Abstract
The Navarana Fjord Escarpment is a major sedimentological feature of the Franklinian Basin in North Greenland. A southern sequence of Ordovician-Silurian shelf carbonates forming the escarpment itself is juxtaposed across a steep scarp slope with a northern deep-water trough succession dominated by sandstone turbidites. The relief of the scarp can be estimated to many hundred metres on the basis of present-day exposures along Navarana Fjord and J. P. Koch Fjord, central North Greenland.
Highlights
The Navarana Fjord Escarpment is a major sedimentological feature of the Franklinian Basin in North Greenland
The evolution of the Lower Palaeozoic basin in North Greenland was interpreted in terms of control by an east-west trending fault system by Surlyk et al (1980) and the Navarana Fjord Escarpment was originally ascribed to one of these faults; its significance has subsequently been discussed in a series of papers by J
These figures loeate a series of shear zones in the earbonates forming the vertical fjord wall
Summary
The Navarana Fjord Escarpment is a major sedimentological feature of the Franklinian Basin in North Greenland. The evolution of the Lower Palaeozoic basin in North Greenland was interpreted in terms of control by an east-west trending fault system by Surlyk et al (1980) and the Navarana Fjord Escarpment was originally ascribed to one of these faults; its significance has subsequently been discussed in a series of papers by J.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.