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The obtained basal depth of a magnetic source is assumed to be the CPD.
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Aeromagnetic data of the Ikogosi warm spring region was used to calculate the basal depth of the magnetic layer (Curie point depth) in the region.
Aeromagnetic data have been used in geothermal investigations to estimate basal depths of the Curie point magnetic layer (Abraham et al. 2014) and to assess concealed structure (Maystrenko et al. 2014).
Then the basal depth (zb) of the magnetic source is calculated from Equation 2.
For this purpose, the basal depth (depth to the bottom) of a magnetic source from aeromagnetic data is considered to be the CPD (Dolmaz et al. [2005]).
Okubo and Matsunaga (1994) showed that forward modelling of magnetic profile data does not produce unique solutions of the basal depth, as at least, three different depth models were deduced from the modeling of one profile.
The basal depth, CPD, Z b is computed using Eq. (3), where Z o is the depth to the centroid and Z t is the depth to the top of a geological body (Ravat et al. 2007; Eletta and Udensi 2012).
Ross et al. ([2006]) applied a comparison of estimated basal depths with heat flow values and thickness of the seismogenic crust to draw conclusions that these parameters provided additional confidence in the basal depths they determined.
A 24-gauge needle attached to a Hamilton syringe was inserted into the right basal ganglia to a depth of 3.5 mm and then withdrawn 0.5 mm to make space for tumor cell accumulation.
In our series, the most reliable morphological parameters to differentiate adenoid basal hyperplasia from adenoid basal carcinoma were the depth of the lesion and the size of the lesion nests.
Relative dominance (RDom): total basal area of a species/basal area of all species × 100.
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