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首页> 外文期刊>Journal of Asian earth sciences >Anomalies of natural gas compositions and carbon isotope ratios caused by gas diffusion - A case from the Donghe Sandstone reservoir in the Hadexun Oilfield, Tarim Basin, northwest China
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Anomalies of natural gas compositions and carbon isotope ratios caused by gas diffusion - A case from the Donghe Sandstone reservoir in the Hadexun Oilfield, Tarim Basin, northwest China

机译:天然气扩散引起的天然气组成和碳同位素比异常-以塔里木盆地哈得逊油田东河砂岩油藏为例

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摘要

Natural gases in the Carboniferous Donghe Sandstone reservoir within the Block HD4 of the Hadexun Oilfield, Tarim Basin are characterized by abnormally low total hydrocarbon gas contents ( 65%), low methane contents ( 10%) and low dryness coefficients ( 0.5), and a reversal of the normal trend of carbon isotope ratios, showing delta C-13 methane (C-1) delta C-13 ethane (C-2) delta C-13 propane (C-3) delta C-13 butane (C-4). Specifically, methane is enriched in C-13 with the variations in delta C-13(1) values between gases from Block HD4 and gases from its neighboring blocks reaching 10 parts per thousand. This type of abnormal gas has never been reported previously in the Tarim Basin and such large variations in delta C-13 have rarely been observed in other basins globally. Based on a comprehensive analysis of gas geochemical data and the geological setting of the Carboniferous reservoirs in the Hadexun Oilfield, we reveal that the anomalies of the gas compositions and carbon isotope ratios in the Donghe Sandstone reservoir are caused by gas diffusion through the poorly-sealed caprock rather than by pathways such as gas mixing, microorganism degradation, different kerogen types or thermal maturity degrees of source rocks. The documentation of an in-reservoir gas diffusion during the post entrapment process as a major cause for gas geochemical anomalies may offer important insight into exploring natural gas resources in deeply buried sedimentary basins.
机译:塔里木盆地哈得逊油田HD4区块石炭系东河砂岩储层中的天然气具有异常低的总烃气含量(<65%),低甲烷含量(<10%)和低干燥系数(<0.5) ,并且碳同位素比的正常趋势发生了逆转,显示了δC-13甲烷(C-1)>δC-13乙烷(C-2)<δC-13丙烷(C-3)<δC- 13丁烷(C-4)。具体来说,甲烷在C-13中富集,来自区块HD4的气体与来自其相邻区块的气体之间的差值C-13(1)值变化达到千分之十。塔里木盆地以前从未报道过这种异常气体,在全球其他盆地中很少见到C-13如此大的变化。通过对天然气地球化学数据和哈德逊油田石炭系油藏地质背景的综合分析,我们发现东河砂岩油藏的气体组成和碳同位素比值异常是由于气体通过密封不良造成的扩散所致。而不是通过诸如气体混合,微生物降解,不同的干酪根类型或烃源岩的热成熟度等途径。圈闭后过程中的储集层内气体扩散是造成天然气地球化学异常的主要原因,这可能为探索深埋沉积盆地的天然气资源提供重要的见识。

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  • 来源
    《Journal of Asian earth sciences》 |2018年第may1期|75-89|共15页
  • 作者单位

    China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China;

    China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China;

    China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China;

    PetroChina, Tarim Oilfield Co, Res Inst Explorat & Dev, Korla 84100, Xinjiang, Peoples R China;

    China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China;

    China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China;

    China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China;

    China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Tarim basin; Hadexun oilfield; Donghe sandstone reservoir; Natural gas; Carbon isotope ratios; Gas diffusion;

    机译:塔里木盆地;哈得逊油田;东河砂岩油藏;天然气;碳同位素比;天然气扩散;

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