Tectonics of the Mid-Atlantic Ridge, 6–8° South latitude |
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| Authors: | Tjeerd H Van Andel G Ross Heath |
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| Institution: | (1) Dept. of Oceanography, Oregon State University, Corvallis, Or., U.S.A. |
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| Abstract: | A regional geophysical traverse of the Mid-Atlantic Ridge in the northern South Atlantic was obtained during CIRCE cruise of the Scripps Institution of Oceanography. During the traverse, four detailed surveys were made of small areas on the crest and east flank. The geomagnetic anomaly profile can be used as a time base for the interpretation of tectonic events of the ridge. The profile also suggests that the rate of sea-floor spreading in this part of the South Atlantic accelerated twice, approximately 40 and 4.5 million years ago, and decelerated at least twice, 38 and 10 million years ago. Accelerations were probably accompanied by uplift and normal faulting of the central part of the ridge, while decelerations produced subsidence with modest contraction, reflected in reverse faulting and folding. The effects of uplift are clearly present in the reflection seismic records, which are, however, not well suited to detect reverse faulting.Spreading without creation of significant relief occurred on the ridge until approximately 5 million years ago. This process produced a low relief with small rifts, strongly reminiscent of the present crestal topography of the East Pacific Rise. A markedly linear secondary relief of 100–200 m, parallel to the ridge axis, developed later by faulting of the flanks. Portions of the crust that were near the crest during periods of uplift are more intensely faulted than those that were remote at all times. The importance of the last uplift of the crest and associated faulting on the flanks is reflected by a decrease in the density of faulting away from the ridge crest.The present crestal zone is very different from the flanks and from the older crests; the relief is nearly ten times greater, transverse disturbances are common, and there is conflicting evidence regarding its age. This striking change in character indicates either a recent change in the spreading process or a recent period of strong deformation which has affected only the crestal zone.Contribution from Scripps Institution of Oceanography, University of California, San Diego. |
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