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Published in:
2000 | OriginalPaper | Chapter
Volcanic and post-volcanic hydrothermal activity in the Intrasudetic Basin, SW Poland; Implications for mineralization
Authors : Krzysztof Mastalerz, Maria Mastalerz
Published in: Organic Matter and Mineralisation: Thermal Alteration, Hydrocarbon Generation and Role in Metallogenesis
Publisher: Springer Netherlands
Included in: Professional Book Archive
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The present-day heat flow varies considerably over the Earth’s surface as a function of upper mantle processes, intracrustal heat generation and thermal conductivity of rocks, (e.g. Chapman et al. 1979). Intracrustal heat transfer is commonly associated with magmatic processes and migration of post-magmatic solutions. This heat transfer is very important with regard to the formation of ore deposits, fossil fuels and hydrocarbon generation and migration (Evans, 1993).