Paleomagnetic evidence of large footwall rotations associated with low-angle faults at the Mid-Atlantic Ridge
Author:
Publisher
Geological Society of America
Subject
Geology
Reference18 articles.
1. Extremely asymmetric magmatic accretion of oceanic crust at the ends of slow-spreading ridge segments
2. flexural rotation of normal faults
3. Seismic reflection imaging of an oceanic detachment fault: Atlantis megamullion (Mid-Atlantic Ridge, 30°10′N)
4. Thin crust, ultramafic exposures, and rugged faulting patterns at the Mid-Atlantic Ridge (22°–24°N)
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