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Magmatic and hydrothermal behavior of uranium in syntectonic leucogranites: The uranium mineralization associated with the Hercynian Guérande granite (Armorican Massif, France)
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文摘

The apex of the Guérande leucogranite is structurally located below a U deposit.

Leaching of U likely occurred at the apical zone of the intrusion.

Sub-solidus alteration with meteoric fluids affected the deformed facies at the apex.

Hydrothermal circulation in the granite is sub-synchronous with U mineralization.

The Guérande leucogranite is proposed as the main source for the U of the deposit.

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