Page 115 - Carbonate Sedimentology and Sequence Stratigraphy

106 WOLFGANG SCHLAGER

0.5 1.0 sec the on suggest right. adjacent

NE platform platform the on experienced the

prograding adjacent margin platforms Both from sediment

the the prograding
by above the platforms. abundant
filled rise on

gradually to easier two the receives

is tendency much is between and
that its it modified).
basin and setting; downwind

a margin this movements (1988,
enclose left in difficult tectonic faces Ginsburg

platforms the of is tracts margin right and

Cenozoic patterns systems synsedimentary the supply: Eberli

Two incoherent and no After

Bank. sequences were there sediment sediment.

Bahama seismically that by caused of stripped

Great The Recognizing indicate are therefore

southwestern aggrades. only shoals. basin the differences is and

across left the sand or across their and upwind
10 km profile on margin reefs extending history faces

Seismic platform stacked of reflections sea-level margin left

7.1.— The consists same the

SW Fig. right. it that Continuous the platform;