1 10 2 https://theses.otagogeology.org.nz/files/original/55193a1a3a439e651b57139dcf0cfb5d.pdf da47e2776b8d8df1e3ca3aaf80ad94b7 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 ((168.856722963000038 -45.024947921999967,168.860207193000065 -45.049148598999977,168.837163041000053 -45.073501008999983,168.825026821000051 -45.086311419999959,168.806758029000093 -45.085869919999936,168.799469689000034 -45.0856922899999,168.774824290000083 -45.054940572999953,168.771122949000073 -45.050318311999945,168.769992171000013 -45.048907433999943,168.754206016000012 -45.029186908999975,168.781692605000103 -45.01208130699996,168.807062766000058 -45.005426978999935,168.822178880000024 -45.001462204999939,168.824177801000019 -45.001660302999937,168.853792100000078 -45.004578263999974,168.856722963000038 -45.024947921999967)) Author last name Last name of the Author Cox 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 Four structural generations are recognised within Otago schist in a forty - five square kilometre area about the Remarkable Range, Central Otago, New Zealand. Initially bedding was isoclinally folded and transposed, producing an axial plane schistosity during the first structural generation, throughout which quartzofeldspathic segregations developed. During the second generation, psammitic schist of the Te Anau Assemblage was thrust over pelitic schist of the Aspiring lithologic association along a high strain zone developed at the base of the Remarkable nappe. Variations in deformation style and rotation of mesoscopic structures can be attributed to finite strain variation across the nappe: pre-existing linear features are rotated towards parallelism with the translation direction. A broad upright synform and a north - south trending fault system developed during the third and fourth generations respectively. Greenschist facies metamorphism accompanied development of first and second generation structures. Differences in kinetic coefficients of metamorphic reactions best accounts for variations in the abundance of zoned minerals between two adjacent isofacial regions. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Remarkables Thesis description Number of pages, maps, CDs, etc. vi. 58 p. ill. Photos. Map (folded 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 1985Cox Creator An entity primarily responsible for making the resource Cox, SC Date A point or period of time associated with an event in the lifecycle of the resource 1985 Title A name given to the resource Remarkable Geology. Subject The topic of the resource Map Metamorphic geology Structural geology high strain zone nappe Otago Schist structural rotation translation direction https://theses.otagogeology.org.nz/files/original/d7028dda7449699ff4b4c38ccfbb95e2.pdf faabae4b2fb4473e2d9e6ad0876356fd 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 ((168.667424133000054 -45.054978712999969,168.660706700000105 -45.056020936999971,168.659066718000076 -45.0562750199999,168.644430863000025 -45.058551861999945,168.501999625000053 -45.080560182999932,168.502410668000039 -45.079891157999953,168.534610983000107 -45.027366523999945,168.55717267600005 -44.990502998999943,168.560942286000113 -44.988448457999937,168.606213023000123 -44.963750259999983,168.614168517000053 -44.959405984999933,168.619111545000123 -44.964198191999969,168.629553274000045 -44.974321012999951,168.634025339000118 -44.978653121999969,168.634410295000066 -44.979023595999934,168.650030480000055 -44.99415608299995,168.683839596000098 -45.026870276999944,168.682437426000092 -45.046675233999963,168.682400342000051 -45.047219057999939,168.682310029000064 -45.048481830999947,168.682295391000025 -45.048679541999945,168.682009959000084 -45.052706128999944,168.668208889000084 -45.05485480599998,168.667424133000054 -45.054978712999969)) Author last name Last name of the Author Turnbull Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? BSc(Hons) Advisers Who supervised/advised this student Bishop, D.G. Campbell, J.D. Abstract The Abstract for this thesis (ABSTRACT of paper given at Geological Society of N.Z. Conference, November 29th, 1969) Schist Structure and Stratigraphy, Faulting and Tertiary Sedimentation in the Queenstown-Bob's Cove Area I.M. Turnbull University of Otago The schist in the Bob's Cove-Queenstown area grades from Chl II to Chl lV and is dividible into 3 stratigraphic units, one of which extends 30 miles to the north, Younging directions and mesoscopic folds in bedding and bedding foliation (termed F1 -folds) show that these units are on the overturned limb of a nappe-like fold with an axis plunging 45° SW and rooting to the NW. Another generation of folds in foliation (F3- folds) is developed close to major faults and individual folds can reach macroscopic proportions, F3 folds were developed during a period or sub-horizontal east-west compression which initiated movement on the Moonlight Fault and other major faults in the area. A new occurrence of marine Tertiary strata (?Landon) is mapped along the downthrown side of a newly-discovered major reverse fault (the 2 Mile Creek Fault) 5 miles E of, and parallel to, the Moonlight Fault. Another NNE-striking fault passes through the summit of Wedge Peak and a third parallels the S bank of 12 Mile Creek to be truncated by the Moonlight Fault. Landon rocks at Bob's Cove are bonded by the Moonlight Fault on the west and rest unconformably on sohist to the east. Lithological evidence shows that those sediments and those in the 2 Mile Creek and Moonlight Fault zones were derived from schist up thrown to the west during a second phase of movement on the Moonlight Fault. A marine connection of the Te Anau Basin is also postulated in some places, as at Bob's Cove, the sediments have been folded in F3 style by the latest period of fault movement in the area. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Bobs Cove Moke Creek Queenstown Thesis description Number of pages, maps, CDs, etc. 42 leaves, ill, photos, diagms, map (folded in pocket); 26 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 1969Turnbull Creator An entity primarily responsible for making the resource Turnbull, IM Date A point or period of time associated with an event in the lifecycle of the resource 1969 Title A name given to the resource Stratigraphy, Structure and Metamorphism in the Bob's Cove-Moke Creek-Queenstown Area, Lake Wakatipu. Subject The topic of the resource Map Lithostratigraphy Structural geology Metamorphic geology greenschist Moonlight Fault nappe pumpellyite