Fig. 8.43. The "Broken Beds" within the Purbeck Beds (Upper Jurassic), Dorset, southern England. This is
an evaporite solution collapse breccia of lagoonal fecal pellet lime mudstones.
Fig. 8.44. Cross-section across the Purbeck fault line, Dorset, England. Both the extent of evaporite deposition, and the resultant solution collapse breccia of the Purbeck Beds, were controlled by syndepositional
movement along a growth fault. Datum pre-Albian unconformity. (For further details see Selley and Stoneley, 1987.)
an evaporite solution collapse breccia of lagoonal fecal pellet lime mudstones.
Fig. 8.44. Cross-section across the Purbeck fault line, Dorset, England. Both the extent of evaporite deposition, and the resultant solution collapse breccia of the Purbeck Beds, were controlled by syndepositional
movement along a growth fault. Datum pre-Albian unconformity. (For further details see Selley and Stoneley, 1987.)