Page 147 - Carbonate Sedimentology and Sequence Stratigraphy

138 WOLFGANG SCHLAGER

negative SB SB SB exposure surface. direction Pomar

or supply-dominated the of
zero after in sense
with a of Flooding maximum-flooding down the in unit.

progradation example backstepping. the step not do tracts middle of

of an and zones systems part right
intervals Mallorca, no is surface coral offlapping in apron

Long Blanc, there transgressive the but

varies. modified. sequence boundary Cap at surfaces; the top the represent back-reef

aggradation (2000), Pomar limestones exposure with coincides at truncated sigmoids truncated dipping landward

reef slope + open shelf of rate the but After reef slope + open shelf Miocene in erosional by morphologically are right lower the if open and margin

continuous aggradation. surfaces erosion only interrupted boundary at unit the remains raised Note

reef core virtually significant subaerial and of it Thus, lowstand.

is with reef core rapid sequence sigmoids center.
Progradation intervals and facies, very is type-1 the that the of the during

inner + outer lagoon outcrop. short by inner + outer lagoon patterns, Progradation the accumulation; indicates unit middle eroded was

of cliff separated bedding modified. morphology the for top
km are holds whose
2 of sediment
of sketch (2000), coral same tracts
Pleistocene Overview (downstepping) Pleistocene Field Pomar measurable and The

7.40.— 7.41.— After no geometry progradation. highstand or

Fig. aggradation Fig. system. leaves Bedding of (2000)