Well, I figured you're the geologist you might be interested.
I'll see if I can get this right.
Mathematically they have now worked out a way to determine the structure of a solid object using two surface sensors and analyzing the wave forms. So what they are saying (if I read it correctly) is that by analyzing the sensor data they can derive the "complete" or near as given the resolution and sensitivity of the sensors, the internal structure of the Earth. So it's similar to what has been done before but it goes way deeper and covers the whole globe rather than just the parts between two points as typical sonar setups do.
I have no idea how they can do this with two sensors on a 3D object so I'm either reading it wrong or am ignorant about some aspect of the findings. Or both. lol
I would imagine its all to do with tracing multiple waves over time and analyzing both the time, phase and amplitude variations to come up with an accurate 3D representation. Implementation might be tough as signals drop in amplitude and I have no idea what physical sensors are capable of resolving to with today's technology.
To be honest, I was hoping someone might be able to explain it to me

Thanks for all the fish.