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Current studies of the Earth’s inner core structure using body waves typically measure the differential travel times between different branches of PKP phases, which are then modeled by ray theory that does not account for the finite widths
Current studies of the Earth’s inner core structure using body waves typically measure the differential travel times between different branches of PKP phases, which are then modeled by ray theory that does not account for the finite widths
Externí odkaz:
http://ndltd.ncl.edu.tw/handle/96q92r
