2002 Denver Annual Meeting (October 27-30, 2002)

Paper No. 13
Presentation Time: 1:30 PM-5:30 PM

THREE-DIMENSIONAL GEOMETRY OF THE PAINTER RESERVOIR STRUCTURES, WYOMING FOLD-THRUST BELT


DISCHINGER, Joseph, School of Geology and Geophysics, Univ of Oklahoma, 100 E. Boyd Street, Norman, OK 73019 and MITRA, Shankar, ConocoPhillips School of Geology and Geophysics, University of Oklahoma, 100 E Boyd St, SEC 810, Norman, OK 73019, dischinger@yahoo.com

The Painter and East Painter Reservoir structures are located in the hanging wall of Absaroka thrust in the Wyoming fold-thrust belt. A detailed structural study has been conducted to understand the three-dimensional geometry and evolution of the structures. The study utilizes interpreted logs and dipmeter data form over fifty wells penetrating the Triassic-Jurassic section. A series of five balanced cross sections have been constructed through the structures. The cross sections have been restored using line-length balancing for the Nugget sandstones, and area balancing of the Ankareh shales, and the Thaynes and Twin Creek limestones. These cross sections have been integrated with the well data to develop a three-dimensional model. The Painter and East Painter structures are interpreted as a pair of opposite-verging fault-related folds within the Triassic-Jurassic units. Both structures are characterized by gentle to moderate-dipping back limbs and steep to vertical front limbs. The front limbs of both structures contain forelimb thrust faults with small displacements. A tight syncline separates the two structures and contains a number of out-of-syncline thrusts. The structures probably developed due to frictional resistance to fault slip along the hanging wall ramp within the Triassic-Jurassic units in the Absaroka thrust sheet. The structures formed primarily by faulted detachment folding, involving a transition from asymmetric detachment folding to progressive fault propagation with increasing shortening. This kinematic model is supported by the rounded fold geometry of the structures, the presence of ductile Triassic units in the cores of the structures, and the relatively small displacements on the forelimb thrusts.