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- W1981313007 abstract "A multichannel seismic reflection profile across the East Pacific Rise near 9°N reveals an approximately 400 m thick layer at the top of the oceanic crust with seismic velocity of about 2.8 km/s at the Rise crest. This velocity increases to about 3.8 km/s, 210 km east of the Rise crest. These low velocities suggest that this layer is probably a porous lava flow layer (layer 2A of seismic refraction studies) generated by volcanic activity at the spreading center. Reflections from the base of the layer imply a relatively sharp transition between the lava flows and the underlying layer (presumably a sheeted dike complex). The underlying layer is a zone about 1.4 km thick (with velocity about 5.7 km/s) whose base may coincide with the top of a low velocity magma chamber from which the crust develops." @default.
- W1981313007 created "2016-06-24" @default.
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- W1981313007 date "1982-01-01" @default.
- W1981313007 modified "2023-10-01" @default.
- W1981313007 title "Lava flow layer‐East Pacific Rise" @default.
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- W1981313007 doi "https://doi.org/10.1029/gl009i001p00017" @default.
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