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The Charcot plate was a fragment of the Phoenix plate. The subduction of the Charcot plate, beneath West Antarctica, stopped before 83 Ma, and became fused onto the Antarctic Peninsula. Researchers have suggested that there are remnants of the western part of the Charcot plate in the Bellingshausen Sea.

References

1. Eagles G, Gohl K, Larter RD (2004-07-10). "High-resolution animated tectonic reconstruction of the South Pacific and West Antarctic Margin" (PDF). Geochem. Geophys. Geosyst. 5 (7). Q07002. Bibcode:2004GGG.....5.7002E. doi:10.1029/2003GC000657.
2. ^ Larter RD, Cunningham AP, Barker PF, Gohl K, Nitsche FO (2002-12-13). "Tectonic evolution of the Pacific margin of Antarctica, 1, Late Cretaceous tectonic reconstructions" (PDF). J. Geophys. Res. 107 (B12): 2345. Bibcode:2002JGRB..107.2345L. doi:10.1029/2000JB000052.

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Ancient oceanic ridges	Aegir Ridge Alpha Ridge Antarctic–Phoenix Ridge Kula–Farallon Ridge Mid-Labrador Ridge Pacific–Farallon Ridge Pacific–Kula Ridge
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