Potential fields are passive methods. They are based on the measurement of the Earth’s natural gravimetric and magnetic fields. In gravimetry, geophysicists measure the vertical component of the gravitational acceleration vector with great precision. In the case of magnetism, it is possible to measure the three components of the magnetic field vector or, more commonly, a single component called the total field. It refers to the direction of the main field that originates in the liquid outer core of the Earth…
The Italian EAGE-SEG Sectioninterviewed Massimo Fervari about the current applications and future perspectives onSeismic Inversion techniques, a technical topic with enormous implicationson the E&P activities of Energy Companies.Seismic Inversion has several applications and Massimo’s brain is certainly among the most passionate ones to pick.
Simon Blondel, Angelo Camerlenghi, Anna Del Ben When we talk about controversial topics in geosciences, the Mediterranean Salt Giant (MSG) and its origin is one which comes immediately to mind. Since the discovery of Messinian evaporites under the Mediterranean...
University of Pisa Geophysical Society, SEG Student Chapter The Student Chapter SEG of the Geophysical Society of Pisa was founded in 2009 with the aim of divulging and improving changes in Geophysical exploration, supporting the collaboration between university and...
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