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The Structural and Metamorphic evolution of cretaceous high-P granulites, Fiordland, New Zealand

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.

  1. http://hdl.handle.net/2123/822
Identiferoai:union.ndltd.org:ADTP/220800
Date January 2002
CreatorsDaczko, Nathan Robert
PublisherUniversity of Sydney. Geosciences
Source SetsAustraliasian Digital Theses Program
LanguageEnglish, en_AU
Detected LanguageEnglish
RightsCopyright Daczko, Nathan Robert;http://www.library.usyd.edu.au/copyright.html

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