Geodynamic evolution of the Pacific margin of West Antarctica based on apatite thermochronology

The West Antarctic continent formed during most of the Palaeozoic and Mesozoic era by accretion of crustal blocks to form the palaeo-Pacific margin of Gondwana. In the mid Cretaceous, Gondwana break-up was associated with a major change from convergence to extension along the palaeo-Pacific margin,...

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Bibliographic Details
Main Author: Zundel, Maximilian
Other Authors: Spiegel, Cornelia, Najman, Yani
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: Universität Bremen 2018
Subjects:
550
Online Access:https://media.suub.uni-bremen.de/handle/elib/1441
https://nbn-resolving.org/urn:nbn:de:gbv:46-00106584-15