1 10 2 https://theses.otagogeology.org.nz/files/original/86891e36a68eaf0e97c3f071505743aa.pdf 8a568051a0d6e510ef7301a7fcf113a4 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 ((171.796770978073795 -42.271332177875628,171.824714226861687 -42.280057280274768,171.820752412595425 -42.286021393864409,171.792424881646554 -42.27714831251911,171.796770978073795 -42.271332177875628)) Author last name Last name of the Author Dickie Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? BSc(Hons) Advisers Who supervised/advised this student Scott, J.M. Abstract The Abstract for this thesis This study presents the first comprehensive analysis of intrusion-related mineralisation within the Reefton Goldfield. Following field, petrographic, EDS, whole rock, LA-ICP-MS and zircon dating analysis, a number of findings relating to both the role and formation of intrusion-related mineralisation in the Reefton Goldfield have been made. The role of granitic intrusions in relation to orogenic gold mineralisation within the Reefton goldfield, New Zealand, is poorly understood. A porphyritic granitic dike intrudes Greenland Group metasediments in the western limb of a north-trending, tightly folded syncline just west of the economically significant historic Blackwater mine. Abundant sulphide-bearing stockwork veins surrounding the granitoid dike define an alteration zone consisting predominately of pyrite ± chalcopyrite with accessory sphalerite ± molybdenite ± arsenopyrite ± galena ± millerite. While gold has not been observed in the alteration zone, it is above background levels, and plentiful molybdenite could be of economic interest. Analysis of the dike and surrounding alteration halo has elucidated the timing and conditions in which mineralisation occurred. Intrusion-related mineralisation occurred following emplacement of the Blackwater Dike into the shallow crust during the Early Cretaceous (119 Ma U-Pb zircon). Prograde contact metamorphism to of Greenland Group country rock was coeval with solidification of the dike. Crystallisation of the Blackwater Dike, led to the development of an aqueous phase with sufficient ore metals bound with chloride, reduced sulphur and other aqueous species to give rise to base metal deposit. Abundant sulphidation consisting of a variable assemblage of pyrite, molybdenite, chalcopyrite, arsenopyrite, sphalerite, galena, and millerite precipitated in association with propylitic and phyllic alteration of the dike and host rock during retrograde alteration. Zoning of alteration assemblages provide a history for the dike localized mineralisation, as rapid cooling from convection and pH increased from wall rock reactions facilitated bulk sulphide precipitation between ~400-200 oC. Trace element analysis of pyrite from Blackwater Dike and surrounding alteration halo to those associated with shear-related mineralisation, suggests that magmatic hydrothermal fluid associated with the dike is not related to gold mineralisation in the Reefton Goldfield. Mineralisation assemblages from the Blackwater Dike alteration halo suggest that it is not related to gold mineralisation in the broader Reefton Goldfield Shear-related mineralisation has a much greater abundance of trace gold within pyrite grains analysed suggesting magmatic fluids sourced from the Blackwater Dike have little role to play in mineralising gold. However, based on the dispersed high sulphidation seen within the Blackwater Dike alteration halo, magmatic hydrothermal systems may have some role to play in remobilizing gold throughout the Reefton Goldfield. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Westland Reefton South Reefton Goldfield Thesis description Number of pages, maps, CDs, etc. 133p 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 2015Dickie Creator An entity primarily responsible for making the resource Dickie, James Edward, 1991 (Jim) Date A point or period of time associated with an event in the lifecycle of the resource 2015 Title A name given to the resource Timing and conditions of mineralisation of the Blackwater Dike, Reefton Goldfield, Westland, New Zealand Subject The topic of the resource Geochemistry Metamorphic geology Metamorphic petrology Mineralogy Ore deposits Alteration chalcopyrite Cretaceous Greenland Group Hydrothermal Intrusion-related mineralisation Molybdenite Porphyry pyrite Reefton goldfield Sulphides Western Province https://theses.otagogeology.org.nz/files/original/470051eb844d86ccd2e68e7a0d787e46.pdf 1424c8fe83a6d3e0565a11d17f45a40a 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 ((170.03288015343864 -45.326151565245354,170.06841811816804 -45.228897382181607,170.168130449338037 -45.229986350473176,170.261550301047464 -45.270897104090764,170.258762661429103 -45.307746037440886,170.124378972385955 -45.306106250860822,170.082433400924543 -45.327667384041703,170.03288015343864 -45.326151565245354)) Author last name Last name of the Author Dickie Project type Is it an MSc, PhD, BSc(Hons) or PGDipSci? BSc(Hons) Advisers Who supervised/advised this student Sibson, R Abstract The Abstract for this thesis The Rock and Pillar Range, Central Otago, is an anticlinal box structure, formed during regional contraction in the Late Cenozoic. All Tertiary sediments have been eroded off the top of the range to expose basement Otago Schist. A sequence of Terrestrial Tertiary sediments; Dunstan Formation, Bannockburn Formation, Wedderburn Formation and Maniototo Conglomerate, at the base of the range have also been buckled in the late Cenozoic contraction. Several outcrops of Miocene basaltic lava flows of the Waipiata Volcanics overlie both the Dunstan and Bannockburn Formations. The Dunstan Formation in this area contains four different populations of quartz sand grains, which originate.from two different provenances; the Haast Schist and a granitic source. Striking E-W across the north end of the range for approximately 11 km is a -14 ° northdippingfault, the Pig Burn Fault (PBF) (new name)that juxtaposes low-grade schist in the hangingwall against high-grade schist in the footwall, indicating normal displacement. The hangingwall block is characterised by extensive brittle fracturing of the schist, which ranges from textural zone (TZ) 1 to 3A, and vertical extension veins filled with carbonate that strike parallel to the fault. The footwall block comprises TZ 3B schist and a -50 m thick mylonite zone adjacent to the fault. Displacement on the fault is estimated at -35 km dowri dip to the north. this is a very low-angle normal fault of regional extent, which shows most of the characteristic features, as described above, of a metamorphic core complex. The timing of this event is uncertain but must predate or partly overlap with cutting of the regional W aipounamu Erosion Surface during the Late Cretaceous. Limited ·structural· data suggests the probability that the very low-angle normal faulting formed along a zone of earlier reverse movement. There are similarities between the features and positions of the Pig Burn Fault and the Hyde-Macraes Shear Zone that suggest that they may be the same structural contact. Department The department where the student is studying primarily. Geology Named locality Named locality describing the field area location. Rock and Pillar Range Thesis description Number of pages, maps, CDs, etc. vi, 110, [4] p. : ill. (some col.), maps (some col., some folded) ; 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 1999Dickie Creator An entity primarily responsible for making the resource Dickie, Benjamin John, 1978- Date A point or period of time associated with an event in the lifecycle of the resource 1999 Title A name given to the resource Rock and pillar geology, Central Otago, New Zealand Subject The topic of the resource Structural geology east Otago faults Otago Schists