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Figure 3: Model results of thermomechanical processes associated with a xenolith sinking in a granitic magma chamber.
Figure 4: Influence of basic parameters on model results of thermomechanical processes associated with a xenolith sinking in a granitic magma chamber.
Model results of a representative thermoelastic structure include transient temperature and sinusoidal steady state transverse displacement.
Finite element model results of MDT sites are used to validate the approach.
The model results of four different Titan's orbital locations are also presented.
GSM TIP model results of E-region parameters are compared with IRI-2012 model.
The methodology combines numerical model results of the resource with economic assessments in a Matlab-based tool designed ad hoc.
The model results of conventional reactor are validated with the plant data and a reasonable agreement is achieved.
Model results of LIMA (Leibniz Institute Middle Atmosphere Model) are used to reveal tides within the polar summer mesopause region.
Model results of chloride distributions were improved in matching the observed data with the calibrated infiltration rates.
New model results of post-Last Glacial Maximum (LGM) isostatic rebound for this area allow a well-constrained interpretation of acoustic units in terms of sequence stratigraphy.
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