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- W2082022333 abstract "Summary Based on nearly 1500 published amphibole analyses the maximum possible Al vi in hornblendes is shown to increase with increase of Al iv . New analyses of hornblendes from amphibole-corundum rocks, with and without anorthite, are given and after critical examination of the available data it is concluded that the maximum verified Al vi -rich calciferous amphibole that approaches the closest to hypothetical tschermakite comes from a kyanite-bearing aluminous high-pressure-crystallized schist from Lukmanier, Switzerland. Pure natural edenite or ferroedenite is unknown, but a new analysis of the nearest known natural edenite, from Mysore, India, agrees with the postulated view that extraordinarily low temperatures are needed for edenite-ferroedenite crystallization, much below that possible in magmas and only rarely achieved in metamorphic rocks containing amphiboles. The limit of the approach of igneous hornblendes to edenite-ferroedenite and tremolite-ferroactinolite is outlined. At least 1100 °C is required for complete expulsion of water from some amphiboles." @default.
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- W2082022333 date "1971-12-01" @default.
- W2082022333 modified "2023-10-16" @default.
- W2082022333 title "On aluminous and edenitic hornblendes" @default.
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- W2082022333 doi "https://doi.org/10.1180/minmag.1971.038.296.01" @default.
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