--> ABSTRACT: Silurian Shale Origin for Light Oil, Condensate, and Gas in Algeria and the Middle East, by John E. Zumberge, Steve Macko, Mike Engel, Folke Johansson, Craig Schiefelbein, and Stephen Brown; #91019 (1996)

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Silurian Shale Origin for Light Oil, Condensate, and Gas in Algeria and the Middle East

John E. Zumberge, Steve Macko, Mike Engel, Folke Johansson, Craig Schiefelbein, and Stephen Brown

Two of the largest gas fields in the world, Hasi R'Mel, Algeria and North Dome, Qatar, also contain substantial condensate and light oil reserves. Gas to source rock geochemical correlation is difficult due to the paucity of molecular parameters in the former although stable isotope composition is invaluable. However, by correlating source rocks with light oils and condensates associated with gas production using traditional geochemical parameters such as biomarkers and isotopes, a better understanding of the origin of the gas is achieved.

Much of the crude oil in the Ghadames/Illizi Basins of Algeria has long been thought to have been generated from Silurian shales. New light oil discoveries in Saudi Arabia have also been shown to originate in basal euxinic Silurian shales. Key sterane and terpane biomarkers as well as the stable carbon isotopic compositions of the C15+ saturate and aromatic hydrocarbon fractions allow for the typing of Silurian-sourced, thermally mature light oils in Algeria and the Middle East. Even though biomarkers are often absent due to advanced thermal maturity, condensates can be correlated to the light oils using 1) carbon isotopes of the residual heavy hydrocarbon fractions, 2) light hydrocarbon distributions (e.g., C7 composition), and 3) compound specific carbon isotopic composition of the ight hydrocarbons. The carbon isotopes of the C2-C4 gas components can then be compared to the associated condensate and light oil isotopic composition.

AAPG Search and Discover Article #91019©1996 AAPG Convention and Exhibition 19-22 May 1996, San Diego, California