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Submarine carbonate breccia beds—a oppositional model for two-layer, sediment gravity flows from the Sekwi Formation (Lower Cambrian), Mackenzie Mountains, Northwest Territories, C...
by
Krause
,
F
.
F
.
,
Oldershaw, A. E.
Published in
Canadian Journal of Earth Sciences
(1979)
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General Earth and Planetary Sciences
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