Site 157

Andel, T.H. van; Heath, G.R.; Bennett, R.H.; Bukry, J.D.; Charleston, S.; Cronan, D.S.; Dinkelman, M.G.; Kaneps, A.G.; Rodolfo, K.S.; Yeats, R.S.

doi:10.2973/dsdp.proc.16.104.1973

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Velocity Structure2

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2004

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“…The CR has a three‐velocity‐layer oceanic structure. Layer 1 with a thickness of 0.2 to 0.9 km and velocities ranging from 2.4 km/s at the top to 2.8 km/s at the base, has been drilled 300 km west of the trench at DSDP site 157 [ van Andel , 1973]. Cores recovered at this site revealed 431 m of Neogene and Quaternary sediments with sonic velocity reaching 2.5 km/s overlying Neogene basalts with mean sonic velocity of 4.5 km/s [ van Andel , 1973].…”

Section: Velocity Structurementioning

confidence: 99%

“…Layer 1 with a thickness of 0.2 to 0.9 km and velocities ranging from 2.4 km/s at the top to 2.8 km/s at the base, has been drilled 300 km west of the trench at DSDP site 157 [ van Andel , 1973]. Cores recovered at this site revealed 431 m of Neogene and Quaternary sediments with sonic velocity reaching 2.5 km/s overlying Neogene basalts with mean sonic velocity of 4.5 km/s [ van Andel , 1973]. Layer 2 with a thickness of 2.8 km and mean velocities of 4.8 km/s at the top and 5.5 km/s at the base, comparable to those of oceanic layer 2b, is well resolved in the central part of our model (Figure 3).…”

Section: Velocity Structurementioning

confidence: 99%

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