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The AAPG/Datapages Combined Publications Database
Houston Geological Society Bulletin
Abstract
Abstract: Interior Salt Domes of Texas, Louisiana, and
Mississippi *
by
Consulting Geologist, Tyler, Texas
*Paper presented before the Society, June 1959
Texas, Louisiana, and Mississippi have a total of 90 interior domes
which have been classified as piercement domes in which salt or identifiable cap
rock
has been encountered by the bit at depths above 5,000
feet and in which the salt has penetrated younger beds. These piercement
domes are distributed as follows: 17 in the Tyler basin of
East
Texas; 28 in the salt basin of Louisiana and 43 in the salt basin of
Mississippi. One is located across the line in Alabama. These domes
occur in a rather narrow basin 30 miles in width and 120 miles in
length in
East
Texas and 30 to 60 miles in width and extending across
the entire width of southern Mississippi and northern Louisiana.
In
East
Texas there are 10 deep-seated domes interspersed
throughout the basin among the piercement domes. This holds true for
the distribution of some 9 deep-seated domes in Louisiana and 17 deep-seated
domes in Mississippi. These deep-seated features differ from the piercement domes inasmuch as the salt has not penetrated the beds
younger than lower Cretaceous and has uplifted the
overburden
in a
domal structure giving all the unpenetrated reservoir beds adequate
structural relief to make ideal traps for the accumulation of oil and
gas. With a possible exception of one or two domes, these deep-seated
domes are all now producing.
The locations of the piercement domes have been known for 30
years and it is only within the past few months that the producing possibilities
have been realized. Two of the piercement domes in
East
Texas have been producing for 30 years and since July, 1956, 4 additional
domes in
East
Texas and 1 in Louisiana have been found to be
productive.
The subsequent drilling has changed our conception as to the age and origin of the domes. It now appears that, instead of growing from the center and deepest part of local synclines, these piercement domes are so tremendous in size and have grown for such a long period of time that their growth has created the local basin as a large rim syncline.
Every known type of geological trap should be present at some depth in close proximity to each and every dome.