The possible role of anoxic alkaline high subcritical water in the construction of the BIFs: the case of the 3.4 Ga Buck Reef Chert, Sth Africa

dc.creatorBassez, Marie-Paule
dc.date.accessioned2025-08-30T04:07:15Z
dc.date.issued2024-07-07
dc.description.abstractThe Back Reef Chert was emplaced between volcanic events. Two non-homogeneously mixed viscous fluids with high SiO2 content, might have been ejected in flow-banding for the construction of the Banded Iron Formations.
dc.identifier.otherhal-04531002
dc.identifier.urihttps://hal.science/hal-04531002
dc.identifier.urihttps://africarxiv.ubuntunet.net/handle/1/9597
dc.language.isoen
dc.subjectAfrican Research
dc.titleThe possible role of anoxic alkaline high subcritical water in the construction of the BIFs: the case of the 3.4 Ga Buck Reef Chert, Sth Africa
dc.typeAcademic Publication

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