首页> 外文期刊>International Journal of Earth Sciences >Liquid hydrocarbon generation potential from Tertiary Nyalau Formation coals in the onshore Sarawak, Eastern Malaysia
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Liquid hydrocarbon generation potential from Tertiary Nyalau Formation coals in the onshore Sarawak, Eastern Malaysia

机译:马来西亚东部砂拉越陆上第三纪尼亚劳组煤的液态烃生成潜力

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Tertiary coals exposed in the north-central part of onshore Sarawak are evaluated, and their depositional environments are interpreted. Total organic carbon contents (TOC) of the coals range from 58.1 to 80.9 wt. % and yield hydrogen index values ranging from 282 to 510 mg HC/g TOC with low oxygen index values, consistent with Type Ⅱ and mixed Type Ⅱ-Ⅲ kerogens. The coal samples have vitrinite reflectance values in the range of 0.47-0.67 Ro %, indicating immature to early mature (initial oil window). T_(max) values range from 428 to 436 ℃, which are good in agreement with vitrinite reflectance data. The Tertiary coals are humic and generally dominated by vitrinite, with significant amounts of liptinite and low amounts of inertinite macerals. Good liquid hydrocarbons generation potential can be expected from the coals with rich liptinitic content (>35 %). This is supported by their high hydrogen index of up to 300 mg HC/g TOC and Py-GC (S_2) pyrograms with n-alkane/alkene doublets extending beyond C_(30). The Tertiary coals are characterised by dominant odd carbon numbered n-alkanes (n-C_(23) to n-C_(33)), high Pr/Ph ratio (6-8), high TJ T_s ratio (8-16), and predominant regular sterane C_(29). All biomarkers parameters clearly indicate that the organic matter was derived from terrestrial inputs and the deposited under oxic condition.
机译:评估了在砂拉越陆上中北部暴露的三次生煤,并解释了它们的沉积环境。煤的总有机碳含量(TOC)为58.1至80.9 wt。 %,产氢指数值范围从282至510 mg HC / g TOC,低氧指数值,与Ⅱ型和Ⅱ-Ⅲ型混合干酪根一致。煤样品的镜质体反射率值在0.47-0.67 Ro%的范围内,表明未成熟到早熟(初始油窗)。 T_(max)值范围为428至436℃,与镜质体反射率数据吻合良好。第三纪煤是腐殖质,通常以镜质体为主,其中大量的锂质体和少量的惰质软化体。富含脂滑石含量(> 35%)的煤有望产生良好的液态烃生成潜力。这由其高达300 mg HC / g TOC的高氢指数和Py-GC(S_2)高温谱图支持,正构烷烃/烯烃双峰延伸超过C_(30)。三级煤的特征是主要的奇碳编号正构烷烃(n-C_(23)至n-C_(33)),高Pr / Ph比(6-8),高TJ T_s比(8-16),和主要的规则甾烷C_(29)。所有生物标志物参数清楚地表明,有机物是从陆生输入物中获得的,并在有氧条件下沉积。

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