Fades Models
237
V.E. � 15: 1
.r auger holes ----._
I
I
I
I
�
•
a
I I
FACIES
Sand
Silt
Silty Clay
Peat
o
som
'-----'-'
0
som
L
V.E ... 15:1
Fig. 8.53. Cross sections through two abandoned splays in the Cumberland Marshes, Saskatchewan. (N.D. Smith et al.
1989)
B
Fig. 8.?4. Cross sections through an interpreted ancient
anastomosed fluvial deposit, Dakota Sandstone, southern
Utah. The anastomosed interval is that characterized by
Coa,sening·ugward
gg�a 1 s��]�fnce/
Shelly mu;d,tom·
manne
Ribbon bodies ·
annstomosed channel>
Tabular sandstone &
mud�ton<:·
floodbasin deposits
Coa! zones · mires
Sandstone with
eonglomerate lavers ·
bruidcd stream·�
ribbon sandstones with floodbasin mudstones and coals
(unit M in the legend at right). Note the relatively low
paleocurrent dispersion. (Kirschbaum and McCabe 1992)
237
V.E. � 15: 1
.r auger holes ----._
I
I
I
I
�
•
a
I I
FACIES
Sand
Silt
Silty Clay
Peat
o
som
'-----'-'
0
som
L
V.E ... 15:1
Fig. 8.53. Cross sections through two abandoned splays in the Cumberland Marshes, Saskatchewan. (N.D. Smith et al.
1989)
B
Fig. 8.?4. Cross sections through an interpreted ancient
anastomosed fluvial deposit, Dakota Sandstone, southern
Utah. The anastomosed interval is that characterized by
Coa,sening·ugward
gg�a 1 s��]�fnce/
Shelly mu;d,tom·
manne
Ribbon bodies ·
annstomosed channel>
Tabular sandstone &
mud�ton<:·
floodbasin deposits
Coa! zones · mires
Sandstone with
eonglomerate lavers ·
bruidcd stream·�
ribbon sandstones with floodbasin mudstones and coals
(unit M in the legend at right). Note the relatively low
paleocurrent dispersion. (Kirschbaum and McCabe 1992)