Geochemistry of a silver-lead-zinc hydrothermal system : ore genesis for the McKay Hill and Horseshoe Hill silver claims in Yukon, Canada
McKay Hill is located in the Ogilvie Mountains, 50 km north of Keno City, Yukon, Canada. The Wernecke Supergroup was deformed by Late Jurassic and Early Cretaceous arc magmatism and orogeny. Mineral phase identification was performed on 14 ore and 15 gangue samples from McKay Hill and Horseshoe Hill...
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ftballstcs:oai:https://cardinalscholar.bsu.edu:20.500.14291/200712 2024-06-09T07:48:50+00:00 Geochemistry of a silver-lead-zinc hydrothermal system : ore genesis for the McKay Hill and Horseshoe Hill silver claims in Yukon, Canada Title on signature form: Geochemistry of a silver-lead-zinc hydrothermal system :|bore genesis for the McKay and Horseshoe Hill silver claims in Yukon, Canada Lara, Hernan Javier Nicholson, Kirsten N. 2017-05-06 application/pdf http://cardinalscholar.bsu.edu/handle/20.500.14291/200712 https://hdl.handle.net/20.500.14291/200712 http://liblink.bsu.edu/uhtbin/catkey/1851712 unknown http://liblink.bsu.edu/uhtbin/catkey/1851712 http://cardinalscholar.bsu.edu/handle/20.500.14291/200712 Silver ores -- Yukon -- Ogilvie Mountains -- Composition Hydrothermal alteration -- Yukon -- Ogilvie Mountains Geochemistry -- Yukon -- Ogilvie Mountains 2017 ftballstcs https://doi.org/20.500.14291/200712 2024-05-15T15:54:41Z McKay Hill is located in the Ogilvie Mountains, 50 km north of Keno City, Yukon, Canada. The Wernecke Supergroup was deformed by Late Jurassic and Early Cretaceous arc magmatism and orogeny. Mineral phase identification was performed on 14 ore and 15 gangue samples from McKay Hill and Horseshoe Hill using the x-ray diffractometer MiniFlex 600. Centrifugation was conducted to align clay minerals along the one-dimensional plane from their crystal faces and to disperse the silt and sand grains. XRF analysis was performed on the Rigaku NEX QC X-ray fluorescence analyzer to determine the chalcophile elements and transition elements. Horseshoe is a basalt, consisting of clinopyroxene (25%), orthopyroxene (9%), plagioclase (31%). McKay Hill is a basalt, consisting of clinopyroxene (20%), orthopyroxene (9%), and plagioclase (30%). Ore minerals include argentite and freibergite. The fugacity of oxygen in tholeiitic magmatic series was controlled by the ilmenite series. Dublin Gulch and McKay Hill show consistent orientation due to the presence of the McQuesten Anticlinorium in western Selwyn Basin. Assessing the anomalies in spidergrams, it could be inferred that Eu2+ substitutes for Ca2+ due to its ionic potential. This Cordilleran Ag-Pb-Zn vein deposit is distinguished by the distribution of refractory metals (Ti, Zr, Cr) and pervasive alteration. Thesis (M.S.) Department of Geological Sciences Methods -- Petrographic data -- Aluminosilicate XRD data -- XRF data : introduction -- Discussion. Other/Unknown Material Ogilvie Mountains Yukon Ball State University: Cardinal Scholar Yukon Canada Gulch ENVELOPE(-61.483,-61.483,-63.997,-63.997) Selwyn ENVELOPE(-138.287,-138.287,62.799,62.799) Ogilvie ENVELOPE(-139.746,-139.746,63.563,63.563) Ogilvie Mountains ENVELOPE(-138.254,-138.254,64.583,64.583) Wernecke ENVELOPE(-135.271,-135.271,63.952,63.952) Dublin Gulch ENVELOPE(-135.804,-135.804,64.043,64.043) McQuesten ENVELOPE(-137.410,-137.410,63.554,63.554) |
institution |
Open Polar |
collection |
Ball State University: Cardinal Scholar |
op_collection_id |
ftballstcs |
language |
unknown |
topic |
Silver ores -- Yukon -- Ogilvie Mountains -- Composition Hydrothermal alteration -- Yukon -- Ogilvie Mountains Geochemistry -- Yukon -- Ogilvie Mountains |
spellingShingle |
Silver ores -- Yukon -- Ogilvie Mountains -- Composition Hydrothermal alteration -- Yukon -- Ogilvie Mountains Geochemistry -- Yukon -- Ogilvie Mountains Lara, Hernan Javier Geochemistry of a silver-lead-zinc hydrothermal system : ore genesis for the McKay Hill and Horseshoe Hill silver claims in Yukon, Canada |
topic_facet |
Silver ores -- Yukon -- Ogilvie Mountains -- Composition Hydrothermal alteration -- Yukon -- Ogilvie Mountains Geochemistry -- Yukon -- Ogilvie Mountains |
description |
McKay Hill is located in the Ogilvie Mountains, 50 km north of Keno City, Yukon, Canada. The Wernecke Supergroup was deformed by Late Jurassic and Early Cretaceous arc magmatism and orogeny. Mineral phase identification was performed on 14 ore and 15 gangue samples from McKay Hill and Horseshoe Hill using the x-ray diffractometer MiniFlex 600. Centrifugation was conducted to align clay minerals along the one-dimensional plane from their crystal faces and to disperse the silt and sand grains. XRF analysis was performed on the Rigaku NEX QC X-ray fluorescence analyzer to determine the chalcophile elements and transition elements. Horseshoe is a basalt, consisting of clinopyroxene (25%), orthopyroxene (9%), plagioclase (31%). McKay Hill is a basalt, consisting of clinopyroxene (20%), orthopyroxene (9%), and plagioclase (30%). Ore minerals include argentite and freibergite. The fugacity of oxygen in tholeiitic magmatic series was controlled by the ilmenite series. Dublin Gulch and McKay Hill show consistent orientation due to the presence of the McQuesten Anticlinorium in western Selwyn Basin. Assessing the anomalies in spidergrams, it could be inferred that Eu2+ substitutes for Ca2+ due to its ionic potential. This Cordilleran Ag-Pb-Zn vein deposit is distinguished by the distribution of refractory metals (Ti, Zr, Cr) and pervasive alteration. Thesis (M.S.) Department of Geological Sciences Methods -- Petrographic data -- Aluminosilicate XRD data -- XRF data : introduction -- Discussion. |
author2 |
Nicholson, Kirsten N. |
author |
Lara, Hernan Javier |
author_facet |
Lara, Hernan Javier |
author_sort |
Lara, Hernan Javier |
title |
Geochemistry of a silver-lead-zinc hydrothermal system : ore genesis for the McKay Hill and Horseshoe Hill silver claims in Yukon, Canada |
title_short |
Geochemistry of a silver-lead-zinc hydrothermal system : ore genesis for the McKay Hill and Horseshoe Hill silver claims in Yukon, Canada |
title_full |
Geochemistry of a silver-lead-zinc hydrothermal system : ore genesis for the McKay Hill and Horseshoe Hill silver claims in Yukon, Canada |
title_fullStr |
Geochemistry of a silver-lead-zinc hydrothermal system : ore genesis for the McKay Hill and Horseshoe Hill silver claims in Yukon, Canada |
title_full_unstemmed |
Geochemistry of a silver-lead-zinc hydrothermal system : ore genesis for the McKay Hill and Horseshoe Hill silver claims in Yukon, Canada |
title_sort |
geochemistry of a silver-lead-zinc hydrothermal system : ore genesis for the mckay hill and horseshoe hill silver claims in yukon, canada |
publishDate |
2017 |
url |
http://cardinalscholar.bsu.edu/handle/20.500.14291/200712 https://hdl.handle.net/20.500.14291/200712 http://liblink.bsu.edu/uhtbin/catkey/1851712 |
long_lat |
ENVELOPE(-61.483,-61.483,-63.997,-63.997) ENVELOPE(-138.287,-138.287,62.799,62.799) ENVELOPE(-139.746,-139.746,63.563,63.563) ENVELOPE(-138.254,-138.254,64.583,64.583) ENVELOPE(-135.271,-135.271,63.952,63.952) ENVELOPE(-135.804,-135.804,64.043,64.043) ENVELOPE(-137.410,-137.410,63.554,63.554) |
geographic |
Yukon Canada Gulch Selwyn Ogilvie Ogilvie Mountains Wernecke Dublin Gulch McQuesten |
geographic_facet |
Yukon Canada Gulch Selwyn Ogilvie Ogilvie Mountains Wernecke Dublin Gulch McQuesten |
genre |
Ogilvie Mountains Yukon |
genre_facet |
Ogilvie Mountains Yukon |
op_relation |
http://liblink.bsu.edu/uhtbin/catkey/1851712 http://cardinalscholar.bsu.edu/handle/20.500.14291/200712 |
op_doi |
https://doi.org/20.500.14291/200712 |
_version_ |
1801380740814864384 |