Wrinkle marks: An intertidal sedimentary structure due to aseismic soft-sediment loading
- 1 October 1984
- journal article
- Published by Elsevier in Sedimentary Geology
- Vol. 41 (1) , 75-95
- https://doi.org/10.1016/0037-0738(84)90003-4
Abstract
No abstract availableKeywords
This publication has 8 references indexed in Scilit:
- Tidal deposits of the Lower Cambrian Random Formation, eastern Newfoundland: facies and paleoenvironmentsCanadian Journal of Earth Sciences, 1982
- Relation entre deformations synsedimentaires et paleoseismicite dans le Messinien de San Miguel de Salinas (Cordilleres betiques orientales, Espagne)BSGF - Earth Sciences Bulletin, 1980
- Carbonate ball and pillow structuresGeological Magazine, 1978
- Sedimentology of Upper Cretaceous Cody-Parkman Delta, Southwestern Powder River Basin, WyomingGSA Bulletin, 1972
- Sedimentology and facies of the meadfoot beds (Lower Devonian) in South-East Devon (England)International Journal of Earth Sciences, 1967
- Aspects of a Middle Cambrian Thanatotope on ÖlandGeologiska Föreningen i Stockholm Förhandlingar, 1965
- Flow Rolls of Upper Devonian Rocks of South-central New York StateJournal of Sedimentary Research, 1965
- I.—Experiments in GeologyTransactions of the Geological Society of Glasgow, 1958