Rhythms in deep sea, fine‐grained turbidite and debris‐flow sequences, Middle Ordovician, eastern Tennessee
- 1 August 1980
- journal article
- Published by Wiley in Sedimentology
- Vol. 27 (4) , 419-432
- https://doi.org/10.1111/j.1365-3091.1980.tb01191.x
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- Sedimentation, subsidence, and evolution of a foredeep basin in the Middle Ordovician, southern AppalachiansAmerican Journal of Science, 1980
- Depositional cycles in two turbidite formations of northern ApenninesJournal of Sedimentary Research, 1975
- EXAMPLES OF ANCIENT DEEP-SEA FAN DEPOSITS FROM CIRCUM-MEDITERRANEAN GEOSYNCLINESPublished by Society for Sedimentary Geology ,1974
- Remagnetization Hypothesis Discounted: A Paleomagnetic Study of the Trenton Limestone, New York StateGSA Bulletin, 1973
- The geosyncline concept and the northern apenninesSedimentary Geology, 1970
- Flysch facies and turbidite sedimentologySedimentary Geology, 1970
- Practical Significance of Birdseye Structures in Carbonate RocksJournal of Sedimentary Research, 1968
- SEDIMENTARY STRUCTURES: MISSISSIPPI RIVER DELTAIC PLAINPublished by Society for Sedimentary Geology ,1965
- Rhythmic Alternations in Early Pliocene Sediments at Alfredton, New ZealandNew Zealand Journal of Geology and Geophysics, 1964
- Pre-orogenic sedimentation in the carpathian geosynclineInternational Journal of Earth Sciences, 1960