The pore pressure regime of the northern Gulf of Mexico: Geostatistical estimation and regional controls

Abstract

Subsurface pressures strongly influence the migration and trapping of hydrocarbons and impact the safety and efficiency of drilling operations. The pore pressure field of the northern Gulf of Mexico (GOM) was analyzed at 1000-ft (305-m) depth intervals from 2500 to 17,500 ft (762 to 5334 m) below the sea floor. Two variables were mapped: 12,976 initial hydrocarbon reservoir pressure gradient values and 43,276 observations on drilling fluid (mud) weight. Because of the acute importance of assessing estimate uncertainty, ordinary kriging was employed, providing explicit evaluations of confidence surrounding mapped values. Expected values and confidence intervals for the distribution of both variables were estimated by 9 mi 2 (23.3 km 2) grid cells across the GOM for each of the 15 depth intervals. Estimation variances were also used to clip each map to specific extents, within which a uniform minimum threshold of certainty was exceeded. Characteristic of young basins with high sedimentation rates, mean pore pressure exceeded hydrostatic pressure throughout the GOM. Four provinces of internally consistent pressure regimes were defined: three south of Louisiana and one off the Texas coast. They reflect geologic controls on pressure arising from regional patterns of sedimentation and the resultant timing and geometry of salt tectonism. One GOM-wide (shallow) vertical transition in the pressure field was found in the mud weight data, and a second vertical transition (deep) occurred in both variables. Hot spot analysis was also applied to identify specific contiguous areas of abnormally high or low rates of change in pressure gradient and mud weight between depth-adjacent intervals.

Maturing global CO2 storage resources on offshore continental margins to achieve 2DS emissions reductions

“…3, based on a generalized Norwegian North Sea basin case. For comparison, average initial-reservoir pressure trends for all Miocene reservoirs on the inner shelf of Texas 26 are shown to be hydrostatic to approximately 2,750 meters 27 , consistent with regional GoM data 28 . Three depth zones are identified in this generic plot: (1) a normally pressured zone between 1 and 3 km depth, (2) a weakly over-pressured zone between 3 and 4 km depth, and (3) a high over-pressured zone between 4 and 5 km depth.…”

Formation Pore Pressure Variation of the Neocomian Sedimentary Succession (the Fahliyan Formation) in the Abadan Plain Basin, SW of Iran

“…Sedimentary basins exhibit a variety of pore pressure distribution patterns. The distribution of pore pressure within a sedimentary basin may affect almost all processes and elements relevant to petroleum occurrence in sedimentary basins, including organic-matter maturation [1][2][3] and petroleum generation (e.g., [1,[4][5][6][7][8][9][10][11][12][13]). In addition, knowing the subsurface pressure of the sedimentary succession in a basin is very critical to select suitable mud weight for safe drilling, casing design, and preventing reservoir damage.…”