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URL : https://hal.archives-ouvertes.fr/hal-02334126

B. Zoheir, B. Lehmann, A. Emam, A. Radwan, Z. Rongqing et al., Lithos 352-353, 105329. FIGURE CAPTIONS Fig. 1: Geological map of the Argemela intrusion and details of the different units. (a) Inset shows location in Central Portugal and relation with the Portuguese main geological domains (GTMZ: Galicia-Tras-Os-Montes Zone; CIZ: Central Iberian Zone; OMZ: Ossa-Morena Zone; SPZ: South Portuguese Zone). The granitic facies, Two models assume constant fluid proportions of either 5%, 2020.

S. Appendix, 2016) with an initial melt water concentration of 6 wt%. The three fluid-present models simulate the progressive W depletion observed during muscovite growth. The three final (F = 0.05) concentrations bracket the range analysed in Ms III, 10% (fluid mass fraction = 0.1, red solid curve) fluid (Appendix and text, 1978.

P. , 14: ?D -? 18 O plot for fluids in equilibrium with quartz and micas from the Argemela intrusion (calculated at 550°C) and evolution of isotopic compositions during the magmatic-hydrothermal transition. See text for details of the calculations and discussion. The magmatic and paleometeoric water boxes are from Sheppard (1986), The Cornubian magmatic water and the pegmatites and skarn boxes are from, 2000.

;. Sheppard, A. , and H. ;. , The quartz (Qtz) and muscovite (Ms) boxes refer to the range of isotopic compositions for these two minerals at Panasqueira (Kelly and Rye, 1977.