How can seafloor spreading be detected?
Answers
Answered by
0
One possible explanation for this apparent discrepancy in the origin of the dike may lie with the generation mechanism of seismo-acoustic T-waves. Although the details of T-wave generation have not been adequately modelled, seismic energy must couple into the water column through the seafloor interface overlying the crustal earthquake. The efficiency of that coupling depends on many factors, including the depth of the seafloor relative to the oceanic sound channel axis
Similar questions