Sentence examples for model density values from inspiring English sources

The model density values returned from both the homogeneous and heterogeneous, geologically constrained geophysical inversion modeling are the key guides for improving the 3D geologic model.

These model density values lie well within the range of geologically reasonable densities for the rock types in the Bradys area.

The geologically constrained geophysical inversion modeling effort presented here returned model density values that lie in the range 1.9 2.8 g/cm3 (Table 1).

One argument to explain this discrepancy is that the Oligocene volcanic units are strongly welded ignimbrites giving rise to the high model density values.

Moving forward, the following questions need to be addressed: (1) Are the model densities consistent with rock density values measured in the Bradys area, and if not, how do the model density values need to be changed?

and (2) How and where can the lithologic boundaries of the 3D geologic model be changed to address inaccurate model density values while at the same time maintain an acceptable level of misfit?

It has to be noted that the consistency between observed and modeled density values will improve when a scale factor for the density model would be estimated and taken into account, which would correct for the higher neutral density values observed for existing density models, which typically is of the order of 20 30% for the selected data period and model (Doornbos, 2011).

In our model, the expected density values were dependent on the number of genes and cis-regulatory elements of each gene.

Therefore, we employed geophysical inversion modeling to find density values for each of the 10 rock units that, collectively, minimize the misfit.

The regional geophysical model was populated with density values by performing 3D heterogeneous inversion modeling (Fullagar and Pears 2007) on the regional gravity data.

The viscosity results are modeled with the free volume theory model in conjunction with density values obtained using the Peng Robinson equation of state (EoS) and the PC-SAFT EoS.