| Autor: |
Collette, B. J., Schouten, J. A. |
| Zdroj: |
Marine Geophysical Researches; August 1970, Vol. 1 Issue: 1 p46-60, 15p |
| Abstrakt: |
First conclusions of a study of the fault pattern in the North Atlantic ocean are briefly outlined. Correlation of fracture zones in deep ocean basins, even over short distances (30 miles) is difficult when using only topographic and seismic profiler data, and requires the additional criterion that the magnetic pattern is shifted along the fracture zones. This implies that each track must be paralleled by at least one more track at close distance to detect breaks in the magnetic pattern. |
| Databáze: |
Supplemental Index |
| Externí odkaz: |
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