Crystal chemistry of iron in low-temperature chlorites, implications for geo-thermometry and the determination of redox paleo-conditions in uranium deposits

In contexts of uranium deposits, redox conditions constitute the main factor controlling the uranium deposition. Often observed in these deposits, chlorites are the unique clay mineral which can be able to record in their structure the redox conditions through their Fe³⁺/SFe ratio. However, the common presence of several populations of chlorites makes difficult to understand the message carried out by these minerals. Thanks to μ-XANES spectroscopy, we are now able to measure on thin sections the Fe³⁺/SFe ratio in chlorites with an accuracy of 5 %. Measurements show that it can reach 60 % in di-tri-octahedral chlorites and 5 % to more than 40 % for tri-octahedral chlorites. In hydrothermal contexts where chlorites crystallize through a dissolution-recrystallization process, their Fe³⁺/SFe ratio decreases with the increase of the global Fe content. Diagenetic chlorites observed resulting from the polymorphic transformation of berthierine have a different behavior because there is no link between their total iron content and their Fe³⁺/SFe ratio: their chemistry is directly inherited from the one of the precursor mineral because this transformation does not allow a reorganization of cations in the structure. This transformation explains that thermodynamic models cannot work for these phases. For the use of chlorites as makers of redox paleo-conditions in contexts of uranium deposits where diagenetic and hydrothermal chlorites can be present, it is decisive to determine their origin, for example analyzing their polytype: Ib (b=90 degrees) for chlorites crystallized from solid-state transformation and IIb for chlorites crystallized through dissolution-recrystallization process. (author)