Upper Llandoverian Grogal Sandstones and Aberystwyth Grits in the New Quay area, Central Wales: A possible upwards transition from contourites to turbidites-Reference-Cited by-同舟云学术

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Upper Llandoverian Grogal Sandstones and Aberystwyth Grits in the New Quay area, Central Wales: A possible upwards transition from contourites to turbidites

Published:2007-04-30 Issue:2 Volume:11 Page:101-108
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geol. J.

Author:

Anketell J. M.,Lovell J. P. B.

Publisher

Wiley

Subject

Geology

Reference10 articles.

1. Anketell , J. M. 1963

2. Fossil contourites in Lower Niesenflysch, Switzerland;Bouma;J. Sedim. Petrol.,1972

3. Contourites in Niesenflysch, Switzerland;Bouma;Eclogae Geol. Helv.,1973

4. Shaping of the continental rise by deep geostrophic contour currents;Heezen;Science,1966

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2. Eye and sheath folds in turbidite convolute lamination: Aberystwyth Grits Group, Wales;Journal of Structural Geology;2011-07

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4. An Upper Llandoverian turbidite sequence of the Bwlch-glas area, near Aberystwyth, Dyfed;Geological Journal;2007-04-30

5. Turbidite systems influenced by structurally induced topography in the multi-sourced Welsh Basin;Geological Society, London, Special Publications;2004

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