Abstract
Isotopic ratios of trace amounts of lead in pyrite and pyrrhotite have been successfully used to distinguish unmineralized Ordovician from mineralized Silurian black shales around the Woodlawn copper-lead-zinc prospect.
Original language | English |
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Pages (from-to) | 1-5 |
Number of pages | 5 |
Journal | Mineralium Deposita |
Volume | 11 |
Issue number | 1 |
DOIs | |
Publication status | Published - Apr 1976 |
Externally published | Yes |