|Northeastern (46th Annual) and North-Central (45th Annual) Joint Meeting (20–22 March 2011)|
|Paper No. 44-4|
|Presentation Time: 2:20 PM-2:35 PM|
MICROSTRUCTURAL CONTROL OF GOLD MINERALIZATION IN SHEAR-ZONE-HOSTED GOLD DEPOSITS: EXAMPLES FROM THE SUPERIOR PROVINCE OF NORTHWESTERN ONTARIO
KOLB, Maura and HILL, Mary Louise, Department of Geology, Lakehead University, 955 Oliver Road, Thunder Bay, ON P7B 5E1, Canada, firstname.lastname@example.org|
Microstructural control of gold mineralization is significant to explaining the close association between gold deposits and major ductile shear zones. Musselwhite Mine and Hammond Reef are two examples of shear-zone-hosted gold deposits located in northwestern Ontario, in the Superior Province of the Canadian Shield. Both deposits lie within or adjacent to regional shear zones, and have been ductilely deformed during regional metamorphism. However the lithologies hosting the gold deposits are very different. At Musselwhite Mine the main ore-hosting lithology is metamorphosed banded iron formation whereas at Hammond Reef gold is found in metamorphosed tonalite. Despite the difference in rock types, microscopic analysis of three different gold-hosting lithologies from these deposits demonstrates close similarities in the microstructures which host gold and the relative timing of gold mineralization.
Gold-hosting microstructures for these deposits are most commonly related to heterogeneous ductile deformation, indicating structural control on mineralization at a microscopic scale. Gold commonly occurs in fractures in competent minerals such as garnet and pyrite. These gold-hosting fractures do not extend throughout the matrix but are restricted to the competent minerals. Gold is also associated with other microstructures, including strain shadows. Gold occurs as inclusions within metamorphic minerals at both Musselwhite Mine and Hammond Reef. Also gold commonly occurs on plane defects such as grain and subgrain boundaries.
In both deposits gold mineralization occurred during synchronous metamorphism and deformation. Inclusions of gold within metamorphic minerals indicate gold mineralization before or during metamorphism, while gold within fractures in metamorphic minerals as well as in strain shadows around metamorphic minerals indicates gold mineralization during or after deformation.
Close similarities between the relative timing of gold mineralization as well as the microstructures which host gold at these shear-zone-hosted gold deposits indicates a role for ductile deformation in controlling gold mineralization at a microscopic scale.
Northeastern (46th Annual) and North-Central (45th Annual) Joint Meeting (20–22 March 2011)
General Information for this Meeting
|Session No. 44|
Structural Geology and Natural Resources in the Central and Northeastern United States
Omni William Penn Hotel: Conference B
1:30 PM-5:30 PM, Monday, 21 March 2011
Geological Society of America Abstracts with Programs, Vol. 43, No. 1, p. 126
© Copyright 2011 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.