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Acemap > Paper > CONSTRAINTS ON THE NATURE OF THE G-BOUNDARY IN SUBDUCTING OCEANIC LITHOSPHERE, BASED ON HIGH FREQUENCY (14 HZ) SEISMIC REFLECTION DATA

CONSTRAINTS ON THE NATURE OF THE G-BOUNDARY IN SUBDUCTING OCEANIC LITHOSPHERE, BASED ON HIGH FREQUENCY (14 HZ) SEISMIC REFLECTION DATA

2015 
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