Travel-time residuals of PP waves reflected under the central Atlantic Ocean

Physics

Scientific paper

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Scientific paper

Travel-time residuals of PP, for waves generated in South and Central America and recorded in Africa and Europe after reflection under the central Atlantic Ocean, are studied to show possible structural variations in the reflection area. The ridge appears as a zone of positive residuals (⋍ + 1.0 s) indicative of lower velocities, and is clearly differentiated from the surrounding oceanic basins where residuals are negative (⋍ - 3.2 s); the ridge influence extends up to about 400 km from the crest.

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