The answer is B. The weight of the sediments causes the crust to subside while the crust in the flanks is uplifted in opposite force. It is noteworthy that this is one way how fold mountains are formed. The sediments are squeezed between the uplifting flanking crusts and folds are formed in the sediments. This phenomenon is common in the seas and oceans where sediments are deposited on the beds by inflowing inland rivers.