Nanoscale isotopic evidence resolves origins of giant Carlin-type ore deposits

Geology
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Abstract

The western North American Great Basin's Carlin-type deposits represent the largest accumulation of gold in the Northern Hemisphere. The controversy over their origins echoes the debate between Neptunists and Plutonists at the birth of modern geology: were the causative processes meteoric or magmatic? Sulfur isotopes have long been considered key to decoding metal cycling in the Earth's crust, but previous studies of Carlin-type pyrite lacked the spatial resolution to quantify differences among the numerous generations of sulfide mineralization. We developed a new dual-method, nanoscale approach to examine the fine-grained ore pyrite. The δ34S of the ore pyrite varies systematically with Au concentration at the nanoscale, indicating that both magmatic and meteoric fluids contributed during mineralization, but the magmas brought the gold. Repeated oscillations in fluid ratios upgraded the metal content, resulting in high gold endowment. Our results demonstrate that high-spatial-resolution studies are key to elucidate the spatiotemporal evolution of complex hydrothermal systems.

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Publication type Article
Publication Subtype Journal Article
Title Nanoscale isotopic evidence resolves origins of giant Carlin-type ore deposits
Series title Geology
DOI 10.1130/G49888.1
Volume 50
Issue 6
Year Published 2022
Language English
Publisher Geological Society of America
Contributing office(s) Central Mineral and Environmental Resources Science Center, Geology, Geophysics, and Geochemistry Science Center
Description 5 p.
First page 660
Last page 664
Country United States
State Nevada
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