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Intracratonic (intraplate) orogens granites hydrothermal deposits

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Giant Metallic Deposits

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Abstract

This chapter (Chapter 10 in 1st edition of this book) emphasizes predominantly hydrothermal metallic deposits in orogenic belts partly related, directly or indirectly, to granitoids emplaced into a thick, mature continental crust as a consequence of collision and crustal extension, as well as orogenic hydrothermal deposits controlled by structures and precipitated from fluids released by dehydration in depth. The emphasis is on the rock-ore association rather than process, hence (syn)orogenic deposits in- or related to granitoids appear here, whereas comparable deposits in, for example, Precambrian greenstone belts appear in Chapter 10. The boundary of the present category against largely subduction-related Cordilleran granitoids (Chapter 7) is vague as there are many transitional ore types that would fit equally well into either category. Fig. 8.1. illustrates in a grossly oversimplified manner the contrasting setting of the pre-orogenic granitoids concentrated in former magmatic arcs, and orogenic granitoids. Anorogenic granitoids are also included here, but strongly alkaline rocks with feldspathoids are considered in Chapter 12. The supracrustal rock associations that form wallrocks or cover to the syn- and postorogenic granitoids and to hydrothermal deposits are reviewed in separate Chapters 9 and 13 for the volcanic-sedimentary (“eugeoclinal”) and nonvolcanic (“miogeoclinal”) mega-facies, respectively.

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Laznicka, P. (2010). Intracratonic (intraplate) orogens granites hydrothermal deposits. In: Giant Metallic Deposits. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-12405-1_8

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