Dr. Or M. BialikMagma-rich continental margins (like the North American Atlantic margin) have a lot of sediment on top of them... too much, actually, at least for classical models to explain, but with faster heat transport, there might be an explanation.
Magma-rich continental margins (like the North American Atlantic margin) have a lot of sediment on top of them... too much, actually, at least for classical models to explain, but with faster heat transport, there might be an explanation.