Characteristics of Cepu Block Oil, Wonocolo Formation, East Java Indonesia: Study of aliphatic biomarkers

Y. Zetra, R. Burhan, Awalia W. Firdaus, Zjahra V. Nugrahaeni, T. Gunawan
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Abstract

The research of organic geochemistry has been carried out through the report of aliphatic hydrocarbon fraction biomarkers in Cepu Block oil, Wonocolo Formation, East Java. Organic geochemistry studies were carried out through biomarker analysis such as the depositional environment, the origin of organic compounds, and the maturity of Cepu Block crude oil samples. The biomarker was analyzed using extraction, fractionation, and structure identification methods by Gas Chromatography-Mass Spectrometer (GC-MS). The odd-to-even carbon number predominance of n-alkanes with a CPI value of 1.04 indicates that the organic material sample had low maturity. The indicator of maturity is also supported by the Ts/Tm ratio of 0.52, and the abundance of 17α(H),21β(H)-hopane which is lower than 17β(H),21a(H)-hopane, and the high abundance of 5α(H)-7-cholestene. The ratio of pristane/phytane (Pr/Ph) of 3.25 and Ts/(Tm+Ts) ratio of 0.34 indicates that the oil sample came from an oxidative depositional environment. The bimodal distribution of n-alkane biomarkers with a ratio of long-chain to short chains n-alkanes (Σ2/Σ1) of 1.25 indicates that the source of oil organic compounds comes from higher plants, bacteria, and algae. The presence of hopane and homohopane, 8β(H)-drimane and homodrimane compounds, and also the sterane group indicates the presence of bacterial input with bacteriohopanetetrol precursors produced by Archaebacteria. The results that have been obtained indicate that the Cepu Block oil sample, Wonocolo Formation has various organic sources with low maturity.
印尼东爪哇Wonocolo组Cepu区块油特征:脂肪族生物标志物研究
通过对东爪哇乌诺科洛组Cepu区块油中脂肪烃组分生物标志物的报道,开展了有机地球化学研究。通过沉积环境、有机质成因、原油成熟度等生物标志物分析,开展了有机地球化学研究。采用气相色谱-质谱联用技术(GC-MS)对生物标志物进行提取、分离和结构鉴定。正构烷烃的奇偶碳数优势,CPI值为1.04,表明有机质样品成熟度较低。Ts/Tm比值为0.52,17α(H)、21β(H)-藿烷丰度低于17β(H)、21a(H)-藿烷,5α(H)-7-胆甾醇丰度较高。原烷/植烷比值(Pr/Ph)为3.25,Ts/(Tm+Ts)比值为0.34,表明油样属于氧化沉积环境。长链正烷烃与短链正烷烃之比(Σ2/Σ1)为1.25的正烷烃生物标志物双峰分布表明,油类有机物来源于高等植物、细菌和藻类。hopane和homhopane, 8β(H)-drimane和homdrimane化合物以及甾烷基团的存在表明存在细菌输入,细菌hoppanetetrol前体是由古细菌产生的。研究结果表明,柴浦区块油样具有低成熟度的多种有机质来源。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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