Arc accretion to the early Paleozoic Antarctic margin of Gondwana in Victoria Land

The Antarctic Ross Orogen was built up during the early Paleozoic in the framework of the convergence between the Paleo-Pacific oceanic plate and the Gondwana continental margin. Models for the Ross Orogen in northern Victoria Land are based on terranes having a variable provenance with respect to t...

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Bibliographic Details
Published in:Gondwana Research
Main Authors: ROCCHI, SERGIO, GEMELLI, MAURIZIO, BRACCIALI L, DI VINCENZO G, GHEZZO C.
Other Authors: Rocchi, Sergio, Bracciali, L, DI VINCENZO, G, Gemelli, Maurizio, Ghezzo, C.
Format: Article in Journal/Newspaper
Language:English
Published: 2011
Subjects:
Magmatic arc
Backarc
Accretion
Antarctica
Ross-Delamerian Orogeny
Antarctic
Bowers
Pacific
Ross Sea
The Antarctic
Victoria Land
Antarc*
Online Access:http://hdl.handle.net/11568/144230
https://doi.org/10.1016/j.gr.2010.08.001
Description
Summary:The Antarctic Ross Orogen was built up during the early Paleozoic in the framework of the convergence between the Paleo-Pacific oceanic plate and the Gondwana continental margin. Models for the Ross Orogen in northern Victoria Land are based on terranes having a variable provenance with respect to the margin. However, recent studies provide evidence for the occurrence of different pieces of the lithospheric puzzle: (i) the Wilson continental magmatic arc, representing the main part of the active Gondwana margin, (ii) the Bowers arc–backarc system, (iii) the Admiralty crustal ribbon including continental material of the Wilson forearc, and (iv) the newly discovered, Cambrian oceanic magmatic Tiger arc, along the Ross Sea coast. An updated model is presented in which, after the Early Cambrian magmatic activity of the Wilson arc, a retreat of the subduction zone in the Early–Middle Cambrian gave way to boudinage of the Wilson forearc, trenchward arc migration, opening of the Bowers backarc basin and inception of the outboard Tiger subduction zone. Renewed convergence resulted in the development of the Middle Cambrian Bowers arc, closure of the backarc and deep underthrusting of portions of it at the Middle–Late Cambrian. Finally, in the latest Cambrian to earliest Ordovician, fast exhumation was coupled in the north with erosion and sediment shed to the northeast, and with extension and potassic magmatism in central and southern Victoria Land.

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