Publication: [1270] Contained (reflected)turbidity currents from the Middle Ordovician Cloridorme Formation, Quebec, Canada: an alternative to the antidune hypothesis




Documented Paleocurrents


# Continental Area Stratigraphic Level Total Records Period Latitude Longitude Tectonic Plate Deposition Environment Paleocurrent Type Lithology Formation
1 North American Middle Ordovician 1 22440 49 -67 North American marine deep flute/grooves siltstone or turbidites