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- W2053051569 abstract "A long-range side-scan sonar survey along the westernmost 720 km of the active section of the Romanche Fracture Zone shows a narrow lineament which can be traced eastwards almost continuously along the north wall of the Romanche Trough until it cuts across the trough at its deepest point (Vema Depth). This lineament is inferred to be the presently active trace of the Romanche Transform Fault. The almost continuous ponded floor along the deep axis of the Romanche Trough was also mapped in detail, as were tectonic trends to the north and south of the trough. Estimated poles of rotation based on both the active fault trace and the sediment pond show considerable differences between the poles describing the motions between North America and Africa, and between Africa and South America. The transform motions near the Equator therefore do not appear to be simply coupled to the movement of the bordering continental blocks. The location of the active transform fault along the younger (northern) flank of the Romanche Trough surveyed here is consistent with a gravimetric model that indicates that the plate boundary should be located under the younger flank of the fracture-zone trough. Alternatively, should the active fault be shown in future surveys not to cross over to the southern (younger) flank of the trough east of Vema Depth, then some shift in the transform motions is indicated." @default.
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- W2053051569 date "1984-04-01" @default.
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- W2053051569 title "A long-range side-scan sonar (Gloria) survey of the Romanche active transform in the Equatorial Atlantic" @default.
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- W2053051569 doi "https://doi.org/10.1016/0025-3227(84)90006-9" @default.
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