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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Other Authors: | , |
Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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Universität Bremen
2018
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Online Access: | https://media.suub.uni-bremen.de/handle/elib/1441 https://nbn-resolving.org/urn:nbn:de:gbv:46-00106584-15 |