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Fig. 10 Mars core structure when stratification and crystallization of an inner core occur simultaneously.
As demonstrated in Fig. 12a, at common square CFT columns, buckling and separation of steel shell from concrete core occur at middle point of length of column.
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This indicates the anisotropic deposition of CdS on the core occurs.
It indicates that the cracking of HPG core occurs around 425 °C (Fig. 4a).
Figure 5 shows that crystallization at the base of Mars' core occurs only at low temperatures below ∼1420 K.
In the Nobeoka Thrust, a single fault core occurs between the hanging wall and footwall, but within each wall, multiple damage zones are localized near the fault core.
We propose that at the short refluxing times, incomplete passivation of the core occurs similarly to the oxidation observed for the CdSe core partially coated with ZnS [18].
MY13 pointed out that the essential change of the number of convection cores and distance to the nearest convective core occurred around the 2 km grid spacing as a global mean (Fig. 8).
However, a stronger coupling between the Au shell and the Au core occurs in the near field at the Fano dip inducing destructive interference, compared to the field at the dipolar bonding mode.
This post-peak vertical exhumation of the central core occurred after ~505 Ma was accommodated by brittle extensional detachments at high stratigraphic levels with km-scale omission of crustal section.
The greatest density of AhR enrichment associated with a DRE core occurred within the proximal promoter.
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