Titlebook: Hydrothermal Mineral Deposits; Principles and Funda Franco Pirajno Textbook 1992 Springer-Verlag Berlin Heidelberg 1992 Pegmatit.classifica

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Introduction wall rocks. The study of fluid inclusions provides data on the nature of the solutions, temperature, pressure and depth of ore formation, while stable isotope systematics helps in constraining the source of the fluids and tracing their movement through, and interaction with, the crust. Thus, it can

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Crustal Evolution, Global Tectonics and Mineral Depositsmineral deposits. The books referred to are those published by Mitchell and Garson (1981), Hutchison (1983) and Sawkins (1990). Equally important in models of ore genesis is an understanding of the evolutionary trends of mineral deposits through the geological ages. This field of study is obviously

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Stratabound Carbonate-Hosted Base Metal Depositsts also occur in the carbonate sequences of Early Proterozoic age, such as those of the Transvaal basin in South Africa, mentioned briefly in the previous chapter (see Fig. 13.23). Important Pb-Zn deposits of Late-Proterozoic age are the Kabwe deposit in Zambia, and the world-famous Tsumeb and adjac