Reflected turbidity currents on an Ordovician basin floor, Canadian Appalachians
- 1 September 1984
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 311 (5982) , 143-145
- https://doi.org/10.1038/311143a0
Abstract
No abstract availableKeywords
This publication has 7 references indexed in Scilit:
- Basin‐wide turbidites in a Miocene, over‐supplied deep‐sea plain: a geometrical analysisSedimentology, 1980
- A physical model for the rate of deposition of fine-grained sediments in the deep seaGSA Bulletin, 1976
- The Sedimentary Structures and Depositional Mechanics of Certain Ordovician Turbidites, Cloridorme Formation, Gaspé Peninsula, QuebecCanadian Journal of Earth Sciences, 1975
- ANTIDUNE CROSS‐STRATIFICATION IN A TURBIDITE SEQUENCE, CLORIDORME FORMATION, GASPÉ, QUEBECSedimentology, 1972
- ANTIDUNE CROSS‐STRATIFICATION IN A TURBIDITE SEQUENCE, CLORIDORME FORMATION, GASPÉ, QUEBECSedimentology, 1971
- Ponded Sediments of the Mid-Atlantic Ridge between 22° and 23° North LatitudeGSA Bulletin, 1969
- THE ORIGIN AND SIGNIFICANCE OF THE INTERNAL SEDIMENTARY STRUCTURES OF TURBIDITESProceedings of the Yorkshire Geological and Polytechnic Society, 1965