1 10 1 https://theses.otagogeology.org.nz/files/original/1526f0d839e8b6317c72c87ad184a7fe.pdf dc920734dd7477260224ea6a82fc9ea3 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 ((168.194297864000077 -45.506042373999946,168.189013693000106 -45.516600855999968,168.178184152000085 -45.538238303999947,168.178056901000105 -45.538494454999977,168.155892306000055 -45.544517449999944,168.150250296000081 -45.546049912999933,168.129684672000053 -45.5041328099999,168.115751513000077 -45.475699618999954,168.120581391000087 -45.471200858999964,168.122549281000033 -45.469367653999939,168.185747213000013 -45.464576477999969,168.188225650000049 -45.474184185999945,168.195720533000099 -45.503198460999954,168.194297864000077 -45.506042373999946)) Author last name Last name of the Author Mackay Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? PGDipSci Advisers Who supervised/advised this student Norris, R.J. Abstract The Abstract for this thesis A small section of the Dun Mountain Ophiolite Belt is mapped in the Coal Hill area, Northern Southland. Ophiolitic rocks are present in two distinctively different melange belts, termed the Western Melange and the Eastern Melange. The Western Melange contains serpentinised ultramafite and microgabbro inclusions in a sheared serpentinite matrix. A large inclusion within this melange, termed the Coal Hill Inclusion, consists of spilite and associated volcanogenic sediments and is correlated with upper Livingstone terrane and basal Maitai Group, the Upukerora Formation. The Eastern Melange is characterized by a varied assemblage of rocks, including microgabbro, spilitic volcanic, conglomerate, sandstone, argillite and Atomodesmatinid limestone. A blue-grey Tertiary mudstone is also exposed in this Eastern Melange. A large sedimentary broken formation occurs within the Eastern Melange and is further broken to form part of the melange in the Windley River area. A small, coherent sliver of lower Livingstone microgabbro has a gradational contact with the Western Melange and is fault bounded to the west. This same fault also separates the melange units from Maitai Group rocks. The basal Upukerora Formation consists mainly of polymict breccias, together with minor interbedded sandstones and limestones. Stratigraphically overlying the Upukerora Formation is the Tramway Formation, composed of fine, grey sandstones and uncommon tuffs and associated arkosic rocks. Two infaulted slivers of Tertiary rocks are mapped in the area. Lithologies include fine, grey sandstones, occasionally with pebbly layers and a probable non-marine rock, with lignitic layers and lenses. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Coal Hill Thesis description Number of pages, maps, CDs, etc. 200 p. : ill., maps ; 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 1982Mackay Creator An entity primarily responsible for making the resource Mackay, Duncan Ross. Date A point or period of time associated with an event in the lifecycle of the resource 1982 Title A name given to the resource Geology of Coal hill. Subject The topic of the resource Map Paleozoic Igneous petrology Metamorphic geology Structural geology Maitai Group melange ophiolite