Balazuc: Results of Jurassic model
Conclusion
- The Uzer fault has induced a significant thrust between the east of the margin
and the basin
- Due to the different compaction rate, the fluid circulations decrease from
west to east
- At Largentiere, there are still significant fluid exchanges (a few cm/yr.) between the basement
and the Triassic layers
- Near the Uzer fault, minor fluid circulations, strongly influenced by the fault
system, are present in the Hettangian and Triassic layers
