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The Vampire Formation is a formation of delta-front siliciclastics deposited in the early Cambrian. The upper unit is trilobitic Cambrian. Some authors place the underlying Ingta formation at least partially in the Cambrian; in places it overlies the sub-Cambrian unconformity.

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  • The Vampire Formation is a formation of delta-front siliciclastics deposited in the early Cambrian. The upper unit is trilobitic Cambrian. Some authors place the underlying Ingta formation at least partially in the Cambrian; in places it overlies the sub-Cambrian unconformity. It contains a rich array of trace fossils spanning the pre-trilobitic Cambrian, including some found only there (once interpreted as sponge-like forms); its uppermost strata contain Fallotaspis-zone trilobites, whereas its lower levels come above Protohertzina and Anabarites-bearing shelly layers in the ; as such, it spans much of the Fortunian. (en)
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  • 3673 (xsd:nonNegativeInteger)
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dbp:location
  • Mackenzie Mountains (en)
dbp:overlies
  • Ingta Formation (en)
dbp:period
  • Cambrian (en)
dbp:thickness
  • up to (en)
dbp:type
dbp:underlies
  • Sekwi Formation (en)
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  • The Vampire Formation is a formation of delta-front siliciclastics deposited in the early Cambrian. The upper unit is trilobitic Cambrian. Some authors place the underlying Ingta formation at least partially in the Cambrian; in places it overlies the sub-Cambrian unconformity. (en)
rdfs:label
  • Vampire Formation (en)
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