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- W2743607621 abstract "Distribution pattern of fluid inclusion homogenisation temparatures and assay of copper ores hove been uscd to ascertain the mineralising fluid ascent direction. Thetrigonametric relationships to calculate the parameters of this direction have been derived which show that the bearing of ascent of ore fluids isN 53.°E-S 53°W having plunge 38° and rake 77°. There is high probability of encountering rich ores underneath 30th level in a direction opposite to fluid ascent at selected locations." @default.
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- W2743607621 date "1995-09-01" @default.
- W2743607621 modified "2023-09-22" @default.
- W2743607621 title "Mineralising fluid ascent direction in the sulphide assemblage of Mosaboni, Singhbhum, Bihar" @default.
- W2743607621 doi "https://doi.org/10.1016/0148-9062(95)99014-o" @default.
- W2743607621 hasPublicationYear "1995" @default.
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