A tsunami deposit in the Stonewall Formation (Upper Ordovician), northeastern margin of the Williston Basin, Canada, and its tectonic and stratigraphic implications

Author:

Pratt Brian R.,Sproat Colin D.

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference66 articles.

1. Cratonic basins;Allen,2012

2. The ups and downs of “Tectonic Quiescence”—recognizing differential subsidence in the epicontinental sea of the Oxfordian in the Swiss Jura Mountains;Allenbach;Sedimentary Geology,2002

3. Williston Basin province—stratigraphic and structural framework to a geologic assessment of undiscovered oil and gas resources;Anna,2013

4. Bezys, R.K., Conley, G.G., 1998. Geology of the Ordovician/Silurian Stonewall Formation in Manitoba. Manitoba Energy and Mines, Stratigraphic Map Series, Os-1, scale: 1:200,000.

5. Spatial variations in tectonic subsidence during Tippecanoe I in the Michigan Basin;Coakley;Basin Research,1994

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