Anish Kumar1, Brian Briscoe2, George R. Kear2,
Terry D. Keegan3, Paul N. Lawless3,
Jonathan W. Malone2, James P. Stoyanoff3, and Elizabeth Zobell4
1 Schlumberger, 1325 S. Dairy Ashford Rd., Houston, Texas 77077
2 Schlumberger, 1515 Poydras St., New Orleans, Louisiana 70112
3 Helis Oil & Gas Company, L.L.C., 228 St. Charles Ave., Ste. 912, New Orleans, Louisiana 70130
4 Department of Geology, Brigham Young University, Provo, Utah 84602
Integration of wireline borehole image and dip data with seismic data always results in a more complete geological understanding of any working area. Borehole image and seismic data were used in a structural and stratigraphic study of the Helis East Black Bay Field Extension (offshore Louisiana) to determine the geological history of the N-Sand.
This paper describes the methodology used in the study. Values of structural dip were obtained from high quality microresistivity images and compared to those determined from seismic two-way travel time values for the N-Sand. Paleocurrent direction and energy of deposition was determined by integrating water based mud microresistivity image interpretation and stratigraphic dips (structure-deleted dips). The depositional history interpretation was accomplished using static and dynamic borehole images and stratigraphic dips. This paper discusses the deposition of the N-Sand, including transgressive and regressive cycles, and compares the results with published sequence stratigraphy of the Miocene.