Oil to Source Rock Correlation Using Biomarker Data Through Pattern Matching and Fingerprinting Analysis in “Kitkat” Field, Jabung Block, South Sumatra Basin

S. R. Muthasyabiha
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Abstract

Geochemical analysis is necessary to enable the optimization of hydrocarbon exploration. In this research, it is used to determine the oil characteristics and the type of source rock candidates that produces hydrocarbon in the “KITKAT” Field and also to understand the quality, quantity and maturity of proven source rocks. The evaluation of source rock was obtained from Rock-Eval Pyrolysis (REP) to determine the hydrocarbon type and analysis of the value of Total Organic Carbon (TOC) was performed to know the quantity of its organic content. Analysis of Tmax value and Vitrinite Reflectance (Ro) was also performed to know the maturity level of the source rock samples. Then the oil characteristics such as the depositional environment of source rock candidate and where the oil sample develops were obtained from pattern matching and fingerprinting analysis of Biomarker data GC/GCMS. Moreover, these data are used to know the correlation of oil to source rock. The result of source rock evaluation shows that the Talangakar Formation (TAF) has all these parameters as a source rock. Organic material from Upper Talangakar Formation (UTAF) comes from kerogen type II/III that is capable of producing oil and gas (Espitalie, 1985) and Lower Talangakar Formation (LTAF) comes from kerogen type III that is capable of producing gas. All intervals of TAF have a quantity value from very good–excellent considerable from the amount of TOC > 1% (Peters and Cassa, 1994). Source rock maturity level (Ro > 0.6) in UTAF is mature–late mature and LTAF is late mature–over mature (Peters and Cassa, 1994). Source rock from UTAF has deposited in the transition environment, and source rock from LTAF has deposited in the terrestrial environment. The correlation of oil to source rock shows that oil sample is positively correlated with the UTAF.
南苏门答腊盆地Jabung区块“Kitkat”油田生物标志物模式匹配与指纹分析对比研究
地球化学分析是油气勘探优化的必要手段。在本研究中,利用该方法确定“KITKAT”油田的原油特征和候选生烃烃源岩类型,了解已探明烃源岩的质量、数量和成熟度。通过岩石热解分析(REP)对烃源岩进行评价,确定烃源岩的烃类型;通过总有机碳(TOC)值分析,确定烃源岩的有机质含量。通过分析Tmax值和镜质体反射率(Ro)来了解烃源岩样品的成熟度。通过GC/GCMS生物标志物数据的模式匹配和指纹图谱分析,获得了候选烃源岩的沉积环境、油样发育位置等原油特征。此外,这些数据还用于了解油源岩的对比。烃源岩评价结果表明,Talangakar组烃源岩具备上述参数。上塔兰加卡尔组有机质来自可产油气的II/III型干酪根(Espitalie, 1985),下塔兰加卡尔组有机质来自可产气的III型干酪根(LTAF)。从TOC含量> 1%开始,所有TAF区间的量值都从非常好到非常好不等(Peters和Cassa, 1994)。UTAF烃源岩成熟度水平(Ro > 0.6)为成熟-晚成熟,LTAF烃源岩成熟度水平为晚成熟-超成熟(Peters and Cassa, 1994)。UTAF烃源岩沉积于过渡性环境,LTAF烃源岩沉积于陆相环境。原油与烃源岩对比表明,油样与UTAF呈正相关。
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