1 10 2 https://theses.otagogeology.org.nz/files/original/f8ca7e802ec374e8a838fabae6a720be.pdf 47f1f877b1a3a7bc0fcc7654e09e8897 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 MULTIPOLYGON (((170.517052682067 -45.8981924221679,170.498483884105 -45.8863561920674,170.514216864362 -45.8700294905412,170.556144002159 -45.8623611434089,170.602896841589 -45.8214381727438,170.618916303892 -45.8131999863651,170.625210283952 -45.7933265865297,170.703566935237 -45.7754009800494,170.72019984987 -45.7681134761579,170.740562129658 -45.7694707605913,170.734408411591 -45.7869718471385,170.716624478748 -45.8056695029933,170.679345831581 -45.8177780357334,170.677873420324 -45.8367998850659,170.648877805233 -45.8457325027839,170.609058461018 -45.8525264841923,170.599160556188 -45.8766097578685,170.566725301227 -45.8854491222552,170.536106187645 -45.8838400463155,170.517052682067 -45.8981924221679))) Author last name Last name of the Author Flectcher Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? BSc(Hons) Advisers Who supervised/advised this student Riesselman, C.R. Gorman, A.R. Abstract The Abstract for this thesis The sedimentary units that line the floor of Otago Harbour contain a rich geological record of past environmental changes and catastrophic events, like earthquakes and floods that may have affected the region. While the surface geology of the region around Otago Harbour has been well studied, very little is known about the units and structures that lie beneath. These subsurface features hold vast amounts of geological evidence which can be used to determine the origin of and processes controlling, the harbour, offering insight into possible hazards the future might hold. A total of 23 harbour-crossing seismic lines were collected between Taiaroa Head an the Leith Canal covering the majority of Otago Harbour. These lines were processed and refined to produce cross sections of the harbour, imaging from the upper sediments right down to the bedrock. The resulting data were then used to produce a 3D model of the paleovalley’s bedrock contact, as well as allowing the identification of major depositional horizons within the sediment. From this modelling and analysis, interpretations related to sedimentary time scales, erosional processes and faulting were made. The paleovalley 3D model showed far deeper depths (upto 160m) than imaged by previous studies, as well as providing evidence to support a time scale for the erosional valley’s formation. Evidence such as the merging of multiple small channels and shallowing paleovalley depths near the centre of the harbour, indicated a paleovalley formed by the erosion of two rivers out from a paleowatershed, situated above today’s Portobello Peninsula and Quarantine and Goat Islands. The 3D model also allowed a calculation of a stored sediment volume which exceeded previous estimates by ~37%. The harbour cross sections supported correlation of past depositional events with major sea level rise on two possible time scales (Pleistocene and Post Glacial). These same depositional horizons also exhibited possible offsets and slumping which sets the foundations for future studies into possible faulting in the harbour. Many of these findings provide insight into the possible future of Otago Harbour, constraining possible transgressional rates as well as identify indicators of a possibly active fault, both which could have a significant impact in terms of hazard assessments and the overall sustainability of Dunedin’s coastal setting. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Otago Harbour Dunedin Thesis description Number of pages, maps, CDs, etc. 145 pages A4 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 2016Fletcher Creator An entity primarily responsible for making the resource Fletcher, Patrick T. Date A point or period of time associated with an event in the lifecycle of the resource 2016 Title A name given to the resource The geological evolution of Otago Harbour: a high-resolution seismic reflection study Subject The topic of the resource Geophysics Sedimentology Controlled source seismology https://theses.otagogeology.org.nz/files/original/2b60a80c6a278a0d174dd2251e3ef26c.pdf f0a9683a49921b0022fe5e4794ab1435 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 ((170.679218834379611 -45.670042188554518,170.855272927038868 -45.462716745033383,171.036352817015455 -45.364756165144449,171.278982924852983 -45.385342375258553,170.769774737987035 -45.699234243271711,170.679218834379611 -45.670042188554518)) Author last name Last name of the Author van Haastrecht Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? BSc(Hons) Advisers Who supervised/advised this student Gorman, A.R. Abstract The Abstract for this thesis The Waihemo Fault System is a major crustal-scale structure that forms the northern boundary of the active north-east striking ranges of Otago, New Zealand. The fault system on the east coast of the South Island is orthogonal to the coast but its offshore geometry is poorly understood. The Waihemo Fault System originated in the Cretaceous as a set of crustal-scale northeast trending normal faults that reactivated as reverse faults in the Late Cenozoic. This study investigates the offshore extent of the Waihemo Fault System, how it changes offshore, and how this compares to the known nature of the onshore fault system. Three multichannel seismic data sets were used in a comparison study to characterise the offshore section of the Waihemo Fault System. Petroleum industry exploration data from the 1980s were compared to recent seismic data from 2012 (RV Kaharoa 48-channel data with a generator-injector airgun source) and 2014 (RV Polaris II 24-channel data with a boomer source), with notably different depth penetration scales and seismic resolutions. The Waihemo Fault System can be seen to extend from the basement through the overlying Tertiary sedimentary units, with the Shag Point Anticline visible on the northern side. The new high-resolution data, as well as the older exploration data, appear to partially confirm previously suggested offshore segment fault models, and extend the fault system further offshore. Strands of the Waihemo Fault System are shown to continue from onshore to offshore away from the coast with an approximate northwest-southeast strike. Within the first 5 km offshore, two fault strands are inferred to merge together with a larger main strand. Small conjugate faulting is present on the main strand; however, is discontinuous and did not produce a surface trace. A southeast plunging, anticlinal structure in the hanging wall was imaged, with lateral offset by the Waihemo Fault System. A gas feature is visible on two of the seismic lines. A previously inferred extension of the Titri Fault System in the area, running parallel to the coastline and extending from south of Dunedin, was not imaged but remains a possibility. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Canterbury Basin Offshore Otago Thesis description Number of pages, maps, CDs, etc. xiv, 69 pages A4, seismic lines in back 8 250mm high, ~1m wide 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 2014van_Haastrecht Creator An entity primarily responsible for making the resource van Haastrecht, Laurine Nathalie (Laurine) Date A point or period of time associated with an event in the lifecycle of the resource 2014 Title A name given to the resource Seismic imaging of the Waihemo Fault System in the southern Canterbury Basin off coastal Otago Subject The topic of the resource Geophysics Controlled source seismology offshore faults Shag Point Anticline Waihemo Fault System