The Old Red Sandstone of Eastern Ekmanfjorden, Vestspitsbergen

Author:

Dineley D. L.

Abstract

AbstractThe Lower Old Red Sandstone deposits of Ekmanfjorden belong mainly to the Lykta Division, but pale sandstones with Giganthaspis representingthe Kapp Kjeldsen Division also occur in the core of what is probably a N.-S. striking anticline. The lower beds of the Lykta Division are soft, dull and silty and not very fossiliferous; above them are some 1,100 feet of sandstones and conglomeratic beds alternatingwith shales or marls. Locally abundant vertebrate remains include the guide fossil Doryaspis. Various sedimentary structures suggest rapid deposition on a broad shallow delta front.

Publisher

Cambridge University Press (CUP)

Subject

Geology

Reference12 articles.

1. Spring Pits; Sedimentation Phenomena

2. Slumping in the Carboniferous rocks of Pembrokeshire

3. The Downtonian and Devonian Vertebrates of Spitsbergen. IX—Morphologic and systematic studies of the Spitsbergen Cephalaspids;Wängsjö;Norsk Polarinst. Skr.,1952

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