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The AAPG/Datapages Combined Publications Database

CSPG Bulletin

Abstract


Bulletin of Canadian Petroleum Geology
Vol. 26 (1978), No. 2. (June), Pages 208-217

A Middle Ordovician Unconformity in the Arctic Lowlands: DISCUSSION

James Dixon

ABSTRACT

The well-documented Middle Ordovician regional unconformity between the Franklin Mountain and Mount Kindle Formations of the northern Interior Plains (NWT) can be continued into the Arctic Lowlands. Paleontological data exist that suggest Middle Ordovician strata are absent. A sedimentary hiatus is recognized between Lower and Upper Ordovician rocks on Somerset Island and is equated to the Middle Ordovician unconformity of the Interior Plains. A similar sedimentary break, described from Baffin Island, also may be the Middle Ordovician regional unconformity.


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