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A SURFACE GEOCHEMICAL SURVEY FROM DEEP WATER OFFSHORE BRUNEI

机译:文莱近海深水表面地球化学调查

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Surface geochemical prospecting involves the search for near-surface or surface anomalies of hydrocarbons, which could indicate the occurrence of petroleum accumulations or active source rocks in the sub-surface. The methodology, as applied in offshore basins, covers a range of techniques, from observation of visible oil seepage at the surface to detection of micro-seeps in near surface sediments using sensitive analytical techniques.Since most rock types are not totally impervious to hydrocarbons, both light and heavy hydrocarbons will migrate upwards, from either mature source rocks or reservoirs, to near surface sediments. While the methodology for surface geochemical surveys is the subject of continuous development, the current, most favoured practice is to detect possible migration pathways from the deep to the near-surface with the aid of seismic data, often together with remote sensing data (satellite imaging etc). The expression of such pathways at the surface is then the focus of surface geochemical prospecting grids.The results of such a survey, in deep water offshore Brunei, are presented, together with conclusions based on the full suite of surface geochemistry analyses, together with details regarding sampling and preservation of the shallow core samples. The use of analyses of the different gas fractions is presented, together with comparisons of Total Scanning Fluorescence and gas chromatography (GC) and combined gas chromatography - mass spectrometry (GC-MS) of the extract.A number of hydrocarbons seeps were detected in the survey area, ranging from being light oil- to condensate-associated, with varying degrees of biodegradation, and including seeps where hydrates were observed in the shallow cores. From thevariation in GC-MS data, the light oils are proposed to have been generated in a deltaic / terrestrial source rock similar to known Brunei oils, with the possibility of two facies / formation variations contributing in different parts of the area.
机译:地表地球化学勘探涉及寻找碳氢化合物的近地表或地表异常,这可能表明在地下发生了石油聚集或活性烃源岩。该方法应用于近海盆地,涵盖了一系列技术,从观测表层可见的油渗漏到使用灵敏的分析技术检测近地表沉积物中的微渗漏。 由于大多数岩石类型并非完全不渗透碳氢化合物,因此轻质和重质碳氢化合物都会从成熟的烃源岩或储层向上迁移到近地表沉积物。尽管地表地球化学调查的方法是不断发展的主题,但当前最受青睐的做法是借助地震数据(通常与遥感数据(卫星成像)一起,检测从深部到近地表的可能迁移路径。等等)。这样的途径在地表的表达成为地表地球化学勘探网格的重点。 介绍了在文莱近海深海进行的这种调查的结果,以及基于整套地表地球化学分析得出的结论,以及有关浅层岩心样品的采样和保存的详细信息。提出了对不同气体组分进行分析的方法,并对提取物的总扫描荧光和气相色谱(GC)以及气相色谱-质谱联用(GC-MS)进行了比较。 在调查区域内发现了许多碳氢化合物渗漏,从轻质油到凝析油伴生,生物降解程度不同,还包括在浅层岩心中观察到水合物的渗漏。来自 GC-MS数据的变化表明,轻质油是在与已知文莱油相似的三角洲/陆源烃源岩中产生的,有可能在该地区的不同地区产生两种相/地层变化。

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