Palynofacies Analysis of Selected Organic-rich Shales from Libyan Sahara: Implication to Palaeoenvironment and Hydrocarbon Source Rock Potential

I. Shushan
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Abstract

Palynofacies analysis was carried out on three (3) packages of shale-cutting samples derived from a well drilled within Gadames Basin. These included: the upper package (Carboniferous at 5,530 ft), the middle package (Carboniferous/Devonian at 5,600 ft and 5,780 ft), and the lower package (Devonian at 6,700 ft). Two palynofacies were identified: "P-1", involving the upper and middle packages (Carboniferous/Devonian), and "P-2", involving the lower package (Devonian). P-1 and P-2 were considered to form one "palynofacies association" located at a mud-dominated oxic shelf (distal shelf) and are analogous to other palynofacies from other countries that are characterized by the dominance of terrestrial upon marine palynomorphs and moderate to low phytoclasts and AOM respectively that typically deposited within a shoreline zone (probably fluvial-deltaic source or marginal marine environment). Spore color index "SCI" evaluation for source rock and thermal maturation, in turn, indicates early mature oil/gas prone (kerogen type II>III) to post mature kerogen type III>IV "gas prone" for the studied cutting sample packages.
利比亚撒哈拉富有机质页岩古环境与烃源岩潜力的古相分析
研究人员对来自Gadames盆地一口井的三(3)包页岩切割样品进行了孢相分析。其中包括:上部包层(石炭系5,530英尺),中部包层(石炭系/泥盆纪5,600英尺和5,780英尺),以及下部包层(泥盆纪6,700英尺)。鉴定出两个古岩相:“P-1”相涉及石炭系和泥盆系上、中包裹体;“P-2”相涉及下包裹体(泥盆系)。P-1和P-2被认为形成了一个位于泥质为主的含氧陆棚(远端陆棚)的“孢粉相组合”,与其他国家的其他孢粉相类似,这些孢粉相的特点是陆相和海洋孢粉相为主,分别为中低植物碎屑和AOM,通常沉积在海岸线带(可能是河流三角洲源或边缘海洋环境)内。烃源岩和热成熟度的孢子色指数“SCI”评价表明,研究的岩样包具有早成熟油气倾向(干酪根类型II>III)和后成熟干酪根类型III>IV的“气倾向”。
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