- Page 1: 1 : 2 5 0 0 0 0 G e o l o g i c a l
- Page 5 and 6: CONTENTSABSTRACT ..................
- Page 7 and 8: FrontispieceA pekapeka (neck pendan
- Page 9 and 10: Fiordland’s proximity to the acti
- Page 11 and 12: INTRODUCTIONTHE QMAP SERIESThis geo
- Page 13 and 14: ThesesPublished papersPublished map
- Page 15 and 16: GEOMORPHOLOGYThe uplifted Fiordland
- Page 17 and 18: TributaryglaciersTrunkglaciersQuate
- Page 19 and 20: to 14 000 years BP, when the major
- Page 21 and 22: Figure 10 A fossil marine arch, ero
- Page 23 and 24: Figure 14 The northern Fiordland co
- Page 25 and 26: STRATIGRAPHYPaleozoic metasedimenta
- Page 28 and 29: ABCFigure 17 dgecumbe Group formati
- Page 30 and 31: thin marble (Fig. 18C), with interb
- Page 32 and 33: quartzofeldspathic biotite gneiss,
- Page 34 and 35: ACBFigure 23 Ordovician Fanny Bay G
- Page 36 and 37: Paleozoic metamorphic rocks of unce
- Page 38 and 39: 28PERMIAN TO URASSIC SEDIMENTARY AN
- Page 40 and 41: Figure 28 Latest Cambrian to earlie
- Page 42 and 43: etasedimentary xenoliths are common
- Page 44 and 45: Late Triassic to Cretaceous plutoni
- Page 46 and 47: heterogeneous, metre- to kilometre-
- Page 48 and 49: The Malaspina Pluton ( wm; 117-114
- Page 50 and 51: granite, leucogranite and tonalite
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and comprises weakly foliated, loca
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sedimentary rocks extend offshore t
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AFigure 47 ocene sedimentary rocks
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Figure 49 Oligocene sedimentary roc
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graded sandstone and mudstone (Cart
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sequence of Oligocene graded sandst
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oup, and is restricted to the area
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QUATERNARYExtensi e Quaternary depo
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y the present-day coast. The ice le
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eorge Sound, and remnants of well-r
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TECTONIC HISTORYFiordland has a lon
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A B CDFigure 65 Fiordland plutonic
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Major active faultsOffshore volcani
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a zone of amphibolite facies gneiss
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GEOLOGICAL RESOURCESAlmost the whol
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HydrocarbonsSequences within the Cr
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ENGINEERING GEOLOGYThis section pro
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GEOLOGICAL HA ARDSThe numerous geol
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NDCenozoic to Holocene faultsABCact
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The most frequent landslide hazard
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earthquakes along the Puysegur subd
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ACNOWLEDGMENTSapping of Fiordland w
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ishop, D. . 1991: High-le el marine
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Ewing, T.A.; Weaver, S.D.; Bradshaw
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Lee, W. .; Ward, C. .; Wilson, . .
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Schacht, B. 1984: Interpretation re
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Ward, C. . 1986: Speculations on th
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The geology of Fiordland is describ