Abstract: Modern Analytical Techniques for Fault
Surface Seal Analysis: A Gulf Coast Case History
Mary J. Broussard, Brian E. Lock
Today's exploration methods, with a major reliance on mapping with 3-D seismic data, generate a great deal of potential information about prospective reservoirs. Effective prospect evaluation requires consideration of the sealing characteristics of faults, and techniques have been developed to improve fault
surface analysis. "Allan"
fault
surface profiles permit assessment of sand juxtaposition across the
fault
, and can be prepared by manual mapping methods if adequate structural maps are available from 3-D seismic interpretation. Commercial software is available to perform similar analysis directly from the 3-D data.
Marathon's Vermilion Block 331 field was selected for a pilot study. The field consists of a low relief anticline, downthrown to a regional growth fault
. Numerous small faults cross the crest of the anticline and compartmentalize reservoir sands of Trimosina A (Pleistocene), Angulogerina B (Pleistocene), and Lenticulina (Miocene) age. Faulted reservoirs with multiple, stacked sands are particularly prone to loss of hydrocarbons by leakage across
fault
surfaces, so that this field was considered ideal for testing the effectiveness of
fault
surface analysis. Seal risk was evaluated by means of
fault
surface profiles along seven of the crestal faults, to determine the limits of trapping potential and paths for vertical migration. Actual hydrocarbon distribution
was compared with the predictions made from
fault
surface analysis.
The role of faults in permitting up-fault
migration along the fracture surface or in providing shale smear barriers to cross-
fault
migration from sand to sand may confound interpretations based only on
fault
surface profile geometries. For this reason, smear gouge ratios were also determined and used in assessing trapping potentials.
AAPG Search and Discovery Article #90955©1995 GCAGS 45th Annual Meeting and Gulf Section SEPM, Baton Rouge, Louisiana