Transitional submarine fan deposits from the late Precambrian Kongsfjord Formats submarine fan, NE Finnmark, N. Norway

• Published in: Sedimentology
• Main Author: PICKERING, KEVIN T.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1983
• Subjects: Kongsfjord; Norway; Finnmark; Kongsfjord*; North Norway
• Online Access: http://dx.doi.org/10.1111/j.1365-3091.1983.tb00664.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3091.1983.tb00664.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3091.1983.tb00664.x

ABSTRACT Three transitional submarine fan environments are recognized in the late Precambrian, 3‐2 km thick Kongsfjord Formation in NE Finnmark, North Norway, namely: (1) middle to outer fan; (2) fan lateral margin, and (3) fan to upper basin‐slope deposits. Middle to outer fan deposits have a high proportion of sandstones, typically showing Bouma T bede with T a in the thicker beds. Deposition was mainly from sheet flows with rare shallow channels. Middle to outer fan deposits are an association of sandstone packets less than 10 m thick but commonly only a few metres thick, interpreted as channels or lobes. Interchannel and fan fringe deposits occur as discrete packets of beds between the thicker bedded and coarser grained channel or lobe deposits. Fan lateral margin deposits are recognized on the basis of their stratigraphic position adjacent to inner/middle fan deposits. They are characterized by: (a) a relatively high proportion of fine‐grained sandstone/siltstone turbidites compared to other major fan environments; (b) relatively small channels oriented at various angles to the regional basin slope; (c) lobes associated with channels, and (d) abundant clastic dykes and other soft‐sediment deformation. Fan lateral margin deposits are distinguished from the outer fan/basin plain successions on account of the very high proportion of siltstone turbidites comparable with middle fan inter‐channel deposits. Fan to upper basin‐slope deposits occur at the top of the formation as an alternation of sandstone turbidites, most of which are laterally discontinuous, and very thin‐bedded upper basin‐slope siltstones with slide deposits.