Relative sea level change along the Slave craton coastline: Characteristics of Archean continental rifting
The >2.8 Ga siliciclastic-dominated, craton-cover succession with subordinate mafic volcanic rocks at Beniah Lake in the Slave craton has been informally referred to as the Bell Lake group. The Beniah Lake succession, up to 1 km thick, is composed of 7–120 m thick coarsening-upward (CU) sequences...
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Veröffentlicht in: | Sedimentary geology 2005-04, Vol.176 (1), p.97-119 |
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