Mineralogical Characterization of a Complex Polymetallic Deposit Containing Gold, Silver, and Organic Carbon

Canadian Institute of Mining, Metallurgy and Petroleum
P. J. Lind J. Awmack L. A. Jameson
Organization:
Canadian Institute of Mining, Metallurgy and Petroleum
Pages:
12
File Size:
1005 KB
Publication Date:
Jan 1, 2017

Abstract

"Peñasquito is a polymetallic deposit containing gold, silver, lead, and zinc. The operation is currently the largest producer of gold in Mexico. Over the next few years, the process flowsheet will be expanded beyond the flotation of lead and zinc to include flotation of pyrite from zinc tails and subsequent leaching of the pyrite concentrate. This paper outlines mineralogical leach characterization that has been carried out to improve the understanding of the complex hosting of gold and silver minerals in the ore. Organic carbon that is present in the ore can have an impact on flotation and leaching. Mineralogical techniques used to characterize this deleterious component of the ore are introduced.INTRODUCTION Goldcorp’s Peñasquito operation is located in the Mexican state of Zacatecas, approximately 200 km from the city of Zacatecas as shown in Figure 1. Peñasquito has been in operation since 2009 and is currently Mexico’s largest gold mine. Mining is carried out by open-pit methods, with oxide ore proceeding to a heap leach facility and sulfide ore treated in the sulfide processing plant.The processing capacity of the sulfide plant is 130,000 tonnes of ore per day and in 2016 production amounted to 450,000 ounces of gold, 17.6 million ounces of silver, 109 million lb of contained lead, and 263 million lb of contained zinc in lead and zinc concentrates. GEOLOGY The Peñasquito deposit is hosted in and adjacent to two breccia pipes; Peñasco and Breccia Azul. The two breccia pipes are branches of a larger intrusive-related complex, which is hosted in the sedimentary Caracol formation as illustrated in Figure 2. The regional geology is dominated by Mesozoic sedimentary rocks which comprise a thick series of marine sediments deposited during the Jurassic and Cretaceous periods. A 2 km thick sequence of carbonaceous and calcareous siltstones and interbedded sandstones is underlain by a 1.5 to 2 km thick limestone sequence (Goldcorp Inc., 2015)."
Citation

APA: P. J. Lind J. Awmack L. A. Jameson  (2017)  Mineralogical Characterization of a Complex Polymetallic Deposit Containing Gold, Silver, and Organic Carbon

MLA: P. J. Lind J. Awmack L. A. Jameson Mineralogical Characterization of a Complex Polymetallic Deposit Containing Gold, Silver, and Organic Carbon. Canadian Institute of Mining, Metallurgy and Petroleum, 2017.

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