The phrase "above the core" is correct and usable in written English.
It can be used in contexts where you are referring to something that is positioned higher than a central or fundamental part of a system or structure.
Example: "The temperature readings were taken from sensors located above the core of the reactor."
Alternatives: "over the core" or "atop the core".
As you can read between the above, the core confusion is that the Surface 2 depends on Office, and the Windows Store for all its applications, while the Surface Pro does not.
As I discussed above, the core themes at AMNH are very different, and there is a strong emphasis on the taxonomic diversity found throughout our lineage, as well as the role of molecular genetics in the study of human evolution.
As discussed above, the core 'Cercozoa' within 'Rhizaria' do show a sister-group relationship to stramenopiles, though our trees provide only Bayesian support for this result (see Fig. 3).
Another merit is the capability to submerge the PCV and the RPV above the core level.
Above the core and below the crust lies Venus's mantle, making up the bulk of the planet's volume.
Water is injected into hot PbBi above the core, and direct contact boiling takes place in chimneys.
The two strategies I outlined above are the core of a successful retention strategy.
Furthermore, the estimated incompatible trace element ratios of the low-μ142Nd end-member are similar to that of a 4.5 4.4 Ga dense melt that was possibly preserved above the core-mantle boundary.
They vary in thickness from 5 to 40 km just above the core-mantle boundary (CMB) where there is a ~10 30 % seismic velocity reduction (e.g., Garnero et al. 1998).
The geomagnetic main field and its secular variation measured by orbiting satellites and at magnetic observatories correspond to those of the poloidal constituent, whereas the toroidal counterparts, which are bound to the core, are not observable above the core-mantle boundary (CMB).
The new experiments revealed that oceanic crust (the basalt) melts at a lower temperature than surrounding mantle rocks do in the zone just above the core-mantle boundary, 1,800 miles (2,900 km) deep.
