Just for the sake of humouring me could you possibly provide me some equations please?

Calculate a medium between the compounds of the Siberian Traps and that of the Uluru sandstone to provide a measurement of the aggregate mantle solution that will have provided suspension between either collision core?

From this calculate a specific temperature of mantle materials that may have provided super-viscosity to the core collision with the pressure provided by the momentum(straight-line velocity+AM) in each core+the characteristics of this material at that temperature?

From this define the likelihood of the scenario I have provided being accurate?

In lieu of the required core samples this may satisfy my curiosity somewhat…….

Am also wondering what the strength of the magnetic fields of either body will have been at the rates they were spinning?

Might a stronger EM field have provided greater capacity to the iron cores to withstand the collision?

Postpocelipse said:

Am also wondering what the strength of the magnetic fields of either body will have been at the rates they were spinning?

Might a stronger EM field have provided greater capacity to the iron cores to withstand the collision?

Would less ferrous metals in the core separate from highly magnetic compounds with that degree of centrifugal force?

K. Scratch this since it’s starting somewhere complex………