Ocean Crustal Seismic Layer 2C
Abstract Normal oceanic crust is chiefly defined by a seismic structure consisting of layers 2 and 3. Houtz and Ewing (1976, 10.1029/JB081i014p02490) further subdivided layer 2 into layers 2A, 2B, and 2C. Though it has been associated with the dike sections sampled in Holes 504B and 1256D, layer 2C...
| Published in: | Geochemistry, Geophysics, Geosystems |
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| Main Author: | |
| Format: | Article |
| Language: | English |
| Published: |
Wiley
2018-09-01
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| Subjects: | |
| Online Access: | https://doi.org/10.1029/2018GC007614 |