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PhD <strong>the</strong>sis, ni ersity <strong>of</strong> Otago, Dunedin,New ealand.Scott, . .; Cooper, A.F. 2006: Early Cretaceous extensionalexhumation <strong>of</strong> <strong>the</strong> lower crust <strong>of</strong> a magmatic arc: E idencefrom <strong>the</strong> Mt Irene Shear Zone, <strong>Fiordland</strong>, New Zealand.et : 1–15.Scott, . .; Cooper, A.F.; Palin, . .; Tulloch, A. .; ula, .;ongens, R; Spell, T.L.; Pearson, N. . 2009a: Tracking <strong>the</strong>influence <strong>of</strong> a continental margin on growth <strong>of</strong> a magmaticarc (<strong>Fiordland</strong>, New Zealand) using <strong>the</strong>rmobarometry,<strong>the</strong>rmochronology, and zircon U-Pb and Hf isotopes. et: TC6007, doi:10.1029/2009TC002489. +Scott, J.M.; Palin, J.M. 2008: LA-ICP-MS U-Pb zircon agesfrom Mesozoic plutonic rocks in eastern <strong>Fiordland</strong>, Newealand. e eala al e l a e :105–113.Scott, . .; Palin, . .; Cooper, A.F. 2009b: eehi e Diorite, Lakeanapouri. e eala al e l a e: 59–65.Scott, . .; Palin, . .; Cooper, A.F.; Fagereng, A.; ing, R.P.2009c: Polymetamorphism, zircon growth and retention <strong>of</strong> earlyassemblages through <strong>the</strong> dynamic e olution <strong>of</strong> a continental arcin <strong>Fiordland</strong>, New ealand. al eta e l: 281–294.Scott, J.M.; Turnbull, I.M.; Ewing, T.A.; Allibone, A.H.; Palin,. .; Cooper, A.F. 2008: Petrology and geochronology <strong>of</strong><strong>the</strong> volcaniclastic and volcanogenic Mesozoic Loch BurnFormation in eastern <strong>Fiordland</strong>, New ealand. e ealaal e l a e : 89–103.Simpson, C.C. 2006: Early Paleozoic metasedimentary rocks <strong>of</strong>southwest <strong>Fiordland</strong>, New ealand: petrology, geochemistry,and detrital zircon geochronology. 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PhD <strong>the</strong>sis, ni ersity<strong>of</strong> Otago, Dunedin, New ealand.95
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1 : 2 5 0 0 0 0 G e o l o g i c a l
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Geology of theFiordland AreaScale 1
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CONTENTSABSTRACT ..................
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FrontispieceA pekapeka (neck pendan
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Fiordland’s proximity to the acti
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INTRODUCTIONTHE QMAP SERIESThis geo
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ThesesPublished papersPublished map
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GEOMORPHOLOGYThe uplifted Fiordland
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TributaryglaciersTrunkglaciersQuate
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to 14 000 years BP, when the major
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Figure 10 A fossil marine arch, ero
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Figure 14 The northern Fiordland co
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STRATIGRAPHYPaleozoic metasedimenta
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ABCFigure 17 dgecumbe Group formati
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thin marble (Fig. 18C), with interb
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quartzofeldspathic biotite gneiss,
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ACBFigure 23 Ordovician Fanny Bay G
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Paleozoic metamorphic rocks of unce
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28PERMIAN TO URASSIC SEDIMENTARY AN
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Figure 28 Latest Cambrian to earlie
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etasedimentary xenoliths are common
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Late Triassic to Cretaceous plutoni
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heterogeneous, metre- to kilometre-
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The Malaspina Pluton ( wm; 117-114
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granite, leucogranite and tonalite
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and comprises weakly foliated, loca
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- Page 70 and 71: y the present-day coast. The ice le
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- Page 78 and 79: Major active faultsOffshore volcani
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