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

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书目名称Hydrothermal Mineral Deposits影响因子(影响力)




书目名称Hydrothermal Mineral Deposits影响因子(影响力)学科排名




书目名称Hydrothermal Mineral Deposits网络公开度




书目名称Hydrothermal Mineral Deposits网络公开度学科排名




书目名称Hydrothermal Mineral Deposits被引频次




书目名称Hydrothermal Mineral Deposits被引频次学科排名




书目名称Hydrothermal Mineral Deposits年度引用




书目名称Hydrothermal Mineral Deposits年度引用学科排名




书目名称Hydrothermal Mineral Deposits读者反馈




书目名称Hydrothermal Mineral Deposits读者反馈学科排名

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Hydrothermal Solutionsents, as well as many other elements (e.g. Mg, B, S, Sr, CO., H.S, NH., Cu, Pb, Zn, Sn, Mo, Ag, Au etc.) as minor constituents (Skinner 1979). The terms fluid and solution are here used interchangeably, although fluid in the strict sense refers to a phase at a supercritical temperature in which a li

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Hydrothermal Systemsular attention is given to what we know of the geometry and physical models of these systems, as inferred from active geothermal areas, or reconstructed from geological observations and laboratory studies. Hydrothermal systems can also be considered in terms of the geotectonic settings in which they

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Crustal Evolution, Global Tectonics and Mineral Depositsrer understanding of the genesis of mineral deposits. This understanding is essentially provided by a unifying framework within which processes of ore genesis can be integrated. In this way mineralisation types can be related to time-space positions, in specific lithospheric plate settings, and with

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Geological Processes and Hydrothermal Mineralisation in Plate Tectonic Settings — Mineral Exploratioer of our planet is the relatively strong and rigid lithosphere — about 100 km thick — broken up into a number of major and minor plates, whose present-day configuration is shown in Fig. 6.1. The boundaries between plates, divergent (rifting, spreading zones), convergent (subduction and collision zo

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Geotectonic and Metallogenic Analysis of Orogenic Belts orogenic belts of New Zealand. These examples are presented as an integrated modelling of tectonics and metallogeny as deduced from the available geological, geochemical and geophysical databases. The usefulness of modelling has already been discussed in connection with ore deposit types, and here

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Greisen Systemsnd tourmaline. Greisenisation is defined by Shcherba (1970) as the high temperature, post-magmatic alteration of rocks by volatile-rich solutions associated with the cooling of granitic intrusives. Burt (1981, p. 832) defines greisenisation as a “hydrothermally altered granitic rock consisting of a