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Few density values for these upper crustal rocks lie above 3.3 g/cm3.3
I D = relative density values.
The ROC analysis is based on optical density values.
Landslide number density values increase with the slope angle.
Increasing MoO3 doping content was found to reduce density values.
The crosswinds are derived simultaneously with the neutral density values.
These density values obtained from samples represent the gross average.
Density values for the different units and corresponding references.
Power density values did not follow the same trend.
Chironomidae density values recorded at each sampling time were used.
This produced very low snow density values [14, 24].
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