Abstract
The direct measurement of gases trapped in sulphide minerals shows that samples from gold-bearing deposits in Britain and Ireland are anomalously rich in methane. Chalcopyrite samples in deposits of Palaeozoic age sited in Neoproterozoic basement (Caledonides greenschist), Munster Basin (Variscides greenschist) and the Carboniferous cover (diagenetic) were compared using mass spectrometry of cold-crushed gases. All host sequences contain sources of organic matter. The content of non-aqueous gas is greater in both sets of greenschist-hosted deposits than in the diagenetic-hosted deposits. However, chalcopyrite accompanying gold in the Neoproterozoic is methane-rich, but in the low-gold Munster Basin it is methane-poor. These gas data from opaque minerals complement fluid inclusion data from gangue minerals, and add support to models for the involvement of organic species in orogenic gold mineralization.
| Original language | English |
|---|---|
| Pages (from-to) | 89-95 |
| Number of pages | 7 |
| Journal | Applied Earth Science |
| Volume | 128 |
| Issue number | 3 |
| Early online date | 11 Mar 2019 |
| DOIs | |
| Publication status | Published - 2019 |
Keywords
- chalcopyrite
- copper mineralisation
- gold
- Caledonides
- cold crush gases
- Britain
- Ireland
- Chalcopyrite
ASJC Scopus subject areas
- Geochemistry and Petrology
- Geotechnical Engineering and Engineering Geology
- Earth and Planetary Sciences (miscellaneous)
Fingerprint Dive into the research topics of 'Methane in sulphides from gold-bearing deposits, Britain and Ireland'. Together they form a unique fingerprint.
Cite this
Parnell, J., Spinks, S., & Blamey, N. (2019). Methane in sulphides from gold-bearing deposits, Britain and Ireland. Applied Earth Science, 128(3), 89-95. https://doi.org/10.1080/25726838.2019.1588517