张迈, 唐友军, 徐兴友, 白静, 李洪波. 松辽盆地长岭凹陷青山口组一段泥页岩非均质性评价--以吉页油1井为例[J]. 地质与资源, 2021, 30(3): 265-272. DOI: 10.13686/j.cnki.dzyzy.2021.03.008
    引用本文: 张迈, 唐友军, 徐兴友, 白静, 李洪波. 松辽盆地长岭凹陷青山口组一段泥页岩非均质性评价--以吉页油1井为例[J]. 地质与资源, 2021, 30(3): 265-272. DOI: 10.13686/j.cnki.dzyzy.2021.03.008
    ZHANG Mai, TANG You-jun, XU Xing-you, BAI Jing, LI Hong-bo. HETEROGENEITY EVALUATION OF SHALE IN THE FIRST MEMBER OF QINGSHANKOU FORMATION IN CHANGLING SAG, SONGLIAO BASIN: A Case Study of JYY1 Well[J]. Geology and Resources, 2021, 30(3): 265-272. DOI: 10.13686/j.cnki.dzyzy.2021.03.008
    Citation: ZHANG Mai, TANG You-jun, XU Xing-you, BAI Jing, LI Hong-bo. HETEROGENEITY EVALUATION OF SHALE IN THE FIRST MEMBER OF QINGSHANKOU FORMATION IN CHANGLING SAG, SONGLIAO BASIN: A Case Study of JYY1 Well[J]. Geology and Resources, 2021, 30(3): 265-272. DOI: 10.13686/j.cnki.dzyzy.2021.03.008

    松辽盆地长岭凹陷青山口组一段泥页岩非均质性评价--以吉页油1井为例

    HETEROGENEITY EVALUATION OF SHALE IN THE FIRST MEMBER OF QINGSHANKOU FORMATION IN CHANGLING SAG, SONGLIAO BASIN: A Case Study of JYY1 Well

    • 摘要: 泥页岩评价是油气地球化学研究的重要内容,是了解油气资源潜力的基础.以长岭凹陷吉页油1井青一段泥页岩为研究对象,在对其有机质丰度、有机质类型及成熟度等特征分析研究的基础上,结合测井曲线,对其非均质性进行刻画描述和分级评价.得到认识如下:1)泥页岩以Ⅰ型、Ⅱ型干酪根为主,成熟度处于低成熟-成熟阶段;2)建立了非均质性刻画模型,并对泥页岩进行了分级评价,青一段暗色泥页岩以Ⅱ级资源为主,部分为Ⅰ级资源,Ⅲ级资源较少,青一上段烃源岩整体资源级别要优于青一下段.

       

      Abstract: Shale evaluation is an important part of oil-gas geochemistry research and the basis for understanding potential of oil-gas resources. Taking the shale in the first member of Qingshankou Formation in JYY1 well in Changling Sag as object, the paper evaluates the heterogeneity on the basis of organic characteristics and well logging curves. It is considered that the shale mainly belongs to Types Ⅰ and Ⅱ of kerogens, in low mature-mature stage. The characterization model of reservoir heterogeneity and grading evaluation of shale show that the dark shale in the first member of Qingshankou Formation is mainly Level-Ⅱ resource, partly Level-Ⅰ and a little Level-Ⅲ, and the overall resource level of source rocks in the upper member is better than that in the lower member of Qingshankou Formation.

       

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