Thermal history of Carlin-type gold deposits in Yukon (Canada) as revealed by organic matter geothermometry, clumped isotope data, fluid inclusion microthermometry, and apatite fission-track analyses Article Swipe
Nicolas Pinet
,
Omid H. Ardakani
,
Josué J. Jautzy
,
Martine M. Savard
,
Patrick J. Sack
,
P Mercier-Langevin
·
YOU?
·
· 2023
· Open Access
·
· DOI: https://doi.org/10.1007/s00126-023-01162-2
YOU?
·
· 2023
· Open Access
·
· DOI: https://doi.org/10.1007/s00126-023-01162-2
Sediment-hosted gold deposits in central Yukon have most of the diagnostic characteristics of Carlin-type gold deposits in Nevada. This study combines organic matter geothermometry with fluid inclusion microthermometry, clumped isotope data (Δ 47 ) for late ore-stage hydrothermal calcite, and apatite fission-track analyses to constrain the thermal evolution of Carlin-type gold zones in central Yukon. The Tmax parameter derived from pyrolysis analyses indicates that organic matter is overmature and records regional temperatures of > 150 °C. Calcite and fluorite associated with the waning stage of mineralization at ca. 74 Ma have mean fluid inclusion homogenization temperatures of 123–173 °C, with an average salinity of 4.8 wt.% NaCl equiv. These temperatures overlap values of 91–162 °C determined from calcite clumped isotope measurements and are similar to data from Carlin-type deposits in Nevada. Fluid mixing is suggested by a variation of the isotopic composition of the fluid in equilibrium with calcite, with the higher temperature end-member having higher δ 18 O H2O values. In thermal models based on Tmax, fluid inclusion microthermometry, clumped isotope measurements, and apatite fission-track data, a higher temperature event at approximately 220 °C is consistent with pyrobitumen reflectance measurements. This event is either related to maximum tectonic burial prior to mineralization or to the flow of acidic hydrothermal fluids early in the main ore-stage. Each analytical technique used in this study is independent of the others and records part of the thermal and chemical evolution of the Yukon Carlin-type gold deposits and their host rocks.
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- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1007/s00126-023-01162-2
- https://link.springer.com/content/pdf/10.1007/s00126-023-01162-2.pdf
- OA Status
- hybrid
- Cited By
- 7
- References
- 54
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W4319320335
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Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W4319320335Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1007/s00126-023-01162-2Digital Object Identifier
- Title
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Thermal history of Carlin-type gold deposits in Yukon (Canada) as revealed by organic matter geothermometry, clumped isotope data, fluid inclusion microthermometry, and apatite fission-track analysesWork title
- Type
-
articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2023Year of publication
- Publication date
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2023-02-06Full publication date if available
- Authors
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Nicolas Pinet, Omid H. Ardakani, Josué J. Jautzy, Martine M. Savard, Patrick J. Sack, P Mercier-LangevinList of authors in order
- Landing page
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https://doi.org/10.1007/s00126-023-01162-2Publisher landing page
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https://link.springer.com/content/pdf/10.1007/s00126-023-01162-2.pdfDirect link to full text PDF
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YesWhether a free full text is available
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hybridOpen access status per OpenAlex
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https://link.springer.com/content/pdf/10.1007/s00126-023-01162-2.pdfDirect OA link when available
- Concepts
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Geology, Calcite, Geochemistry, Mineralogy, Fission track dating, Mineralization (soil science), Hydrothermal circulation, Fluid inclusions, Apatite, Fluorite, Meteoric water, Chemistry, Paleontology, Soil water, Soil science, Organic chemistryTop concepts (fields/topics) attached by OpenAlex
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7Total citation count in OpenAlex
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2025: 2, 2024: 3, 2023: 2Per-year citation counts (last 5 years)
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54Number of works referenced by this work
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10Other works algorithmically related by OpenAlex
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