Abstract The Jennings salt dome is one of the first domes recognized in the Gulf Coast, having been discovered in 1901. However, the salt was not encountered and cap rock wholly penetrated until after 1926, when the structure was definitely proved to be a true salt dome. Drilling exploration for the past nine years has been limited to the flanks of the dome, mainly its southeast flank. The Yount-Lee Oil Company has drilled the west, north, and southeast flanks of the dome. The southeast flank is the only one proved productive, with four wells now producing out of fourteen drilled. Geophysical as well as geological observations have indicated an overhang on the southeast flank. The productive sands on this flank are Middle Oligocene in age and are classified as high-pressure sands.

Abstract The Jennings oil field was one of the earliest oil fields of the first class on the Gulf Coast. It is on a dome in Tertiary sediments. Although the salt has not been drilled into, limestone which has never been drilled through and which resembles cap rock underlies the main part of the field, and is taken to indicate the presence of a salt dome. There is a surface mound that is probably the remnant of a salt dome mound and a depression that in part is probably a “central depression.” The Jennings field has been one of the most prolific of the Gulf Coast oil fields, and had many long-lived wells with enormous total production.

Abstract The presence of a geosyncline along the Gulf Coast of Texas and Louisiana is indicated both by geologic and geophysical data. The formations which are exposed at the surface or in drilling are known in general to dip gulfward. The known stratigraphic thickness of formations plus shrewd extrapolation below reach of the drill indicate that the depth to the basement at Houston is greater than 20,000 feet, at Jennings, Louisiana, greater than 25,000 feet, and south of New Orleans greater than 30,000 feet. Seismic prospecting indicates that the basement certainly is deeper than 15,000 feet and, less definitely, that it is deeper than 20,000 feet. The torsion-balance data indicate that the base of the salt core of the salt domes lies at a depth of 17,000–20,000+ feet in the Houston district. The depth of the Gulf of Mexico in the Sigsbee Deep is 12,500, and throughout most of its area, is less than 10,000 feet, Tne thickness of the post-Lower Cretaceous sediments in the central part of the Gulf of Mexico presumably is not more than a very few thousand feet. The basement of the post-Lower Cretaceous beds in the Gulf Coast must be warped down at least 5,000 feet at Houston and at least 15,000 feet in the area south of New Orleans. A regional trough of gravity minimum lies axially along the Gulf Coast. Calculations suggest that it is best explained by a geosyncline on the basement plus a progressive character of the basement from granitic under the land to basaltic under the Gulf of Mexico. A study of the depression of the basement to compensate sedimentation suggests that the trough line of the geosyncline should lie nearly at the present coast line; and that is approximately the position which the gravitational calculations indicated for the actual position of the trough line. Although isostatically negative, the area has been one of continued subsidence; and the rate of subsidence seems to have kept even pace with the rate of sedimentation.

Abstract Combination traps. Salt domes: occurrence – Gulf Coast salt plugs – cap rock – associated traps – origin. SOME TRAPS combine structural, stratigraphic, and fluid barriers in varying proportions. The reader might, in fact, classify as combination traps some of the traps that have been described earlier as either structural or stratigraphic traps, for the contribution of each element to the trap is sometimes a matter of personal judgment.