Charcot plate

From Wikipedia, the free encyclopedia
Jump to navigation Jump to search

Template:Short description 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

<templatestyles src="Reflist/styles.css" />

  1. Script error: No such module "Citation/CS1".
  2. a b Script error: No such module "Citation/CS1".

Script error: No such module "Check for unknown parameters".

Script error: No such module "Navbox".


Template:Asbox Template:Palaeo-geo-stub