Abstract
Three types of stratiform scheelite deposits are recognised. They all commonly have a close spatial association with tourmalinite. Regional prograde calc-silicate rocks in Precambrian rift settings commonly contain >100 ppm WO3 with enrichment to 0.5–1% WO3 in retrograde metamorphic assemblages at fold hinges, joints, faults, shears and granite and pegmatite dyke contacts. The calc-silicate progenitor was probably a impure dolomitic carbonate sediment. Amphibolite-hosted scheelite deposits occur in metamorphosed altered mafic volcanics formed in a narrow rift graben. Scheelite occurs both as stratiform and stratabound footwall stringer ore which has undergone minor remobilization during tectonism. Tourmalinites are rarely the host for stratabound quartz-scheelite±wolframite veins remobilized from the host tourmalinite and associated metavolcanics during tectonism.
Tourmaline associated with stratiform scheelite deposits comprise zoned schorl-dravite and are no different from other tourmalines associated with submarine exhalative ores. Tourmalinites are characterized by high SiO2, Al2O3, B2O3 and Fe2O3 and, although they are commonly stratigraphically equivalent to submarine exhalative base metal deposits, they are depleted in P2O5, BaO and MnO.
It is suggested that soft base-soft acid ligand complexes transported W from the mantle or leached crust for surficial submarine hot spring deposition. Enrichment during tectonism, especially in calc-silicate hosted deposits, took place at the sites of fluid focussing where \(P_{O_2 } \), \(P_{H_2 O} \) and pH were high. This enrichment by up to 102 derives from dissolution of scheelite by chloride solutions resulting in redeposition of scheelite in retrograde metamorphic assemblages.
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Plimer, I.R. The association of tourmalinite with stratiform scheelite deposits. Mineral. Deposita 22, 282–291 (1987). https://doi.org/10.1007/BF00204521
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DOI: https://doi.org/10.1007/BF00204521