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Preliminary stratigraphy and depositional framework of Miocene in offshore Texas and Louisiana for CO2-EOR resource assessment
Mariana I. Olariu, Ramon H. Treviño and Timothy MeckelBureau of Economic Geology, The University of Texas at Austin
Siliciclastic Miocene strata are currently the most productive of all units in the northern Gulf of Mexico’s outer continental shelf, accounting for 40% of all hydrocarbons produced and 40% of all remaining proved reserves. Good hydrocarbon reservoirs make great prospective CO2 storage targets. Numerous depleted oil and gas fields in the offshore Miocene may serve as initial storage or enhanced recovery targets.Prospective Miocene sand trends in the southeast Texas and southwest Louisiana offshore occur in narrow belts which are approximately parallel to the present coastline. There was a southward movement of the shoreline during the Miocene.
Offshore Texas growth fault system consists of major faults that tend to strike northeast-southwest and is characterized by downdip shortening into shale ridges that accommodate updip extension. The offshore of Louisiana is characterized by large-displacement, dominantly down-to-the-basin, listric growth faults that sole on a regional detachment zone above the Oligocene section. Regional deformation is a product of salt mobilization from the level of the autochthonous Jurassic Louann Salt.
The middle Miocene basin-margin sequence records a relatively brief (ca. 5.5 m.y.) depisode. The Texas/Louisiana shore-zone system connected two deltaic depocenters (wavedominated Corsair Delta to the west and Central Mississippi delta to the east) and was separated by a narrow shelf from the offlapping, muddy shelf-fed apron. Well-developed shorezone sand bodies and significant margin offlap demonstrate large-scale strike transport of sediment from the adjacent Mississippi delta system.
The upper Miocene depisode records extensive margin offlap, primarily centered on the Mississippi dispersal axes,that began immediately following the Textularia Wareni flooding and was terminated by a regional flooding event associated with the Robulus E biostratigraphic top. In the west-central Gulf, adjacent to the Mississippi delta system, abundant strike-reworked sediment locally prograded the strand plain to the shelf edge.
ABSTRACT
Figure 1. Location map of the study area About 700 well logs (SP) have been used for subsurface correlation. Stratigraphic dip and strike-cross sections are indicated in red. Normal faults (purple) can be traced over considerable distances along strike (tens of km). The structural strike (NW-SE) is parallel to the depositional strike and to the coastline.
LOCATION AND GEOLOGIC SETTING
Figure 3. Correlation chart showing lithostratigraphic divisions (modified from Hentz and Zeng, 2003) and regional paleogeography of Miocene in the Gulf of Mexico Basin (from Galloway et al., 2000).
Figure 2. Oil (green) and gas (red) fields The Lower Miocene is the primary hydrocarbon-producing zone in offshore Texas and Louisiana and gas is the the dominant hydrocarbon.
Figure 6. Strike cross-section offshore Louisiana CO2 sequestration most sitable in the Upper to Middle Miocene from MFS 1 (Bigenerina A) to MFS 8 (Cibicides Optima)
Figure 4. Dip cross-section in Texas The stratigraphy of the Miocene section in offshore Texas and Louisiana is complicated by structural deformation associated with growth faulting (see Fig. 1).
Figure 5. Strike cross-section offshore Texas Geologic sequestration of CO2 is more suitable in sandstone reservoirs between MFS 6 (Textularia Wareni) and MFS 10 (Robulus L)
CROSS-SECTIONSUM 12 - 6.4 MaTextularia W - Bigenerina A
MFS 6 - MFS 1
MFS 1
MFS 6
MFS 5
MFS 9
MFS 10
Marginulina AMFS 11
MFS1
MFS4
MFS5
MFS6
MFS7
MFS8
MFS9
MFS10
MFS11
MFS12
TOPCAPACITY
BASE_CAPACITY
600
700
800
900
1000
1100
1200
1300
1400
1500
1600
1700
180 0
1900
2000
2100
2200
2 30 0
2400
2 500
2600
2 700
2800
2900
3000
3100
3 200
330 0
340 0
3500
3600
3700
3 800
3900
4 000
4100
4200
4300
4 400
4500
4600
4 700
4800
4900
5000
5100
5200
5300
5400
5500
5600
5700
5800
5 900
6000
6100
6200
6300
6400
6500
6600
6700
6800
6900
700 0
7100
7200
7300
7400
7 500
7600
7 700
7800
7 900
8000
8100
820 0
8300
8400
8500
8600
8700
8800
8 900
9000
9100
9200
9300
9400
9500
9600
9700
MFS1
MFS2
MFS3
MFS4
MFS5
MFS6
MFS7
MFS8
MFS9
4900
5000
5100
5200
5300
5400
5500
5600
5700
5800
5900
600 0
6100
6200
6300
6400
6500
6 600
6700
6 800
6900
7000
7100
7200
7300
7400
7500
760 0
7700
780 0
7900
8000
8100
8200
8300
8400
8500
8600
8700
8800
8900
9000
9100
9200
9300
9 400
9500
9600
9700
9800
9 900
1000
010
100
1020
010
300
1040
010
500
1060
010
7 00
1080
010
900
1100
011
100
112 0
011
300
1140
011
500
1160
011
700
1180
011
9 00
1200
012
100
1220
012
300
1240
012
500
1260
012
700
1280
012
900
1300
013
100
1320
013
3 00
1340
013
500
1360
013
700
1380
01 3
900
1400
014
100
1420
014
300
144 0
014
500
1460
014
700
1480
014
900
1500
00
BASECAPACITY
Type log offshore Texas Type log offshore Louisiana
TOP_CAPACITY2500
4500
6500
8500
10500
1250012900
Depth(ft)
MFS6
MFS7
MFS8
MFS9
BASE_CAPACITY
MFS4
MFS5
MFS10
2500
4500
6500
8500
10500
1250012900
500
MFS11
MFS12
SP SP
MFS1 -4600 -4600
-4000 -4000
-2500 -2500
-1000 -1000
500 500
2000 2000
3500 3500
5000 5000
6500 65006800 6800
MFS4
MFS5
MFS6
MFS7
MFS8
MFS9
MFS10
MFS11
MFS12
-2000 -2000
-1000 -1000
0 0
1000 1000
2000 2000
3000 3000
4000 4000
5000 5000
6000 6000
7000 70007200 7200
MFS2 O
MFS3 O
MFS4 O
MFS5 O
MFS6 O
MFS7
MFS8 O
MFS9
TOP_CAPACITY
BASE_CAPACITY
Depth(ft)
MFS1
SANDSTONE MAPS
Figure 8. Sandstone map for the startigraphic interval from Textularia Wareni to Bigenerina Humblei Overall the map displays an elongate geometry for the sandstone bodies which seem to thin laterally to the east.
Figure 9. Sandstone map for the startigraphic interval from Bigenerina Humblei to Cibicides Optima Overall the map displays an elongate geometry for the sandstone bodies which seem to thin laterally to the east. The sandstone becomes thicker in the offshore area (Texas-Louisiana offshore zone).
Figure 10. Sandstone map for the Upper and Middle Miocene from Bigenerina A to Robulus L Overall the map displays a strike-elongate (parallel to the present day costline) geometry for the sandstone bodies which seem to thin laterally to the east. The sandstone becomes thicker in the offshore area (TexasLouisiana offshore zone). Based on the sandstone thickness the capacity distribution is relatively low updip (northwestward), with an increasing storage potential in the basinward direction.
Jefferson
Chambers
Galveston
500450400350300250200150100500
MFS6_MFS7sand
km
0 40
Jefferson
Chambers
Galveston
500450400350300250200150100500
MFS7_MFS8sand
km
0 40
Jefferson
Chambers
Galveston
2900
2700
2500
2300
2100
1900
1700
1500
1300
1100
900
700
500
300
100
MFS1_MFS10sand
km
0 40
GATOR POINT
RUBBS, WEST
ALTA LOMA, EAST
S. SAND
ANAHUACANAHUAC
MARGINULINA 7100
ANAHUAC
CHGD. SHALLOW SDS.
ANAHUAC, W.
MARGINULINA
ANGELINA
13,000
ANGELINA
11,200
ANGELINA
11,800
BAUER RANCH
NODOSARIA
BIG HILL
MARGINULINA 9000
BIG HILL
HACKBERRY 9400
BIG HILL
MARGINULINA 8500
BIG HILL
FRIO A SOUTH
BIG HILL
FRIO A
BIG HILL
MARGINULINA 8800
BIG HILL
MARGINULINA 8600
BIG HILL
MARGINULINA
BIG HILL
MARGINULINA 8000
BIG HILL, WEST
MARGINULINA 8200
BAYOU S
GAS
BAYOU, S.
O
CLEAR LAKE
FRIO
CLEAR LAKE
00 MARGINULINA
CLEAR LAKE
CLEAR LAKE, W.
FRIO
DEVILLIER
VICKSBURG
DICKINSON
FRIO 8,000
DOUBLE BAYOU
FRIO 8700
DOUBLE BAYOU
FRIO 8200
ELWOOD
VICKSBURG
FANNETT
GAS (NON-ASSOC.)
FIG RIDGE
F-2
FISHERS REEF
FRIO 11
FISHERS REEF
FRIO 8200
FISHERS REEF
FRIO 10-B
FISHERS REEF
FRIO 8400
FISHERS REEF
FRIO 8800
FRANKS
WEITING, UPPER
FRANKS
SCHENCK SAND
FRANKS
WEITING, LOWER
GALVESTON BAY, W.
MIO. 7,150
GALVESTON ISLAND
SIPHONINA
GALVESTON ISLAND
DISCORBIS 7760
GALVESTON ISLAND
DISCORBIS 5
GUM ISLAND, N.
HACKBERRY 4
HAMSHIRE, WEST
NODOSARIA
HILDERBRANDT BAYOU
HACKBERRY
HITCHCOCK, NE.
FRIO 9100
JACKSON PASTURE
FRIO 8000
LA BELLE
MARGINULINA 8500
LA BELLE
MARGINULINA 8200
LA BELLE
MARGINULINA UP.
LAFITTES GOLD
MIOCENE D-3
LAFITTES GOLD
MIOCENE R-2
LAKE STEPHENSON
FRIO-MASS. 9400
LOVELLS LAKE
MARG. 7600
LOVELLS LAKE
FRIO 1
LOVELLS LAKE
MARG. 7300MARRS MCLEAN
FB-7, NODOSARIA
MARRS MCLEAN
FB-3, HACKBERRY
MARRS MCLEAN
HACKB. 11,100
MARRS MCLEAN
FB-6, NODOSARIA
MARRS MCLEAN
FB-8, NODOSARIA
MARRS MCLEAN
FRIO B
MARRS MCLEAN
FRIO B 10,600
MARRS MCLEAN
MCLEAN 10,400
MARRS MCLEAN
MCLEAN
MARRS MCLEAN
FRIO B 10,900
MAYES, EAST
FRIO 8800
MAYES, SOUTH
FRIO 9000
MAYES, SOUTH
FRIO 9100
MAYES, SOUTH
FRIO 19, EAST
MAYES, SOUTH
FRIO 15
V-2
POINT BOLIVAR, N
12300
PORT ACRES
HACK. LO.
PORT ARTHUR
-C-
PORT ARTHUR
-B-2-
HACKBERRY 8000
FRIO HACKBERRY
COOK MTN.COOK MTN. UPPERCOOK MOUNTAIN
RED FISH REEF
FB B-1, FRIO 10
RED FISH REEF
FB B-3, FRIO 9
RED FISH REEF
FB A FRIO 11
RED FISH REEF
FB B-1, FRIO 11B
RED FISH REEF
FB A-1, FRIO 1
RED FISH REEF S.
FRIO 15
RED FISH REEF, SW.
F-15-A
RED FISH REEF, SW.
F-11B
SABINE PASS
MIOCENE S-2
SARAH WHITE, EAST
9200
SEABREEZE
F-2
SEABREEZE
SEABREEZE FB B
SEABREEZE
FIG RIDGE
SEABROOK
TEX 2SHIPCHANNEL
F-24
SMITH POINT
FRIO 9000
SMITH POINT
FRIO 9400SMITH POINT, EAST
12,650
STEPHENSON POINT
FRIO 10
TEXAS CITY DIKE
FRIO 10200
TEXAS CITY DIKE, NORTH
FRIO A
TRINITY BAY
F-4
TRINITY BAY
FRIO 3
UMBRELLA POINT
F-4 GAS
O
0
WILLOW SLOUGH
FB-B, SBZ
WILLOW SLOUGH
FB-A, SBZ
WILLOW SLOUGH
FB-B, UN 2
Oligocene
ANAHUAC MAIN FRIO
Oligocene
CEDAR POINT FRIO 5900
Oligocene
RIO
CLEAR LAKE FRIO
Oligocene
ESPERSON DOME S. CROCKETT
Eocene, Middle
FIG RIDGE SEABREEZE
Oligocene
GILLOCK BIG GAS
Oligocene
GILLOCK EAST SEGMENT
OligoceneGILLOCK, S. BIG GAS
Oligocene
LOVELL'S LAKE FRIO 1
Oligocene
LOVELL'S LAKE FRIO 2
Oligocene
OYSTER BAYOU SEABREEZE
Oligocene
SPINDLETOP CAPROCK
Tertiary
TRINITY BAY FRIO 12
Oligocene
TURTLE BAY MIDDLETON
Oligocene
ER FRIO
pper
Jefferson
Chambers
Galveston
CREOLE-OFFSHORECREOLE-OFFSHORE
WEST CAMERON BLOCK 5CREOLE-OFFSHORE
WEST CAMERON BLOCK 28
SABINE PASSHIGH ISLAND BLK. 20-SHIGH ISLAND BLK. 19-S
ST. TR. 60-S, CENTRAL
MCFADDIN BEACH, E.
BLK. 87-SG O M-MCFADDIN BEACH DOME
HIGH IS. BLK. 24LPIRATE'S COVE
HIGH IS. BLOCK 31-L
BLOCK 176-S
GOM-ST-214-L
SA013
E
SM239SM239HITCHCOCK
HITCHCOCK
WEST CAMERON BLOCK 10WEST CAMERON BLOCK 1WEST CAMERON BLOCK 6WEST CAMERON BLOCK 4
WEST CAMERON BLOCK 19WEST CAMERON BLOCK 17 WEST CAMERON BLOCK 45
WEST CAMERON BLOCK 33
EAST CAMERON BLOCK 4WEST CAMERON BLOCK 49
HIGH IS. 4-L NW-4
EAST CAMERON BLOCK 17EAST CAMERON BLOCK 17
EAST CAMERON BLOCK 17HIGH ISLAND BLK 13-LG. O. M.-ST-83-S
HIGH ISLAND 90S
VERMILION BLOCK 16BLOCK 23L
LIGHTHOUSE POINTVERMILION BLOCK 14GOM 27-L
VERMILION BLOCK 28 EUGENE ISL
EUCRYSTAL BEACH
EUGENE ISLAND BLOCK 1POCO
EUGENE ISLAND BLOCK 8SHIPWRECK
GALVESTON 175-S
EUGENE ISLAND BLOCK 9
BLOCK 98-L
GALVESTON 102-L
LAFITTES GOLD
WC028
WC017
WC045
WC045
WC040
WC066
WC033EC002
WC045 WC041WC066
WC068WC049 WC055
WC076
WC071
EC014SA007
WC081
EC033SA017
WC095
WC118
WC109 EC014
SA011WC116HI022 EC014
LP000SA010 VR024
VR014
VR039
EC038 VR050
TS000EC046
VR014
HI052EC049
VR050
TS000EC064 EC049
EC064
EC051EC049TS000
TS000
EC057 EC057EC060
WC165
HI088 WC167HI093
WC294
EI024VR041EC064
WC178SM236EC062
SM231VR054
HI105EC062
WC187 SM235HI086
WC198HI116
EI047
HI111WC196 VR064 E
SM243HI119 EC081SM241
HI140EI047
EI047GA144
HI128
HI160 HI129EC090
EI047SM249
SM252EI048HI154
SM249HI167
EC096VR088HI166
HI164HI178
WC222
SM261
SM255WC311
HI179
HI177 HI196VR095
GA189
EC106 EI070HI196
HI006AHI195 HI199
HI194 HI199GA209
HI009AGA210
ANAHUAC
GALVESTON BAY, W.
GALVESTON ISLANDGALVESTON ISLANDGALVESTON ISLAND
LAFITTES GOLDLAFITTES GOLD
SABINE PASS
HITCHCOCK
km
0 40
0008-
- 8000- 8000
0009 -
- 9000
- 9000
- 9000
- 10000
00001-
- 8000
000 8 -
00001-
-9 0 00
0009-
- 10000
- 1 0 000 000
9-
-1
0 0000
-50- 6 000
-90
0 0
00031-
-1
4 000
0001 1-
00011-
- 1 1000
-12000
01-
- 14000
- 160
- 1500
- 14000
- 120 0 0
0
-120 00
00031- - 1300 0
Jefferson
Chambers
Galveston
km
0 40
Figure 7. The U.S. Geological Survey geopressure-gradient model of the regional pressure system spanning the onshore and offshore portions of Texas and Louisiana Characterization of the regional pressure system is critical for assessing the occurrence of undiscovered petroleum resources, evaluating hydrocarbon reservoir-seal integrity, and determining the feasibility of geological sequestration and long-term containment of fluids.
Jefferson
Chambers
eston 69 70 71
107312 106105311170 104310 103102309 101169
A 28
34 2589 7 1610
1112
31
13
32
14
30292827262524232216 21201918171
1
333343536374
38394041424344454647
1
48 2492
5
6867666564636261605958575655 7854 91053 1134
6 56
4 3 2
69707118
72737475767778798081 171682 1583 14137 1265
197 8 9 10 11 12 13
201014
110410310210110099989796 29594 2193 2292 232491 2590 2627
98 289
3 4
26 25
5
24 23 622 21 20 20720819 209
7
18 1711
8
12105 1617106 18107 1920108109110111112113114115 3736116 35117 3433118 3212 313011 291027
13141528 29 30 31 32 33
A 35 133
34 35 2132122112103036 37 38 39 2940 282726140 2524139 23138 2221137 1136135134133132131130 3839129 40128 414213 4314 444515
2
461659 58 57 56 55 54 53 3152 51 21421521621721821950 49 48 47 323346 3435141 3637142 3845 143 3940144
44
1451461471481491507
151 5554152 538
153 5251154 50155 4948156 4715760 61 62 63 5064 65 66 67 22522422368 222221220
72 49484746176 4573 44175 43174 424117374 17217117075 16976 16810
1671669
5657165 58164 5960163 61162 6263161 6416010151100 99 98 97 96 95 94 22693 22722822923023123292 91 90 89 53545588 56177 5758178 5917987 606118018118286 18318485
24185
2518618784 7372291 71290 7083 69289 68288 6766287 65
52102 103 104 105 106 107 108 239238237236235234109 233110 111 112 113 70696867192 6665114 191 64200 6362199115 198
96306 97307 98164 99308
A 14
148 149 150 151 152253252153 251250249248247154 155 156 157 919089158 8887218
231230197
229228198316317318199
110319 111112320 113200114321
350351352259
146353 147148354260
149150355 151356
19726
19611627
195190189117 188 7475292 76118 29371
7778294 79295119 8081296 82120147 146 145 144 143 142 240241242243141 244245246140 139 138 137 73747576136193 7778194 79201 80135 81202
47203204134
72 46205206207133 208302132 9190301 89300 8887299131 86298 8584297130 83129 128
488685217 84159
216 838221521416049
213212211161 210209162 303 92304 9394305163 95100165 166 167 168 A 167
185 184 183 182 181254255256257258259260
180 179 178 177 6992176 93949596219 97175
98220 99221 100101222174 68
223224225173
226227172 315314 109313 108171A 1 A 2 A 171 A 170 A 169 A 168
186 187 188 189267266265264263262
190261
191 192 70193 194111110109108107
195235 106105234 104233 103
196 71102232
115322 116201 117323 118A 6 A 5 A 4 A 3 A 172 A 173 A 174 A 175
217 216 215 214268269270271272
213273274
212 91211 210 209112113114115
208116236 117118237 119
90238
207120121239240
206241242243
205330329
204328 127327 126125
203326 124123325 122
202 324 121120119A 7 A 8 A 9 A 10 A 11 A 12 A 179 A 178 A 177
218
A 176
219 220
281280279 92278277
221
276275222 223 224 225
131130129226
128127250 12693
125249227
124248 123122247246228
245244229
331332230
333334 128335 129231
130336 131132337232133338 134135
A 20136A 19 A 18 A 17 A 16 A 15
A 13 A 180 A 181113
A 182
246
282283284A 183
285
245
28612A 184
244 243 242 241
132133240
134135112
136251 137239
138252 139253 140141254
238
255256237
347346345236
344343235
145342 144143341 142234
141340 140339 139233
138137A 21 A 22 A 23 A 24 A 25 A 26 A 27 113A
A 29 A 189 A 18828828776543
A 187
250
A 186
251 252
A 185
253
151
254
150113B
149148147262 146
255
145261 144260 143142259
256
258257
257
348349258
152261
153154262 A 39 A 38 A 37 A 36
SP
cores
faults
federal state boundary (GoM)
TX LA
Chambers
Je�erson
Vermilion
Cameron
KM
0 36
TxLa merge 3D seismic dataset
MFS2
Depth(ft)
MM 15.6 -12 MaAmphistegina B - Textularia W
MFS 9 - MFS 6