Figure 9. Structural framework and regional stress regime of the Borneo region show strike-slip faulting and transpressional tectonism from the Late Pliocene to the present day which probably caused major structural development.
Figure 9. Structural framework and regional stress regime of the Borneo region show strike-slip faulting and transpressional tectonism from the Late Pliocene to the present day which probably caused major structural development.