Abstract
Detailed studies of the mineral associations, compositions and parageneses of the sulphide ores of the north Pennines were undertaken by use of reflected-light microscopy and electron-probe microanalysis. These data are considered in terms of the conditions of formation of the assemblages and suggest higher temperatures of formation and more diverse fluid compositions in the orefield to the north of the Stainmore syncline than in comparable areas to the south.
Original language | English |
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Pages (from-to) | b99-b109 |
Number of pages | 11 |
Journal | Transactions of the Institution of Mining and Metallurgy, Section B: Applied Earth Science |
Volume | 89 |
Publication status | Published - 1980 |