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Therefore, this correlation shows that the maximum source depth is ~2 km, but that the ash from shallow levels (~2 km to near the surface) is more abundant.
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For this figure we have used the maximum estimated source depth where a range of possible values have been evaluated, or where multiple depths have been suggested for the same deformation events.
There is a peak in the number of displacement episodes in our study that suggest a maximum deformation source depth of 4-5 km (Fig. 2C), and only half of the deformation signals were thought to be deeper than this.
If the gradient is constant over the depth range, then v can be further simplified as v ∝ p(s) − p(g), where p(s) and p(g) denote the pore pressures at the 222Rn source depth (the maximum depth from which 222Rn can reach the detector) and the ground surface, respectively; p(g) is almost constant (=1 atm) despite small fluctuations with weather conditions, and p(s) is variable.
The depth for which this correlation reaches maximum (the best matching) is chosen as the estimated source depth.
(2) To improve the sensitivity to source depth.
It is important to consider that both CAM and TIA provide maximum estimates for z: the TIA provides the depth of intersection points, which have to be considered as maximum possible depth of the source.
This simulates the cessation of gas generation after the source rock reached its maximum buried depth.
Maximum depth was the greatest water depth measured among transects.
Bathymetric data from 105 lakes were compiled from existing sources and were used as validation for the classification results based on an expected maximum ice depth of 1.6 m.
Maximum frost depth varies with climate and topography.
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