1 10 2 https://theses.otagogeology.org.nz/files/original/59297ccdb41ffb21d7f5448a9e56ac36.pdf 0a79b5a6c0bf607323945b0db0053bbd 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 ((163.063226984762508 -78.364465528103011,163.056438554277065 -78.364474041634281,163.056563437798815 -78.363077275439778,163.057006578052523 -78.35811837509975,163.059220573182643 -78.333280402512472,163.06191456612342 -78.302916202400823,163.22784843912882 -78.302971914014805,163.328947990762572 -78.30295912052604,163.326109749356448 -78.31851218207197,163.323518629202766 -78.332675493362686,163.31775999346786 -78.364031735648737,163.24448227080552 -78.364179498978643,163.232059564208953 -78.364202714882524,163.167458492236449 -78.364314874391326,163.063226984762508 -78.364465528103011)) Author last name Last name of the Author Aslund Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? MSc Advisers Who supervised/advised this student Craw, D. Abstract The Abstract for this thesis The area studied is located within the Dromedary massif, southern Victoria Land, Antarctica. The geology of this region includes a number of pre-metamorphic mafic intrusives within Koettlitz Group metasediments, which are the focus of the present study. The Dromedary gabbro is a composite body comprising several tholeiitic anorthositic and gabbroic plutons, and an olivine-bearing alkaline gabbro. Subsequent amphibolite facies metamorphism and deformation of Dromedary gabbro were strongly influenced by original rock composition. The Glee intrusives, a collection of dismembered hybrid intrusive rocks, represent mixing of a mafic magma with a Kspar phenocryst-bearing granitic magma. Glee intrusive whole rock geochemical trends are compatible with trends predicted using a simple linear endmember mixing model. This suggests the Glee mafic endmember was similar in composition to alkaline Dromedary gabbro. Pyroxene-bearing quartz diorite exposed south of Renegar Glacier and diorite intruded into Dromedary gabbro is similar in composition to some Glee intrusives and were possibly also generated by mixing of two magmas. A body of iron-rich nepheline syenite was emplaced into marble northwest of Mt Dromedary. Studies suggest assimilation of marble influenced oxygen isotopic composition of the syenite and encouraged the development of garnet-albite-amphibole coronas around pyroxene, but did not result in generation of substantial quantities of nepheline. Pre-metamorphic intrusive lithologies exposed in the Mt Dromedary region are compatible with anorogenic magmatism and may represent a rifting or failed rifting event which occurred prior to the compressional "Ross Orogeny". OURArchive handle The handle from the Otago University Research Archive (OURArchive) <a href="http://hdl.handle.net/10523/2936">http://hdl.handle.net/10523/2936</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. Dromedary Massif Renegar Glacier Antarctica Thesis description Number of pages, maps, CDs, etc. iv, 109 p. : ill. (some col.), maps (some col.) ; 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 1990Aslund Creator An entity primarily responsible for making the resource Aslund, Tania, 1966- Date A point or period of time associated with an event in the lifecycle of the resource 1990 Title A name given to the resource Magmatism and metamorphism of mafic intrusives of the Dromedary massif, Antarctica Subject The topic of the resource Geochemistry Metamorphic geology Granite Harbour Intrusives Igneous petrology mafic inclusions magmatism https://theses.otagogeology.org.nz/files/original/870e493ffb825084679c6cdc8c685122.pdf 2f5c023cf699493e0a22d0db02bc8feb 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 ((167.983212910194766 -45.854689460774829,167.902637199005682 -45.848732478229493,167.910223938552264 -45.788100179206516,167.992112851647761 -45.793633390413497,167.983212910194766 -45.854689460774829)) Author last name Last name of the Author Aslund Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? BSc(Hons) Advisers Who supervised/advised this student Landis, C.A. Abstract The Abstract for this thesis An area approximately 40km2, 10km north of Ohai, western Southland was mapped in detail. The area is roughly divided in two by the Tin Hut Fault, which is steeply dipping and strikes N-S. Rocks to the west of the fault comprise steeply eastward dipping, eastward facing volcaniclastic sediments of the Elbow Formation, Takitimu Group. To the east are rocks of the Caravan Formation, characterised by distinctive pyroxene-phyric basalts and two-pyroxene andesites intruding volcaniclastic sediments. In the southern part of the area, the Caravan strata have been overturned and now face south. To the north Caravan sediments are right way up and facing east. The genetic relationship between Takitimu Group and the Caravan Formation is uncertain. Productus Creek Group, an eastward dipping, richly fossiliferous Permian marine sequence, depositionally overlies the Caravan Formation. Together they comprise the Caravan 'subterrane'. Trapped between Takitimu and Caravan in the northern part of the area is a wedge of Lower Triassic Murihiku sediments and associated melange (Tin Hut Melange). The presence of this infaulted sliver places a lower limit on the timing of juxtaposition of the Caravan subterrane and Takitimu terrane. Emplacement of the Beaumont Intrusives (porphyritic hornblende-andesite) and an olivine monzonite dyke, both of which are found intruding Takitimu and Caravan rocks, post-dates any major strike-slip fault movement. The Caravan subterrane and intrusions are unconformably overlain by the Barretts Formation, a Jurassic conglomerate-sandstone sequence up to 200m thick, containing volcanic, plutonic and minor metamorphic detritus. Cretaceous Ohai Group sediments are faulted against Elbow Formation rocks in the NW. Ohai Group sediments are not found overlying Caravan subterrane, Murihiku Supergroup, Barretts Formation or melange. Murihiku Supergroup sediments have been thrust over Barretts Formation from the east along the Letham Ridge Thrust. Wairaki Melange crops out intermittently along the trace of this low angle fault. It comprises highly veined, deformed, fossiliferous blocks of Permian age in a sheared siltstone matrix. Triassic sediments also appear to have been incorporated in places. QFL data from Barretts sandstones show a range of compositions, from relatively quartzofeldspathic (e.g. QFL- 34:43:23) to lithic-rich (e.g. 3:35:62) sandstones, which are remarkably similar to that of Jurassic, as well as Middle and Upper Triassic Murihiku sandstones. Heavy mineral assemblages are also similar: both contain clinopyroxene, biotite, hornblende, muscovite, epidote, opaques, and rare garnet and titanite. In contrast, Lower Triassic Murihiku sandstones plot in a confined QFL field (average QFL- 3:47:50), and heavy mineral assemblages are comprised dominantly of epidote and opaques. I suggest that the arc which supplied material to the Murihiku depositional basin also contributed detritus to the Jurassic Barretts Formation. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Beaumont West Southland 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 1988Aslund Creator An entity primarily responsible for making the resource Aslund, T Date A point or period of time associated with an event in the lifecycle of the resource 1988 Title A name given to the resource Permian-Jurassic Relations, Beaumont Area, western Southland. Subject The topic of the resource Map Mineralogy Sedimentary petrology Geochemistry Barrets Formation Barretts Formation Beaumont Caravan Formation Jurassic Leatham Ridge Thrust Murihiku (provenance) arc Murihiku Terrane Ohai Group Productus Creek Terrane Southland Region Takiti Tin Hut Melange Wairaki Breccia Wairaki River