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A sustained felsic magmatic system: the Hercynian granitic batholith of the Spanish Central System

Published online by Cambridge University Press:  03 November 2011

Carlos Villaseca  and
Víctor Herreros
Carlos Villaseca
Affiliation:
Carlos Villaseca and Víctor Herreros, Dpt. Petrología y Geoquímica, Fac. CC. Geológicas, Universidad Complutense, 28040 Madrid, Spain; e-mail: granito@eucmax.sim.ucm.es
Víctor Herreros
Affiliation:
Carlos Villaseca and Víctor Herreros, Dpt. Petrología y Geoquímica, Fac. CC. Geológicas, Universidad Complutense, 28040 Madrid, Spain; e-mail: granito@eucmax.sim.ucm.es
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Abstract

A batholith of around 10,000 km2 was formed during the Hercynian orogeny in the Spanish Central System (SCS). Geochronological data indicate concentrated magmatic activity during the period 325-284 Ma. This late-orogenic magmatism is essentially granitic with only minor associated basic rocks (< 2% in outcrop). The SCS is a remarkably homogeneous batholith showing a restricted range of geochemical granite types without any evolutionary pattern related to time. These peraluminous granites show a limited variation in Na2O/K2O) (0·60-0·95), K/Rb (140-240), (La/Yb)n (6-13), and Eu/Eu* (0·34-0·62) ratios. This constancy in chemical characteristics is also reflected in their isotopic signatures: most monzogranites have initial 87Sr/86Sr ratios in the range of 0·7073-0·71229, initial εNd values vary between —5·4 and —6·6 and δ 18O values group in the restricted range of 8·9-9·6‰. The lack of significant differences among SCS granitoids, maintained during a long geological period, suggests constancy in the nature of their source regions and conditions of magma generation. (1) Limited range of crustal sources: an essentially magmatic recycling during Hercynian orogen is suggested. Mantle-derived components are very limited and restricted to a minor role in the origin of the batholith. Geochemical and isotopic features of SCS granitoids are compatible with felsic lower crustal sources. (2) Constraints in melt conditions: uniformity in residual mineral assemblages (feldspars and garnet are always present in the granulitic residua) combined with a lack of attainment of equilibrium conditions during accessory phase dissolution in the crustal melting process is suggested. Granitic melts never reach saturation in some trace elements (REE, Th, Y, Zr), restricting their chemical variability. (3) Homogenisation in magma chambers: long-lived magmatic systems whose successive pulses accumulate into large magma chambers have the opportunity to mingle, thus reducing source differences.

Keywords

collision granitescrustal anatexisgeochemistryHercyman Iberian Beltisotopesperaluminous batholith
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 91 , Issue 1-2: Fourth Hutton Symposium: The Origin of Granites and Related Rocks , 2000 , pp. 207 - 219
Copyright
Copyright © Royal Society of Edinburgh 2000

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