Compared to cratonic North America, this result indicates that the southern Methow block was displaced from the south by 1800 ± 500 km, meaning it lay south of the Sierra Nevada subduction zone but well north of other paleomagnetically constrained Cretaceous rock units from the Insular super...
The stratigraphic expansion, once analysed with the log curves, occurs in a sand-tosand/ shale-to-shale mode, meaning that the net to gross ratio of a stratigraphic interval on one side of the fault is roughly the same of that in the other side. More over, as far as log fac...