Change of stress magnitudes during the polyphase tectonic history of the Cretaceous Gyeongsang basin, southeast Korea

摘要

In order to evaluate the change of stress magnitudes in the Gyeongsang basin during its tectonic history,we analyzed multiple faulting episodes in the Barremian-Aptian Hasandong Formation at the Yusu site. As elsewhere in southeast Korea,the recorded sequence consists of a succession of more than fourteen faulting episodes,and the relative chronology shows that a strike-slip faulting episode usually coexisted with a coaxial extensional episode. Likewise,seven couples of synchronous coaxial episodes recognised in the Gyeongsang basin are assigned to seven tectonic events (T-1 to T-7 events). The friction line (in the sense of Byerlee) allows us to determine the ratios between principal stress magnitudes as well as the origin of the dimensionless Mohr diagram. This line can be deduced from tension fractures on fault planes affected by friction and from the lower limit of scattered distribution of the normal stresses vs. shear stresses of faults. Dimensionless failure envelopes drawn for coaxial strike-slip and extensional episodes are adjusted to the experimental Mohr failure envelope derived from rock mechanic tests to determine the complete stress tensors. The maximum principal stress magnitudes of strike-slip episodes show a transition from 169 MPa in the Barremian-Coniacian T-1 Event through 263 MPa and 246 MPa in the T-2 and T-4 events,respectively to 235 MPa in the Quaternary T-7 Event; additional horizontal extension (Δσ _T) have changed from -6 MPa in the T-1 Event through -8 MPa in the T-2 Event to -17 MPa in the T-7 Event. Because the studied site is currently exposed,the determined overburden (1.9 km) for the T-7 Event seems to be important,indicating the presumable occurrence of this event during the early Quaternary rather than at the present day.