Paper
Three-dimensional geometry and evolution of a salt-related growth-fault array: Eugene Island 330 field, offshore Louisiana, Gulf of Mexico

https://doi.org/10.1016/S0264-8172(98)00021-XGet rights and content

Abstract

The geometry and evolution of a growth-fault array bounding the Eugene Island 330 Field were studied using 3-D seismic interpretation and analysis of displacement patterns. The 3-D geometry of the kinematically coherent fault array is complex and characterized by both lateral and vertical branching and linkage of individual fault segments, so that fault patterns and interactions very considerably between different structural levels. Three types of faults are distinguished: growth faults with throw increasing downward; compensation faults with closed tip lines; and composite faults, which combine elements of both growth and compensation faults. Reconstruction of the fault array's evolution using displacement backstripping illustrates the growth and linkage of some isolated faults and the upward separation of others into distinct segments. The results may have important implications for understanding the history of hydrocarbon migration and entrapment in the EI-330 field and other fault-bounded minibasins in the Gulf of Mexico.

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      This method therefore suggests that faults grow in accordance with the “constant length” model throughout most of their slip history (Walsh et al., 2002; Kim and Sanderson, 2005; Jackson et al., 2017). In the modified method or the maximum throw subtraction method, the throw pattern at the time of deposition of a certain horizon is calculated by subtracting the maximum along-horizon throw (Tmax) from the entire fault surface (Rowan et al., 1998; Dutton and Trudgill, 2009); the outcome suggests decreased fault lengths as the throw is removed (Fig. 5D–F). On the basis of the maximum fault displacements and lengths indicated in earthquake rupture data and published papers, a linear relationship can be assumed to exist between the maximum cumulative displacement on a fault (Dmax) and the fault surface (L) in logarithmic coordinates (Cowie and Scholz, 1992; Kim and Sanderson, 2005; Watterson, 1986).

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