bentukan log
TRANSCRIPT
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PROGRADATIONAL
(Regressive, Seaward -
Stepping)
RETROGRADATIONAL
(Backstepping, Transgressive,
Landward-Stepping)
AGGRADATIONAL
Thicker, less shaly upward
Sediment source moving closer (regression)
Typical of HIGHSTAND systems tract
Similar thickness, shaliness
Sediment source maintained nearby
Typical of LOWSTAND systems tract
Upward thinning, shalier
Sediment source moving away (transgression)
Typical of TRANSGRESSIVE systems tract
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Changes in these patterns can be used for sequence stratigraphic interpretation and
correlation
Flooding Surface/
Sequence Boundar
!a"i#u# Flooding
Surface
$ncise
d
%alleSequenc
e
Boundar
&ig'stand is
#issing,
proal erodedawa
Lowstand is #issing,
proal an interfluve
TST
LST
TST
TST
TST
LST/TST
LST
&ST
Idealized parasequence stacking patterns of a complete marginal marine depositional
sequence
!a"i#u# Flooding
Surface
Transgressive Surface
&ig'stand*
+rogradational
Transgressive*
Retrogradational
Lowstand*
ggradational
&ig'stand*
+rogradational
Sequence Boundar
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2
0
12
0
-
2150
m
-
2175
m
-2200
m
-
2225
m
-
2250
m
G
R
Aggradational succession
possible composite incised valley fill
Progradational to Retrogradational -
shorefacedeltaic deposits
Aggradational to retrogradational succession
valley fill! Channel fill overlain by delta lobes!
"equence#oundary!
$a%imum
&looding "urface
Cored
interval
*
An example from Southeast Asia
$a%imum
&looding "urface!
$a%imum
&looding "urface
"equence#oundary!
Lowstand-TransgressiveSystems Tract?
Lowstand-
TransgressiveSystems Tract?
Highstand
Systems Tract?
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-
2200
m
-
2225
m
-2350
m
-
2375
m
-
2250
m
-
2275
m
-
2300
m
-
2325
m
-
2400
m
2
0
12
0
2
0
12
0
G
R
G
R
!a"i#u# Flooding
Surface
!a"i#u# Flooding
Surface
!a"i#u# Flooding
Surface
Cored
interval!a"i#u# Flooding
Surface
!a"i#u# Flooding
Surface
$a%imum
&looding
"urface!
Transgressive
Systems Tract
Transgressive
Systems Tract
Highstand
Systems TractHighstand
Systems Tract
HighstandSystems Tract