Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8123683 | International Journal of Coal Geology | 2016 | 50 Pages |
Abstract
The Rock-Eval oil saturation index (OSI) (S1 Ã 100 / TOC) value is variable because of the different characteristics of these hydrocarbon residue occurrences. OSI values in microfacies A are normally high (74.8-242.8 mg HC/g TOC, average of 117.2 mg HC/g TOC), and likely much higher if microfractures develop (> 200 mg HC/g TOC). OSI values (averaging 43.7 mg HC/g TOC) are lowest in microfacies F because of adsorption on the shales, and OSI values are the highest in microfacies D (371.3 mg HC/g TOC) and E (199.9 mg HC/g TOC) since the hydrocarbon residues are stored both in microfractures and pores between the grains. Both OSI values are high in microfacies G and H because of low TOC content. The combination of petrographic and OSI analysis appear to be a promising tool for characterizing shale oil systems.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Economic Geology
Authors
Xiaomin Xie, Maowen Li, Ralf Littke, Zhenkai Huang, Xiaoxiao Ma, Qigui Jiang, Lloyd R. Snowdon,