Please use this identifier to cite or link to this item:
https://hdl.handle.net/2440/128283
Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Van Leeuwin, A. T. dV. | - |
dc.coverage.spatial | Fisher Terrane, East Antarctica | - |
dc.date.issued | 2017 | - |
dc.identifier.uri | http://hdl.handle.net/2440/128283 | - |
dc.description | This item is only available electronically. | en |
dc.description.abstract | The Fisher Terrane, located in the central region of the Prince Charles Mountains, east Antarctica, evolved during the Mesoproterozoic as a magmatic arc system. Metapelitic schists from the Fisher Massif were deposited after 1206 ± 49 Ma and yield metamorphic monazite ages of c. 538–505 Ma relating to the regionally recognized Neoproterozoic to early Cambrian Prydz Event. Calculated phase equilibria modelling constrains the metamorphic conditions during this event to 2.6–4.0 kbar and 553–576°C, relating to apparent thermal gradients of 144 °C/kbar to 212 °C/kbar. Conditions such as these are plausibly related to metamorphism taking place in an extensional back-arc setting which was then subsequently inverted and thickened via continental collision. A migmatitic felsic gneiss from Nilsson Rocks yields metamorphic monazite 206Pb/238U ages between 1115–1050 Ma with a weighted average age of 1085.0 ± 7.1 Ma. This metamorphic event may relate to a similarly aged episode of subduction related magmatism identified elsewhere in the central Prince Charles Mountains. This study therefore presents evidence of previously unidentified Prydz-aged high-thermal gradient metamorphism in the Fisher Terrane as well as identifying an older c. 1085 Ma metamorphic event not documented elsewhere in the Prince Charles Mountains. | en |
dc.language.iso | en | en |
dc.subject | Honours; Geology; East Antarctica; Prince Charles Mountains; THERMOCALC; metamorphism; U–Pb geochronology; tectonics, Gondwana | en |
dc.title | New constraints on the tectonometamorphic evolution of the Fisher Terrane, central Prince Charles Mountains, eastern Antarctica | en |
dc.type | Thesis | en |
dc.contributor.school | School of Physical Sciences | en |
dc.provenance | This electronic version is made publicly available by the University of Adelaide in accordance with its open access policy for student theses. Copyright in this thesis remains with the author. This thesis may incorporate third party material which has been used by the author pursuant to Fair Dealing exceptions. If you are the author of this thesis and do not wish it to be made publicly available, or you are the owner of any included third party copyright material you wish to be removed from this electronic version, please complete the take down form located at: http://www.adelaide.edu.au/legals | en |
dc.description.dissertation | Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2017 | - |
Appears in Collections: | School of Physical Sciences |
Files in This Item:
File | Size | Format | |
---|---|---|---|
VanLeeuwenATdV2017_Hons.pdf | 6.05 MB | Adobe PDF | View/Open |
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.