Sedimentary breccia and diamictite of the Cambrian Spurs Formation in northern Victoria Land, Antarctica: two kinds of debris flows in a submarine channel system
Sign Up to like & getrecommendations! Published in 2018 at "Antarctic Science"
DOI: 10.1017/s0954102018000123
Abstract: Abstract The submarine channel-fill system of the Cambrian Spurs Formation exhibits unique metre-scale cycles of breccia and diamictite. The studied sections, Eureka Spurs, are located at the Mariner Glacier in the central-eastern part of northern… read more here.
Keywords: cambrian spurs; submarine channel; channel; breccia diamictite ... See more keywords