1 10 1 https://theses.otagogeology.org.nz/files/original/75e97b1b4f7cbc8a9747fade0f7b1f70.pdf 75d80cd0b631b900d1b89c5eb861374a 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 ((170.596584263000068 -45.336973920999981,170.656064123000078 -45.305477226999983,170.673870611000098 -45.338403647999939,170.65764106600011 -45.360285570999963,170.626340852000112 -45.37001915299993,170.596008361000031 -45.365789448999976,170.596584263000068 -45.336973920999981)) Author last name Last name of the Author Bogie Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? PGDipSci Advisers Who supervised/advised this student Coombs, D.S. Abstract The Abstract for this thesis A series of major north-west trending faults, which make up the Waihemo Fault Complex, provide a boundary between textural zone 1 and 2A semi-schists, which have been metamorphosed to the prehnite-pumpellyite metamorphic facies, and textural zone 3B and 4 schists which have been metamorphosed to the greenschist facies. Original lithologies can be recognized within the semi-schists. Sandstone and siltstone are predominant with minor argillite, limestone, chert, tuff and conglomerate. Most of the minor lithologies are contained within argillite-siltstone sequences which are contained within sandstone-siltstone sequences. Limestone outcrops as massive beds, lenses and interbedded with chert and/or chloritic slate. Two types of occurrences of chert were found; those interbedded with limestone and red chert enclosed within argillite. Tuff was found as chloritic slates interbedded with limestone and as prehnite-rich beds enclosed within siltstone. Conglomerate occurred as lenses within interbedded sandstone-siltstone sequences and as a large irregular mass within an argillite-siltstone sequence. The quartzofeldspathic schists south of the Waihemo No. 2 Fault are overlain by pre-Eocene quartz conglomerates and sands which are overlain by Bortonian glauconitic marine silts. These are in turn overlain by plio-pliestocene remnant piedmont terraces and loess. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Waihemo Thesis description Number of pages, maps, CDs, etc. 58 leaves : col. illus., maps (2 fold. col. in pocket) ; 30 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 1978Bogie Creator An entity primarily responsible for making the resource Bogie, Ian. Date A point or period of time associated with an event in the lifecycle of the resource 1978 Title A name given to the resource Geology of the mid-part of the Waihemo fault complex, North Otago. Subject The topic of the resource Map Metamorphic geology Sedimentary petrology Structural geology chert greenschist limestone prehnite-pumpellyite Waihemo Fault Complex