The Structural and Metamorphic evolution of cretaceous high-P granulites, Fiordland, New Zealand
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Type
ThesisThesis type
Doctor of PhilosophyAuthor/s
Daczko, Nathan RobertAbstract
Fiordland is located southwest of South Island of New Zealand. The field area of this thesis is in northern Fiordland, at the boundary of pristine arc rocks (Median Tectonic Zone) and a belt of Paleozoic paragneisses and orthogneisses of variable age that represent the metamorphosed paleo-Pacific Gondwana margin.Fiordland is located southwest of South Island of New Zealand. The field area of this thesis is in northern Fiordland, at the boundary of pristine arc rocks (Median Tectonic Zone) and a belt of Paleozoic paragneisses and orthogneisses of variable age that represent the metamorphosed paleo-Pacific Gondwana margin.
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Date
2001-01-01Licence
Copyright Daczko, Nathan Robert;http://www.library.usyd.edu.au/copyright.htmlFaculty/School
Faculty of Science, School of GeosciencesDepartment, Discipline or Centre
Division of Geology and GeophysicsAwarding institution
The University of SydneyShare