Partial Report for Gulf-margin normal faults, Louisiana and Arkansas (Class B) No. 1022
Compiled in cooperation with the Louisiana Geological Survey
citation for this record: Wheeler, R.L., and Heinrich, P.V., compilers, 1998, Fault number 1022, Gulf-margin normal faults, Louisiana and Arkansas, in Quaternary fault and fold database of the United States: U.S. Geological Survey website, http://earthquakes.usgs.gov/hazards/qfaults, accessed 07/23/2014 11:20 AM.
|Synopsis||A belt of mostly seaward-facing normal faults borders the northern Gulf of Mexico in westernmost Florida, southwestern Alabama, southern Mississippi, all of Louisiana and southernmost Arkansas, and eastern and southern Texas (Ewing and Lopez, 1991 #2032). For the purposes of his compilation, the Gulf Coast faults are divided in four large groups because they number in the hundreds. To reflect regional differences in the characteristics of the faults, those in Florida and Alabama are evaluated together in a single group, as are those in Mississippi, those in Louisiana and Arkansas (described here), and those in Texas.
Because numerous individual faults are combined into a single group for this compilation, it is not possible to provide to provide digital information about the azimuth, length, and dip of each individual fault.
The gulf-margin normal faults in Louisiana and Arkansas are assigned as Class B structures because their low seismicity and because they may be decoupled from underlying crust, making it unclear if they can generate significant seismic ruptures that could cause damaging ground motion.|
|County(s) and State(s)||ARKANSAS |
|Physiographic province(s)||COASTAL PLAIN |
|Reliability of location||Poor|
Compiled at 1:2,500,000 scale.
|Geologic setting||A belt of mostly seaward-facing normal faults borders the northern Gulf of Mexico. These gulf-margin faults face southwest in westernmost Florida, southwestern Alabama, and southern Mississippi; south in Louisiana and southernmost Arkansas; and southeast in eastern and southern Texas (Ewing and Lopez, 1991 #2032). In early to middle Mesozoic time, the opening of the Gulf of Mexico formed a south-facing, rifted, passive margin at the southern edge of North America (DuBar and others, 1991 #2010; Salvador, 1991 #2019; Salvador, 1991 #2020). Subsequently, the rifted margin was buried beneath the thick, Middle Jurassic, Louann Salt and an overlying, carbonate and clastic, marine sequence that continues to accumulate today. This post-rift sequence thickens seaward (Salvador, 1991 #2020). It is at least 2 km thick everywhere in the belt of gulf-margin normal faults. At the coastline, the sequence is at least 10 km thick west of the Mississippi River and at least 5 km thick farther to the east. Thicknesses exceed 12 km under coastal Texas and southern Louisiana and perhaps 16 km offshore Louisiana. |
Rapid deposition and the resulting enormous thickness of the post-rift sediments caused them to collapse and spread seaward. Salt flowed southward and pierced upward, and the overlying sediments extended on listric, normal, growth faults that flatten downward into detachments in the salt and in overpressured shales (Ewing, 1991 #1994; Nelson, 1991 #1995). These listric normal faults, their splays, and their antithetic and transfer faults make up the belt of gulf-margin normal faults described here.
Regional fluctuations in the overall deposition rate divide the belt of gulf-margin faults into two parts with different main ages of faulting and different degrees of Quaternary faulting. (1) The Interior zone of Ewing (1991 #1994) includes the entire belt except southern Louisiana, coastal Texas, and their offshore extensions. Triassic-Jurassic rifting and sedimentation, including deposition of the Louann Salt, led to Mesozoic growth faulting and salt tectonism. A line of large grabens approximates the landward limit of Jurassic salt, and Cenozoic faulting is sparse in the Interior zone (Ewing, 1991 #1994; Salvador, 1991 #2019; Ewing and Lopez, 1991 #2032). (2) The Coastal zone of Ewing (1991 #1994) covers southern Louisiana, coastal Texas, and their offshore extensions, and is separated from the Interior zone by the Early Cretaceous shelf edge (Ewing, 1991 #1994; Ewing and Lopez, 1991 #2032). Late Cretaceous and especially Cenozoic clastic sediments prograded southward led to abundant Cenozoic and continuing growth faulting and salt tectonism (for example DuBar and others, 1991 #2010, p. 584-585; Salvador, 1991 #2019). The post-rift sequence as a whole is at least 9-11 km thick throughout the Coastal zone (Salvador, 1991 #2020). Calculations show that the crustal load from rapid Quaternary sedimentation may aid Quaternary normal faulting and reactivate Tertiary faults of the Coastal zone by imposing extensional bending stresses on the post-rift sequence; older extensional stresses imposed by the Mesozoic sediment load have had time to relax (Nunn, 1985 #2215).
Epicenter maps show only sparse, low-magnitude seismicity within the fault belt (Engdahl, 1988 #1959; Stover and Coffman, 1993 #1986). The only damaging earthquakes reported through 1989 in this huge tract of land are four MMI VI earthquakes in westernmost Florida (1780), southern Louisiana (1930), and eastern Texas (1891, 1932) (Stover and Coffman, 1993 #1986). This level of seismicity is even less than that of sparsely seismic North and South Dakota, which together cover approximately the same area as the belt of gulf-margin faults and which had seven earthquakes of MMI VI since 1909 (Stover and Coffman, 1993 #1986). Furthermore, some of the sparse seismicity in the normal-fault belt may be artificially induced. Earthquakes of mbLg 3.4 and 3.9 and M of 4.0 and 4.7 in southeastern Texas and M 4.9 in southwestern Alabama may have been induced by extraction of oil and gas or injection of fluids for secondary recovery (Pennington and others, 1986 #1876; Chang and others, 1998 #1806; Gomberg and others, 1998 #1828; Gomberg and Wolf, 1999 #3440). Therefore, the natural seismicity rate in the normal-fault belt might be even less than the recent historical record would indicate.
The post-rift sequence and its belt of gulf-margin normal faults may be mechanically decoupled from the underlying crust. The stress field is extensional throughout the post-rift sequence in both the Interior and Coastal zones of the normal-fault belt, as determined mostly from drill-hole data that demonstrate fault slips and well-bore breakouts (Zoback and Zoback, 1991 #2006). The orientations of Shmin are radial to the Gulf of Mexico, in contrast to the east-northeast trends of SHmax that characterize most of North America east of the Rocky Mountains; the stress field in the crust beneath the thick post-rift sequence is unknown (Zoback and Zoback, 1991 #2006). Consistent with the stress field in the post-rift sequence, the normal-faulting focal mechanism of the 1997, M 4.9 earthquake in southwestern Alabama indicated south-southwest extension (Chang and others, 1998 #1806). The presence of the normal faults throughout the post-rift sequence from westernmost Florida to southern Texas (Ewing and Lopez, 1991 #2032) demonstrates that the sequence is sliding and extending seaward on detachments in weak salt and overpressured shales.
In summary, the belt of gulf-margin normal faults in from Florida through Texas has strikingly low historical seismicity; the stress field and seismogenic potential of the underlying crust are unknown; and, therefore, the ability of the fault belt to generate significant seismic ruptures that could cause damaging ground motion is unclear. Accordingly, the fault belt is assigned to class B.
|Sense of movement||Normal|
|Dip Direction||S; N|
|Geomorphic expression||Scarps and drainage, topographic, and tonal lineaments (DuBar and others, 1991 #2010), particularly in southern Louisiana.|
|Age of faulted surficial deposits||Eocene to Holocene (Saucier and Snead, 1991 #2021; Haley and others, 1993 #1932).|
|Most recent prehistoric deformation||Quaternary (<1.6 Ma)|
|Slip-rate category||Less than 0.2 mm/yr|
|Date and Compiler(s)||1998|
Russell L. Wheeler, U.S. Geological Survey
Paul V. Heinrich, Louisiana Geological Survey
|References||#1806 Chang, T.M., Ammon, C.J., and Herrmann, R.B., 1998, Faulting parameters of the October 24, 1997 southern Alabama earthquake [abs.]: Seismological Research Letters, v. 69, p. 175-176.|
#2010 DuBar, J.R., Ewing, T.E., Lundelius, E.L., Jr., Otvos, E.G., and Winker, C.D., 1991, Quaternary geology of the Gulf of Mexico Coastal Plain, in Morrison, R.B., ed., Quaternary nonglacial geology; conterminous U.S.: Boulder, Colorado, Geological Society of America, The Geology of North America, v. K-2, p. 583-610.
#3829 Durham, C.O., Jr., and Peeples, E.M., III, 1956, Pleistocene fault zone in southeastern Louisiana, in Rogers, J.K., ed., Transactions of the Gulf Coast Association of Geological Societies: Gulf Coast Section of the Society of Economic Paleontologists and Mineralogists, Annual meeting, San Antonio, Texas, October 31-November 2, 1956, v. 6, p. 65-66.
#1959 Engdahl, E.R., compiler, 1988, Seismicity map of North America: Boulder, Colorado, Geological Society of America Continent-Scale Map 004, 4 sheets, scale 1:5,000,000.
#1994 Ewing, T.E., 1991, Structural framework, in Salvador, A., ed., The Gulf of Mexico basin: Boulder, Colorado, Geological Society of America, The Geology of North America, v. J, p. 31-52.
#2032 Ewing, T.E., and Lopez, R.F., compilers, 1991, Principal structural features, Gulf of Mexico basin, in Salvador, A., ed., The Gulf of Mexico basin: Boulder, Colorado, Geological Society of America, The Geology of North America, v. J, pl. 2.
#3440 Gomberg, J., and Wolf, L., 1999, Possible cause for an improbable earthquake—The 1997 Mw 4.9 southern Alabama earthquake and hydrocarbon recovery: Geology, v. 27, p. 367-370.
#1828 Gomberg, J., Wolf, L., Raymond, D., Raymond, R., Barnes, A., Carver, D., Bice, T., Cranswick, E., Meremonte, M., Frankel, A., Overturf, D., Hopper, M., Rhea, S., and Eckhoff, O., 1998, A noteworthy earthquake in an unlikely place [abs.]: Seismological Research Letters, v. 69, p. 175.
#1932 Haley, B.R., Glick, E.E., Bush, W.V., Clardy, B.F., Stone, C.G., Woodward, M.B., and Zachry, D.L., 1993, Geologic map of Arkansas: Arkansas Geological Commission and U.S. Geological Survey, 1 sheet, scale 1:500,000.
#2200 Hanor, J.S., 1982, Reactivation of fault movement, Tepetate fault zone, south central Louisiana: Transactions of the Gulf Coast Association of Geological Societies, v. 32, p. 237-245.
#2201 Heinrich, P.V., 1988, Tectonic origin of Montgomery terrace scarp of southwestern Louisiana [abs.]: Transactions of the Gulf Coast Association of Geological Societies, v. 38, p. 582.
#2202 Heinrich, P.V., 1997, Pleistocene fault-line scarps and neotectonics in southwest Louisiana: Geological Society of America Abstracts with Programs, v. 29, no. 3, p. 23.
#2210 McCulloh, R.P., 1991, Surface faults in East Baton Rouge Parish: Louisiana Geological Survey Open File Series No. 96-01, 25 p., 5 pls., scale 1:24,000.
#2211 McCulloh, R.P., 1996, Topographic criteria bearing on the interpreted placement of the traces of faults of the Baton Rouge system in relation to their fault-line scarps: Louisiana Geological Survey Open-File Series No. 96-01, 13 p.
#2253 McCulloh, R.P., and Autin, W.J., 1991, Revised mapping of surface faults, East Baton Rouge Parish, Louisiana: Transactions of the Gulf Coast Association of Geological Societies, v. 41, p. 473-474.
#1995 Nelson, R.H., 1991, Salt tectonics and listric-normal faulting, in Salvador, A., ed., The Gulf of Mexico basin: Boulder, Colorado, Geological Society of America, The Geology of North America, v. J, p. 73-89.
#2215 Nunn, J.A., 1985, State of stress in the northern Gulf Coast: Geology, v. 13, p. 429-432.
#1876 Pennington, W.D., Davis, S.D., Carlson, S.M., DuPree, J., and Ewing, T.E., 1986, The evolution of seismic barriers and asperities caused by the depressuring of fault planes in oil and gas fields of south Texas: Bulletin of the Seismological Society of America, v. 76, p. 939-948.
#2019 Salvador, A., compiler, 1991, Cross sections of the Gulf of Mexico basin, in Salvador, A., ed., The Gulf of Mexico basin: Boulder, Colorado, Geological Society of America, The Geology of North America, v. J.
#2020 Salvador, A., compiler, 1991, Structure at the base and subcrop below Mesozoic marine section, Gulf of Mexico basin, in Salvador, A., ed., The Gulf of Mexico basin: Boulder, Colorado, Geological Society of America, The Geology of North America, v. J.
#2021 Saucier, R.T., and Snead, J.I., 1991, Quaternary geology of the Lower Mississippi Valley, in Morrison, R.B., ed., Quaternary nonglacial geology; conterminous U.S.: Boulder, Colorado, Geological Society of America, The Geology of North America, v. K-2.
#1986 Stover, C.W., and Coffman, J.L., 1993, Seismicity of the United States, 1568-1989 (revised): U.S. Geological Survey Professional Paper 1527, 418 p.
#2006 Zoback, M.D., and Zoback, M.L., 1991, Tectonic stress field of North America and relative plate motions, in Slemmons, D.B., Engdahl, E.R., Zoback, M.D., and Blackwell, D.D., eds., Neotectonics of North America: Boulder, Colorado, Geological Society of America, Decade Map Volume 1, p. 339-366.