Cambrian platform - outer shelf relationships in the Nordenskiöld Fjord region, central North Greenland

Authors

  • J.R Ineson
  • J.S Peel

DOI:

https://doi.org/10.34194/rapggu.v133.7972

Abstract

Cambrian sequences around the head of Nordenskiöld Fjord, central North Greenland, preserve the transition from platform interior carbonates of the Ryder Gletscher Group (redefined) to outer shelf-slope and platform margin sequences assigned to the Brønlund Fjord and Tavsens Iskappe Groups. Study of this transition has allowed redefinition and integration of these two stratigraphic schemes. Shallow subtidal to intertidal, well-bedded carbonates of the platform interior grade north-eastwards into high-energy grainstones and algal boundstones of the platform margin complex. Platform foreslope facies show well-developed clinoform bedding and wedge out into dark carbonates and clastics of the outer shelf sequence.

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Published

1987-12-31

How to Cite

Ineson, J., & Peel, J. (1987). Cambrian platform - outer shelf relationships in the Nordenskiöld Fjord region, central North Greenland. Rapport Grønlands Geologiske Undersøgelse, 133, 13–26. https://doi.org/10.34194/rapggu.v133.7972