Big easy prospect: a well-preserved low-sulfidation epithermal Au-Ag system in the late neoproterozoic, Newfoundland, Canada ...
The Big Easy prospect is a low-sulfidation epithermal gold occurrence of Neoproterozoic age in the Burin-Bonavista region of Newfoundland, Canada. Mineralization is predominantly hosted in epiclastic rocks of the Musgravetown Group. This well-preserved system lies within the tectonostratigraphic Ava...
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| Format: | Text |
| Language: | English |
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Memorial University of Newfoundland
2024
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| Online Access: | https://dx.doi.org/10.48336/y4b8-s984 https://research.library.mun.ca/15899/ |
| Summary: | The Big Easy prospect is a low-sulfidation epithermal gold occurrence of Neoproterozoic age in the Burin-Bonavista region of Newfoundland, Canada. Mineralization is predominantly hosted in epiclastic rocks of the Musgravetown Group. This well-preserved system lies within the tectonostratigraphic Avalon Zone and is dated as Late Neoproterozoic (ca. 573 Ma). Previous work suggests that the most prospective period for epithermal deposits within the Neoproterozoic Avalon Zone is from ca. 620 Ma until the nominal end of the Neoproterozoic at 541 Ma. This period encompassed three episodes of arc magmatism, as recognized in the Burin Peninsula region: ca. 620 Ma (e.g., Broad Island Group), ca. 585 – 570 Ma (Marystown and Musgravetown Groups), and ca. 565 Ma (Long Harbour Group). Big Easy appears to have been associated with the 585 – 570 Ma episode, as were a number of volcanic/volcaniclastic-hosted occurrences in this region. The mineralization at Big Easy is subdivided here into four different styles of discrete ... |
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