Late Cambrian stratigraphy of the Heritage Range, Ellsworth Mountains: implications for basin evolution

• Published in: Antarctic Science
• Main Authors: Curtis, Michael L., Lomas, Simon A.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Cambridge University Press 1999
• Subjects: Pacific; Ellsworth Mountains; Frazier; Heritage Range; Minaret; Liberty Hills; Frazier Ridge; Independence Hills; Springer Peak; The Minaret; Antarctic Science
• Online Access: http://nora.nerc.ac.uk/id/eprint/503140/; https://doi.org/10.1017/S0954102099000103

Deposition of the Upper Cambrian succession of the Ellsworth Mountains was influenced by major, episodic tectonically-driven changes to the depositional basin geometry. We subdivide the succession into four stratigraphical sequences based on the recognition of three sequence-bounding unconformities. The upper part of Sequence 1 is composed of the laterally equivalent Liberty Hills, Springer Peak and Frazier Ridge formations, a siliciclastic fluvial to marine deltaic association displaying NW-directed palaeocurrents. A switch in the position of the Late Cambrian depocentre from the north-west to the south coincided with cessation of terrigenous clastic deposition and accumulation of Sequence 2, the limestones of the Minaret Formation. Previously unreported talus breccias from the Independence Hills provide important clues to basin configuration at this time. A brief period of emergence of the Minaret Formation is inferred, prior to rapid subsidence and disconformable deposition of Sequence 3 (the ‘transition beds’) in outer-inner shelf environments. Localized intra-basinal uplift occurred prior to the deposition of Sequence 4 (the lower Crashsite Group), the base of which is locally an erosive unconformity, with a correlative conformity exposed elsewhere. We interpret the Upper Cambrian succession as representing the ‘rift-drift’ transition from initial rifting (preceded by Middle Cambrian volcanism) to thermal subsidence along the South African sector of the palaeo-Pacific margin of Gondwana.