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These geochemical surface prospecting methods are not applicable to the large majority of petroleum reservoirs, which do not have leakage to the surface.
For example, features of back scarp (scarp, sharp slope or cliff), landslide valley or collapsed valley (depression or gully), landslide mass (hilly block), landslide bench and sliding surfaces can be known by using the foregoing geophysical prospecting methods.
During each data acquisition, it is required that 3D seismic prospecting, electrical prospecting and ground penetrating radar prospecting are implemented simultaneously and survey lines deployed in different prospecting methods have overlapping sections.
The original Vs models derived by seismic prospecting methods (Raptakis. Soil Dynamics and Earthquake Engineering 2012 34: 69–77), similarly performed prior to and after preloading, were used for site amplification estimates as a function of frequency.
Gamma-ray spectrometry is one of the most cost-effective prospecting methods for investigating anomalies in potassium, uranium, thorium and alteration indexes associated with hydrothermal and radioactive ore deposits.
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Surface geochemical prospecting method was applied in Deccan Syneclise for evaluation of hydrocarbon resource potential of the basin.
In this study, we propose a natural source prospecting method to directly assess the depths and distributions of oil layers.
A new geophysical borehole prospecting method has been taken into use at the Geological Survey of Finland (GTK), known as the radiofrequency imaging method (RIM).
Helicopter transient electromagnetic (TEM) method is a kind of common geophysical prospecting method, widely used in mineral detection, underground water exploration and environment investigation.
The solution for the electrical potential arising from an electrical current flowing into the ground from a point source of current (a grounded electrode) is the starting theoretical point for the resistivity prospecting method.
Gravimetry is generally used as a prospecting method for underground structures at various scales (volcanoes, geothermal, gas and oil reservoirs, mineral resources, stratigraphy) and contributes to the static imagery in addition to other methods like magneto-tellurics (e.g., Volpi et al. 2003, Newman et al. 2008; Geiermann and Schill 2010) or seismics (Concha et al. 2010; Sanjuan et al. 2010).
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