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- W2022157112 abstract "Vertical movements of lithospheric slivers due to slow‐slip, long‐offset transform tectonics may cause major topographic anomalies such as the rough topography of the equatorial Atlantic, where a number of long offset transforms are clustered. These vertical motions even may have caused the intermittent emersion and sinking of islands throughout the evolution of the equatorial Atlantic. We studied a transform‐related topographic anomaly observed at the Vema Fracture Zone in the Atlantic at 11°N in the form of a transverse ridge (Figure 1). We used multichannel seismic reflection surveys to image the morphology, thickness, and internal structure of the carbonate platform capping the crest of the transverse ridge. We found that the Vema transverse ridge is actually an uplifted sliver of oceanic crust and—about 3 m.y.a.—its summit was above sea level." @default.
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- W2022157112 date "1994-08-09" @default.
- W2022157112 modified "2023-09-26" @default.
- W2022157112 title "Imaging crustal uplift, emersion, and subsidence at the Vema Fracture Zone" @default.
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- W2022157112 doi "https://doi.org/10.1029/94eo01013" @default.
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