Transgressive
System Track (TST)
In
transgressive sequence system tracks, sedimentation rate and sediment influx
exceeds sea level rise resulting in sediments being deposited closer to
shore along margins, on the platform and farther up slope reducing the
sediment availability. In transgressive system tracks, sea level rise results
in an increased sediment influx because the exposed self has become inundated
and initiating carbonate sedimentation or the "start-up phase" in which
carbonate accumulation is less than relative sea level rise and deposition
on the shelf resumes being deposited closer to shore.Followed
by the "catch-up phase" in which sediment accumulation exceeds the rate
of seal level rise resulting in a prograding shift of sediments being deposited
onto the slopes. The transgressive systems track peaks with the "keep-up
phase" in which sediment accumulation closely matches the rate of sea level
rise.(Handford and Loucks 1993)
The
above figure taken from represents a cross-section of a transgressive sequence
of a normal carbonate cycle. The
transgressive sequence is denoted by the sequence of sediments ranging
from 0 to +150.0 on the bar scale adjacent to the picture.
http://www.geol.sc.edu/kendall/SeaSlugMix.mov
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