https://theses.otagogeology.org.nz/files/original/ffd9bfa7434d439eeadc0bfdcdb871f7.pdf 42de293c365683075ec799c02a772bed Dublin Core The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/. Title A name given to the resource Geology theses OU Geology thesis Thesis or dissertation completed by University of Otago Geology students Location WKT (WGS84) The location stored in WKT (WGS84) format POLYGON ((166.603676563107427 -46.018031336973308,166.65911596528025 -46.080084975838837,166.576013260586905 -46.10150711667594,166.542548755981869 -46.049593418330119,166.603676563107427 -46.018031336973308)) Author last name Last name of the Author Badger Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? BSc(Hons) Advisers Who supervised/advised this student Carter, R.M. Abstract The Abstract for this thesis Rock exposure on Gulches Head Peninsula; in Anchorage Cove; and northwards to Stripe Head comprises a basement of metamorphosed Lower Ordovician and Tuhua Sequence flysch sediments and quartzites which have been intruded by four different intrusive rock types. Mafic Alkali Diorite dykes and sills were probably intruded into low stratigraphic levels of Tuhua sediments during the Tuhua Orogenic Cycles. Three other intrusive rock types (members of the Kakapo Granite Batholith) were intruded following the metamorphism of the Tuhua sediments and intrusives - possibly during the Rangitata Orogeny. Low stratigraphic represents of an ?Oligocene transgressive sequence (Kaikoura Sequence sediments) unconformably overlie the basement Tuhua Sequence and ?Rangitata Sequence rocks. Two new Lower Ordovician fossil localities, containing Lancefieldian (La2) graptolite faunas, are described. Detailed investigation of the supposed Last Cove Fault was completed in Edwardson, Cunaris and Long Sounds, and although geomorphologic criteria strongly suggest the presence of this fault within the Tuhua Sequence meta-sediments between Cunaris and Long Sounds and possibly between Cunaris and Edwardson Sounds, no geologic evidence to support this interpretation has been found. A sea level magnetometer survey was undertaken in Chalky and Preservation Inlets. Survey courses and magnetic contours are presented with a short discussion. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Gulches Head Peninsula Fiordland Thesis description Number of pages, maps, CDs, etc. 100 leaves : illus., maps (fold.) ; 29 cm. Dublin Core The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/. Identifier An unambiguous reference to the resource within a given context 1973Badger Creator An entity primarily responsible for making the resource Badger, Chris P. Date A point or period of time associated with an event in the lifecycle of the resource 1973 Title A name given to the resource Geology of Gulches Head Peninsula, S.W. Fiordland Subject The topic of the resource Map Igneous petrology Paleontology Sedimentology Structural geology graptolites Last Cove Fault