Chann el Belts
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0· GUEYDAN AXIS
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TOP OAKVII,.\..€
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TOP CllTA> I
® GEORGE WEST AXIS
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I t
tOATVM
N
I
SoM
Chor>nel fill
Mud I cllly
+ -- MvHii<;J!erlll sQnd bodies
Multistory sond bodies
SW
Fig. 9.3. Representative stiike�parallel cross sections of
major coastal�plain fluvi�l deposits, Cenozoic of the Gulf
Coast, Texas. The fluvial style of the Gueydan system,
BAR ACCRETION
sw
N
:AT A�
i
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I
•
I
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t
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.
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a -:ir or.< CATAHOUlA
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TOP QAKVtLLE
t
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l
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TOP CATAHO\JLA
® MOULTON STREAM PLAIN
Concenlrll!ions of channel
fill ond ossociQted sploy
facies
-
!
o
,_ _ "'� 0
KM
30
100
V I:: X"'2 00t
500
255
shown in diagram A, is illustrated in Figs. 9.4 and 9.5. The
locations of these cross sections are shown in Fig. 9.14.
(Galloway 1981)
NO SCALE
Sploy
FLOODPLAIN AGGRADATION
Fig. 9.4. Schemat\c reconstruction of the Gueydan fluvial style, Texas. (Galloway 1981)