnetic Methods: Electromagnetic geophysics: Notes from the past and the road ahead
Abstract During the last century, electrical geophysics has been transformed from a simple resistivity method to a modern technology that uses complex data-acquisition systems and high-performance computers for enhanced data modeling and interpretation. Not only the methods and equipment have changed but also our ideas about the geoelectrical models used for interpretation have been modified tremendously. This paper describes the evolution of the conceptual and technical foundations of EM methods. It outlines a framework for further development, which should focus on multitransmitter and multireceiver surveys, analogous to seismic data-acquisition systems. Important potential topics of future research efforts are in the areas of multidimensional modeling and inversion, including a new approach to the formulation and understanding of EM fields based on flux and voltage representation, which corresponds well to geophysical experiments involving the measurement of voltage and flux of electric and magnetic fields.