1 10 1 https://theses.otagogeology.org.nz/files/original/edf179ba3f63c7a0223607572e7cdd1f.pdf 504ce7a1fe0166220f564ba335a6f61a 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 ((170.703077147000045 -44.384497988999954,170.627277264000099 -44.383270180999943,170.629136006000067 -44.333161812999947,170.629139577000046 -44.333071847999975,170.629148373000021 -44.332850244999975,170.624281396000015 -44.328902663999941,170.626144710000062 -44.266634154999963,170.647943528000042 -44.266966450999973,170.705524829000069 -44.334883119999972,170.704828560000124 -44.334869343999969,170.703077147000045 -44.384497988999954)) Author last name Last name of the Author Fagan Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? BSc(Hons) Advisers Who supervised/advised this student Norris, R.J. Abstract The Abstract for this thesis In the upper Hakataramea Valley, metagreywackes of the Torlesse Supergroup are unconformably overlain by mid-Tertiary shallow marine shelf deposits, the latter largely obscured by Plio-Pleistocene terrace gravels. An attempt is made to describe the extent of textural and mineralogical reconstitution within the metagreywackes. A microscopic metamorphic-textural zonation scheme is adopted and a comparison is made with the mesoscopic textural scheme of Bishop (1970). The metamorphic mineralogy is examined and individual minerals and mineral assemblages falling within the prehnite-pumpellyite and pumpellyite-actinolite facies are described in detail. Possible minimum values for depth of burial, temperature, pressure and a possible maximum value for the geothermal gradient are determined at the prehnitepumpellyiteJpwnpellyite- actinolite isograd. 500 metres of Notocenozoic sediments representing part of a marine transgression-regression sequence are described briefly and partial environmental reconstructions are attempted, based largely on grainsize parameters. A brief account of the Plio-Pleistocene geology is given and a detailed possible sedimentary, metamorphic and structural evolution is described. OURArchive handle The handle from the Otago University Research Archive (OURArchive) <a href="http://hdl.handle.net/10523/2788">http://hdl.handle.net/10523/2788</a> OURArchvive access level Abstract Only Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Hakataramea Valley Canterbury south Thesis description Number of pages, maps, CDs, etc. 63 leaves , ill. Photos, maps (folded in pocket), 27 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 1971Fagan Creator An entity primarily responsible for making the resource Fagan, Robert Keith Date A point or period of time associated with an event in the lifecycle of the resource 1971 Title A name given to the resource Structure, stratigraphy and metamorphism in the upper Hakataramea valley area, South Canterbury, New Zealand Subject The topic of the resource Map Metamorphic geology Sedimentary petrology gravel metagreywacke