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.creator | Bassez, Marie-Paule | |
| dc.date.accessioned | 2025-08-30T04:07:15Z | |
| dc.date.issued | 2024-07-07 | |
| dc.description.abstract | The 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.other | hal-04531002 | |
| dc.identifier.uri | https://hal.science/hal-04531002 | |
| dc.identifier.uri | https://africarxiv.ubuntunet.net/handle/1/9597 | |
| dc.language.iso | en | |
| dc.subject | African Research | |
| dc.title | 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.type | Academic Publication |