Development of the Middle Triassic Kobbe Formation shelf-margin prism and transgressive-regressive cycles on the shelf (Hammerfest Basin, SW Barents Sea)

Author:

Rossi Valentina MarziaORCID,Olaussen Snorre,Staine Ivan Nicola,Gennaro Matteo

Funder

ENI

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference52 articles.

1. Chapter 5 calcretes;Alonso-Zarza,2010

2. Shelf-edge architecture and bypass of sand to deep water: influence of shelf-edge processes, sea level, and sediment supply;Carvajal;J. Sediment. Res.,2009

3. Source-to-Sink Sediment Volumes within a Tectono-Stratigraphic Model for a Laramide Shelf-To-Deep-Water Basin: Methods and Results, Tectonics of Sedimentary Basins: Recent Advances;Carvajal,2012

4. Thick turbidite successions from supply-dominated shelves during sea-level highstand;Carvajal;Geology,2006

5. Growth of the paleo-Orinoco shelf-margin prism: process regimes, delta evolution, and sediment budget beyond the shelf edge;Chen;GSA Bull.,2017

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