The Charcot Plate was a fragment of the Phoenix Plate. [1] The subduction of the Charcot Plate, beneath West Antarctica, stopped before 83 Ma, and became fused onto the Antarctic Peninsula. [2] Researchers have suggested that there are remnants of the western part of the Charcot Plate in the Bellingshausen Sea. [2]
References
- ^ 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.
- ^ a b 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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The Charcot Plate was a fragment of the Phoenix Plate. [1] The subduction of the Charcot Plate, beneath West Antarctica, stopped before 83 Ma, and became fused onto the Antarctic Peninsula. [2] Researchers have suggested that there are remnants of the western part of the Charcot Plate in the Bellingshausen Sea. [2]
References
- ^ 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.
- ^ a b 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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| This tectonics article is a stub. You can help Wikipedia by expanding it. |
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| This palaeogeography article is a stub. You can help Wikipedia by expanding it. |