Popis: |
Paleomagnetic analysis of 382 specimens from 27 sites in the Sweetwater Ba F Zn district in the southern AppalachianValley and Ridge province of eastern Tennessee indicates that peak dolomitisation or recrystallisation of the host rocks occurred during Mississippian time at 334 ± 8 Ma. This age is coeval with the 334 ± 14 Ma paleomagnetic age for host rock dolomitisation in the Mascot-Jefferson City Mississippi Valley-type (MVT) district ∼ 70 km to the northeast. These ages suggest that a single fluid flow event at 334 ± 8 Ma, either topographically or thrust-fault-driven, caused a regional chemical remagnetisation of the carbonates hosting MVT mineralisation in eastern Tennessee, indicating an early onset of the Alleghenian Orogeny in the southern Appalachians. |