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Dissertations / Theses on the topic 'Volcanogenic massive sulfide'

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Published: 4 June 2021

Last updated: 1 February 2022

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1

Hettula, J. (Jesse). "Pyhäsalmi volcanogenic massive sulfide deposit, central Finland." Bachelor's thesis, University of Oulu, 2017. http://urn.fi/URN:NBN:fi:oulu-201710253010.

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Pyhäsalmi mine is located in central Finland, at the eastern side of the Pyhäjärvi lake. The Pyhäsalmi deposit is polymetallic Zn-Cu VMS ore body with total reserve, mined and yet to be mined, of 58.3 Mt @ Cu 0.9 %, Zn 2.4 %, S 37.8 %, Au 0.4 g/t and Ag 14 g/t. At the end of 2013, 51 Mt of ore has been mined. The mine will be in operation until August of 2019. The Pyhäsalmi deposit is hosted in a felsic-dominated bimodal Proterozoic succession. Local hydrothermal alteration is composed of sericite-quartz alteration, and intensifies when it is in close proximity with the upper ore body. The de

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2

Miranda, Gasca Miguel Angel. "The volcanogenic massive sulfide and sedimentary exhalative deposits of the Guerrero Terrane, Mexico." Diss., The University of Arizona, 1995. http://hdl.handle.net/10150/187087.

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More than 60 volcanogenic massive sulfide and sedimentary exhalative deposits are located in the composite upper Jurassic-lower Cretaceous Guerrero terrane of western Mexico. The deposits range from less than 100,000 metric tons up to 6 million metric tons. Most of the deposits are Zn-Pb-Cu Kuroko type and are located within the Zihuatanejo and Teloloapan subterranes. The Guanajuato and Calmalli, Baja California, deposits are Zn-Cu. The Cu type Copper King, Guerrero, deposit is located in the Papanoa complex. Arroyo Seco, Michoacan, is the only Pb-type and can be classified as a sedimentary-ex

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3

Lalonde, Erik. "Alteration and Cu-Zn mineralization of the turgeon volcanogenic massive sulfide deposit (New Brunswick, Canada)." Thesis, Université Laval, 2014. http://www.theses.ulaval.ca/2014/30505/30505.pdf.

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Le gîte Turgeon est un sulfure massif volcanogène (SMV) riche en Cu-Zn, encaissé dans les roches volcano-sédimentaires ordoviciennes du Groupe de Fournier dans la Boutonnière Elmtree-Belledune, au Nouveau-Brunswick (Canada). Le Groupe de Fournier comprend les formations Devereaux et Pointe Verte, qui sont tous les deux composées de gabbros et de basaltes cousinés. Le gîte Turgeon est composé de deux lentilles de sulfures massifs Cu-Zn avec des stockwerks chalcopyrite-pyrite sous-jacents aux deux lentilles. La géochimie indique que les roches encaissantes sont des basaltes et des andésites d’af

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4

van, Hees Gregory W. H. "Chemostratigraphy and Alteration Geochemistry of the Lundberg and Engine House Volcanogenic Massive Sulfide Mineralization, Buchans, Central Newfoundland." Thesis, Université d'Ottawa / University of Ottawa, 2012. http://hdl.handle.net/10393/20659.

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The world-class Buchans Mining Camp hosts a number of high-grade, low-tonnage volcanogenic massive sulfide (VMS) deposits. The Lundberg and Engine House zones form the lower-grade stockwork to the Lucky Strike deposit and have yet to be mined. A detailed study of the Lundberg and Engine House zones was conducted to establish the stratigraphic setting of the deposits, to determine the petrology of the host volcanic rocks and distribution of alteration facies, and to characterize the mineralization with the goal of improving exploration for polymetallic massive sulfide deposits in the Buchans ca

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5

Ruks, Tyler William. "Stratigraphic and paleotectonic studies of Paleozoic Wrangellia and its contained volcanogenic massive sulfide (VMS) occurrences, Vancouver Island, British Columbia, Canada." Thesis, University of British Columbia, 2015. http://hdl.handle.net/2429/54599.

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Wrangellia is a fundamental component of the North American Cordillera and contains significant mineral deposits, including Myra Falls (Nyrstar N.V.), which is currently the largest producing volcanogenic massive sulfide (VMS) deposit in western Canada. Understanding the evolution of Wrangellia is therefore important for understanding the crustal growth and metallogenic history of the North American continent, and in doing so, facilitating the discovery of new mineral wealth. Geochronological, lithogeochemical and Nd and Pb isotopic studies of the Paleozoic Wrangellia arc (PWA), Vancouver Isla

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6

Gemmell, Thomas P. "Geology of the Kidd Creek Deep Orebodies - Mine D, Western Abitibi Subprovince, Canada." Thèse, Université d'Ottawa / University of Ottawa, 2013. http://hdl.handle.net/10393/26116.

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The giant Kidd Creek Mine is an Archean Cu-Zn-Ag deposit in the Abitibi Greenstone belt, located in the Superior Province of Canada and is one of the largest known base metal massive sulfide mines in the world with a tonnage of 170.7 Mt (Past production, Resource and Reserve). The massive sulfides in Mine D comprise a number of ore lenses that are interpreted to be the downplunge continuation of the Central orebody from the upper mine. These are referred to as the West, Main, and South lenses. The massive sulfides overlie a silicified rhyolitic unit at the top of a mixed assemblage of rhyolite

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7

Wilson, Ryan. "Hydrothermal Fe-Carbonate Alteration Associated with Volcanogenic Massive Sulfide (VMS) Deposits in Cycle IV of the Noranda Mining Camp, Rouyn-Noranda, Quebec." Thèse, Université d'Ottawa / University of Ottawa, 2012. http://hdl.handle.net/10393/22838.

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Massive sulfide deposits in the Noranda mining camp, northwestern Québec, are mainly associated with extensive footwall alteration defined by intense chloritization and sericitization. However, Fe-carbonate alteration also occurs in proximity to some deposits. To test the exploration significance of carbonate alteration in the camp, two areas of intense carbonate alteration were examined, around the small Delbridge deposit and near the new Pinkos occurrence in the Cyprus Rhyolite. Between 1969 and 1971, the Delbridge deposit produced 370,000 t of ore grading 9.6% Zn, 0.61% Cu, 110 g/t Ag, and

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8

Jamieson, John William. "Tracing sulfur sources in an Archean hydrothermal system using sulfur multiple isotopes a case study from the Kidd Creek volcanogenic massive sulfide deposit /." College Park, Md. : University of Maryland, 2005. http://hdl.handle.net/1903/2697.

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Thesis (M.S.) -- University of Maryland, College Park, 2005<br>Thesis research directed by: Geology. Title from t.p. of PDF. Includes bibliographical references. Published by UMI Dissertation Services, Ann Arbor, Mich. Also available in paper.

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9

Steeves, Nathan. "Mineralization and Alteration of the Late Triassic Glacier Creek Cu-Zn VMS Deposit, Palmer Project, Alexander Terrane, Southeast Alaska." Thèse, Université d'Ottawa / University of Ottawa, 2013. http://hdl.handle.net/10393/23654.

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The Glacier Creek volcanogenic massive sulfide (VMS) deposit is hosted within Late Triassic, oceanic back-arc or intra-arc, rift-related, bimodal volcanic rocks (Hyd or Tats Group) of the allochthonous Alexander terrane known as the Alexander Triassic Metallogenic Belt (ATMB). The deposit presently consists of four tabular massive sulfide lenses with a resource of 4.75 Mt. at 1.84% Cu, 4.57% Zn, 0.15% Pb, 0.28 g/t Au and 29.07 g/t Ag. A deposit-scale thrust fault offsets stratigraphy along the axial surface of a deposit-scale anticline. The massive sulfide lenses are barite-rich and are div

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10

Prior, Glen James Carleton University Dissertation Earth Sciences. "Volcanology and geochemistry of archean rhyolites and related volcaniclastic rocks associated with the Kidd Creek volcanogenic massive sulfide deposit, Abitibi Greenstone Belt, Superior Province, Canada." Ottawa, 1996.

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11

Drieberg, Susan L. "The magmatic-hydrothermal architecture of the Archean Volcanic Massive Sulfide (VMS) System at Panorama, Pilbara, Western Australia." University of Western Australia. School of Earth and Geographical Sciences, 2003. http://theses.library.uwa.edu.au/adt-WU2004.0064.

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[Truncated abstract. Formulae and special characters can only be approximated here. Please see the pdf version of this abstract for an accurate representation.] The 3.24 Ga Panorama VMS District, located in the Pilbara Craton of Western Australia, is exposed as a cross-section through subvolcanic granite intrusions and a coeval submarine volcanic sequence that hosts Zn-Cu mineralization. The near-complete exposure across the district, the very low metamorphic grade, and the remarkable preservation of primary igneous and volcanic textures provides an unparalleled opportunity to examine the P-

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12

Schmandt, Danielle. "Mineralogy and origin of Zn-rich horizons within the arctic volcanogenic massive sulfide deposit, Ambler District, Alaska." 2009. http://hdl.handle.net/10090/8994.

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13

Danielson, Thomas J. "Age, paleotectonic setting, and common Pb isotope signature of the San Nicolás volcanogenic massive sulfide deposit, southeastern Zacatecas State, central Mexico." Thesis, 2001. http://hdl.handle.net/2429/11279.

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The San Nicolas deposit is a world class polymetallic volcanogenic massive sulfide (VMS) deposit located in southeastern Zacatecas State, central Mexico. The location of the deposit in a metallogenic province previously thought to be barren with respect to VMS mineralization, coupled with the large size of the deposit, make understanding the framework within which the deposit formed important for further mineral exploration efforts in the region, as well as for providing a more complete understanding of the geology of the region. A geological, geochronological, lithogeochemical, and isot

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14

Grant, Hannah Lucy Jane. "The distribution and controls on silver mineralization in the Main Zone of the 2.68 Ga Archean Hackett River Zn-Pb-Cu-Ag volcanogenic massive sulfide (VMS) deposit, Nunavut, Canada." Thesis, 2009. http://hdl.handle.net/1974/1719.

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The 2.68 Ga Zn-Pb-Cu-Ag Hackett River Main Zone (HRMZ) volcanogenic massive sulfide (VMS) deposit, within the Hackett River Greenstone Belt of the Archean Slave Craton is highly enriched in Ag (and Pb) compared to other VMS deposits of a similar age and type. The mineralization has been sub-divided into five categories based on mineralogy, textures and stratigraphic location: 1) disseminated footwall sulfides, 2) copper-rich stringer sulfides, 3) pyrite-poor sphalerite-pyrrhotite-chalcopyrite mineralization located at the top of the stringer zone, 4) mineralization in calc-silicate altered uni

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15

Crowe, Douglas Edward. "Geochemistry of volcanogenic massive sulfide and high-grade Au granite-hosted ore deposits, southern Alaska ; and, Development and application of laser microprobe techniques for analysis of sulfur, carbon and oxygen isotope ratios." 1990. http://catalog.hathitrust.org/api/volumes/oclc/23277076.html.

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Thesis (Ph. D.)--University of Wisconsin--Madison, 1990.<br>Typescript. Four plates on folded leaves in pocket. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references.

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16

Weick, Reinhold James. "Petrography and stable isotope geochemistry of alteration and mineralization in the Rambler volcanogenic massive sulphide deposit, Baie Verte, Newfoundland /." 1993. http://collections.mun.ca/u?/theses,74228.

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