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In the absence of detailed gravity and seismic modeling studies along this profile, the MT model presented here can be explained taking clues from other MT studies carried out elsewhere.
Several similarities between the results obtained using this MT model and those from earlier gravity, seismic (Tewari and Kumar, 2003), and MT models (Gokarn et al., 2001) are discussed in the following section.
MT model is also constrained using residual gravity data and corroborates well with the MT data.
Geologic model corroborates well with the MT model described later.
Similarly, the MT model used here and earlier MT model reported by Gokarn et al. (2001) both found deep crustal conductors (C1 and C2 in Fig. 5(a)).
The seismic and gravity models (shown in Fig. 2) are superposed over the MT model.
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In addition, after exposure of oMWCNTs to Cd-MT model mice, oMWCNTs could affect the synthesis of Cd-MT.
The results of Figure 5 showed the distribution of Cd content in liver, kidney, and blood after exposure of different doses of oMWCNTs to Cd-MT model mice.
For the exposure group with 750 μg/mouse oMWCNTs, the ALT content showed no difference with the Cd-MT model group.
This may be the reasons that the elution curve shows two different strength peaks for the Cd-MT model and coexposure groups).
The livers were harvested at 4 h after intravenous exposure of oMWCNTs (about 500 μg/mouse) to Cd-MT model (4 mice) and normal mice (4 mice), respectively.
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