Publication: [1251] Ophiolitic detritus in the Upper Ordovician Flysch of Notre Dame Bay and is bearing on the tectonic evolution of the western Newfoundland




Documented Paleocurrents


# Continental Area Stratigraphic Level Total Records Period Latitude Longitude Tectonic Plate Deposition Environment Paleocurrent Type Lithology Formation
1 North American Upper Ordovician 1 22723 49.4 -55.45 North American marine shallow paleocurrent indicator not specified sandstone Gull Island