Jump to content

Bellingshausen Plate

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by 87.88.188.118 (talk) at 17:10, 22 October 2006 (+fr:). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

The Bellingshausen Plate was an ancient tectonic plate that fused on to the Antarctic Plate. It is named after the Russian explorer of Antarctica Fabian Gottlieb von Bellingshausen.

The plate was in existence during the Late Cretaceous and early Tertiary periods adjacent to eastern Marie Byrd Land. Independent plate motion ceased at 61 mya. The boundaries are poorly defined.

References

  • Eagles, G., K. Gohl and R. D. Larter (2004) Life of the Bellingshausen plate, Geophysical Research Letters, 31, L07603 Abstract
  • McCarron, Joe J. and Robert D. Larter, Late Cretaceous to early Tertiary subduction history of the Antarctic Peninsula, Journal of the Geological Society, March 1998