Please excuse my poor phrasing; this has been translated from Spanish.
Although I have no formal background in Earth sciences, I have always been curious about the planet’s geological history. Some years ago, I came across the work of Warren Carey and other proponents of the Expanding Earth theory; however, ever since watching Neal Adams’ videos, I have sought a way to graphically reproduce this model by following oceanic isochron lines. I began using GPlates and PyGplates—and even Blender—but my lack of technical skill prevented me from successfully modifying the Earth’s radius variable (constant).
I recently joined this forum and saw what you have achieved; it meets most of my expectations, though it remains a geometric explanation that accounts for the majority of the deformations.
I would now like to make a proposal:
There is a paleomagnetism database containing samples from across the globe, including data on their age and latitude at the time of formation.
Would it be possible to map some of these samples—organized by continent—to their original discovery sites, run your models backward in time, and determine whether the margin of error is acceptable?
My suggestion would be to select a group of samples from the same time period and see if they align with the expected paleomagnetic latitude.
If the margin of error regarding latitude proves acceptable, it could serve as scientific support for the Expanding Earth theory using paleomagnetic data.
I am not aware if this has been done before.
Best regards,
Patxi Moya