--> Abstract: Burial History and Its Impact from the Petroleum Systems of Rio Muni Basin, Equatorial Guinea: Delivery, Capture and Degradation, by Niall J. McCormack, Michelle Thomas Stanley, and Andrew Pepper; #90082 (2008)

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Burial History and Its Impact from the Petroleum Systems of Rio Muni Basin, Equatorial Guinea: Delivery, Capture and Degradation

Niall J. McCormack, Michelle Thomas Stanley, and Andrew Pepper
SAWA Exploration, Hess Corp, Houston, TX

The Rio Muni Basin, offshore Equatorial Guinea, is a volumetrically significant petroleum system sourced primarily from Lower Cretaceous source rocks and reservoired primarily in Senonian deep marine clastics. We will address the thermal evolution of the source intervals, including the impact of Miocene uplift, erosion and re-burial, and how this evolution effects quantities and timing of expulsion of oil and gas into the system. Differences in source, reservoir and trap histories relating to uplift in-board, and little to no uplift out-board, lead to differing fluid properties, exemplified in the Elon and Ceiba pool respectively.

The primary controls on the timing and volume of hydrocarbons expelled are present day crust type and thickness, and overburden thickness at time of maximum burial. Much of the outboard area lies on oceanic crust, while the inboard area contains a structurally complex and variable continental crust. To determine the thermal evolution of the basin, we used crustal thickness derived from 3-D gravity inversion, temperature data and a series of 1-D basin models to map and predict lateral variation in heat flow. We then restored the eroded section beneath the Miocene unconformity using e-logs and biomarker thermal stress indicators. Uplift and erosion was quantified using both maximum thermal stress indicators with 1D models, and geophysical log responses. From the resulting points a map of net erosion was created and used in the thermal history modeling.

The resultant quantitative forward model of expelled fluid volumes from the source rocks, linked with the burial and thermal history of the reservoirs, explains differences in fluid properties. This model explains the presence of biodegraded residues in oils reservoired presently at high temperatures in the Ceiba field, and the non-biodegraded oil in the cool reservoir of the Elon pool.

AAPG International Conference and Exhibition, Cape Town, South Africa 2008 © AAPG Search and Discovery