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- W1978640033 abstract "Abstract Fluids with compositions in the system CO2-H2O-NaCl were trapped in quartz veins enclosed in low-grade metamorphic rocks (chlorite zone) on the southern flank of the Canigó Massif, eastern Pyrenees. The veins, which also contain arsenopyrite crystals, were formed contemporaneously with the main Hercynian foliation and metamorphism. Volumetric properties of the fluid and the results of arsenopyrite geothermometry suggest P-T trapping conditions of 4.6–6 kbar and 450–530° C. This implies that an episode of metamorphism with an average geothermal gradient of 25° C km−1 occurred during the main deformation event. This episode preceded the low-P/high-T metamorphism described around domes and to date considered as characteristic of the Hercynian orogeny in the Pyrenees." @default.
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- W1978640033 date "1993-01-01" @default.
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- W1978640033 title "Low-thermal-gradient Hercynian metamorphism in the eastern Pyrenees" @default.
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- W1978640033 doi "https://doi.org/10.1111/j.1525-1314.1993.tb00130.x" @default.
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