DEEP CHANNELS, MASSIVE BEDS AND TURBIDITY CURRENT GENESIS IN THE CENTRAL PENNINE BASIN-Reference-Cited by-同舟云学术

DEEP CHANNELS, MASSIVE BEDS AND TURBIDITY CURRENT GENESIS IN THE CENTRAL PENNINE BASIN

Published:1970-02 Issue:4 Volume:37 Page:495-519
ISSN:0044-0604
Container-title:Proceedings of the Yorkshire Geological Society
language:en
Short-container-title:Proceedings of the Yorkshire Geological Society

Author:

Collinson J. D.

Publisher

Geological Society of London

Subject

Geology

Reference38 articles.

1. The Mam Tor sandstones: a “turbidite” facies of the Namurian deltas of Derbyshire, England;Allen;J. sedim. Petrol,1960

2. Asymmetrical ripple marks and the origin of water laid cosets of cross-strata;Allen;Lpool Manchr geol. J.,1963

3. PRIMARY CURRENT LINEATION IN THE LOWER OLD RED SANDSTONE (DEVONIAN), ANGLO-WELSH BASIN

4. ON BED FORMS AND PALAEOCURRENTS

5. Some flume experiments on large grains but little denser than the transporting fluid, and their implications;Bagnold;Minut. Proc. Instn Civ. Engrs,1955

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