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• W2122517784 abstract "New bathymetric and magnetic anomaly data from the Phoenix Ridge, Antarctica, show that extinction of all three remaining segments occurred at the time of magnetic chron C2A (3.3 ± 0.2 Ma), synchronous with a ridge-trench collision south of the Hero Fracture Zone. This implies that the ultimate cause of extinction was a change in plate boundary forces occasioned by this collision. Spreading rates slowed abruptly at the time of chron C4 (7.8 ± 0.3 Ma), probably as a result of extinction of the West Scotia Ridge, which would have led to an increase in slip rate and transpressional stress across the Shackleton Fracture Zone. Spectacular, high-relief ridges flanking the extinct spreading center, mapped for the first time using multibeam swath bathymetry, are interpreted as a consequence of a reduction in spreading rate, involving a temporary magma oversupply immediately prior to extinction." @default.
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• W2122517784 date "2000-01-01" @default.
• W2122517784 modified "2023-10-14" @default.
• W2122517784 title "Autopsy on a dead spreading center: The Phoenix Ridge, Drake Passage, Antarctica" @default.
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• W2122517784 doi "https://doi.org/10.1130/0091-7613(2000)28<607:aoadsc>2.0.co;2" @default.
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