Masters Theses
Keywords and Phrases
Hydrous metasomatism; Ivrea-Verbano Zone; LA-ICP-TOF-MS; Magmatic sulfide deposit; Metal and volatile mass transfer; Ultramafic-mafic magmatism
Abstract
"Constraining the processes that control the transport and deposition of sulfides in the deep lithosphere is an important step in expanding ore deposit exploration search space to include exhumed lower crustal rocks. The ultramafic sulfide ore-bearing Valmaggia pipe in the Ivrea-Verbano Zone of NW Italy, an exhumed cross section of the overlying lower continental crust and subcontinental lithospheric mantle, gives critical insight into metallogenic processes in lower crustal settings. The ~300 m wide metasomatized pipe hosts Fe-Ni-Cu-(PGE±Co±Au) sulfide mineralization that is commonly associated with locally abundant carbonates and hydrous silicates (phlogopite, amphibole). Previous studies suggested that sulfides were physically transported into the pipe via vapor bubble flotation of sulfide droplets. In order to test this hypothesis, petrography is combined with electron microprobe analysis, and laser ablation time-of-flight ICP-MS trace element maps of sulfide/volatile relationships. Results show that sulfide textures vary between semi-massive to disseminated blebs that are commonly in textural or spatial relationship with volatiles. Carbonates and hydrous silicates exist in various and randomly distributed sizes, textures, orientations, and compositions in relation to sulfides. The data shows that bubble-pair transport cannot fully explain the variability of volatile orientations, or textural and compositional relationships. Instead, it is argued that the observed variability of the textures and chemical relationships in the pipe resulted from the co-precipitation of carbonates and sulfides from the same fluid/melt"-- Abstract, p. iii
Advisor(s)
Locmelis, Marek
Committee Member(s)
Hogan, John Patrick
Oboh-Ikuenobe, Francisca
Wronkiewicz, David J.
Department(s)
Geosciences and Geological and Petroleum Engineering
Degree Name
M.S. in Geology and Geophysics
Publisher
Missouri University of Science and Technology
Publication Date
Summer 2024
Pagination
xi, 244 pages
Note about bibliography
Includes_bibliographical_references_(pages 230-243)
Rights
©2024 Shelby Leann Clark , All Rights Reserved
Document Type
Thesis - Open Access
File Type
text
Language
English
Thesis Number
T 12441
Electronic OCLC #
1460022445
Recommended Citation
Clark, Shelby Leann, "Fe-Ni-Cu-Pge Sulfide Transport Mechanisms And Carbon-Sulfur Interactions In Lower Crustal Magmatic Settings: A Study From The Valmaggia Ultramafic Pipe, Ivrea-Verbano Zone, Italy" (2024). Masters Theses. 8219.
https://scholarsmine.mst.edu/masters_theses/8219