Model for turbidite-to-contourite continuum and multiple process transport in deep marine settings: examples in the rock record
- 1 January 1993
- journal article
- Published by Elsevier in Sedimentary Geology
- Vol. 82 (1-4) , 241-255
- https://doi.org/10.1016/0037-0738(93)90124-n
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Sequence of structures in fine-grained turbidites: Comparison of recent deep-sea and ancient flysch sedimentsPublished by Elsevier ,2003
- Turbidite to current-reworked sand continuum in Upper Cretaceous rocks, U.S. Virgin IslandsMarine Geology, 1987
- Permo‐Triassic reconstruction of western Pangea and the evolution of the Gulf of Mexico/Caribbean regionTectonics, 1982
- Contourites: Their recognition in modern and ancient sedimentsEarth-Science Reviews, 1979
- Tectonic significance of distal turbidites in the Middle Ordovician Blockhouse and lower Sevier formations in East TennesseeAmerican Journal of Science, 1978
- The Paleobathymetry of the Atlantic Ocean from the Jurassic to the PresentThe Journal of Geology, 1977
- Sediment transport down a seamount flank by a combined current and gravity processMarine Geology, 1977
- Upper Llandoverian Grogal Sandstones and Aberystwyth Grits in the New Quay area, Central Wales: A possible upwards transition from contourites to turbiditesGeological Journal, 1976
- GRAIN SIZE OF TURBIDITE RIPPLESSedimentology, 1969
- Textural Evidence for Deposition of Many Western North Atlantic Deep-Sea Sands by Ocean-Bottom Currents Rather than Turbidity CurrentsThe Journal of Geology, 1964