莱阳凹陷莱阳组泥页岩有机地球化学特征

Organic geochemical characteristics of the Laiyang Formation shales in Laiyang sag

  • 摘要: 胶莱盆地白垩系莱阳组泥页岩发育,且发现油气显示。通过对胶莱盆地莱阳凹陷莱阳组野外观测和室内分析,系统研究莱阳组泥页岩有机地球化学特征。胶莱盆地莱阳组烃源岩主要分布于水南段及逍仙庄段,烃源岩有机质丰度相对较高,但变化范围较大,校正TOC含量为0. 22%~3. 43%;干酪根类型包括Ⅱ1、Ⅱ2和Ⅲ型,以Ⅱ1和Ⅱ2为主,腐泥组含量40%~82%,镜质组3%~33%,惰质组10%~45%,不含壳质组组分;镜质体反射率0.50%~2.22%,成熟度相对较高。通过对暗色泥页岩厚度、有机质丰度、有机质类型、镜质体反射率等特征分析,认为莱阳凹陷莱阳组水南段为页岩气有利层段。

     

    Abstract: The Laiyang Formtion shales in Laiyang sag,with oil and gas found,are well developed. Based on the field survey and lab analysis,the authors make a systematic study on the organic geochemical characteristics of the Laiyang Formtion shales in Laiyang sag. The source rocks of Laiyang Formation,with high total organic matters content ranging from 0. 22% to 3. 43%,mainly distribute in the Shuinan section and the Xiaoxiangzhuang section. Kerogen is composed of sapropelinite (40% -82%),vitrinite (3% -33%) and inertinite (10% -45%),and no exinite was found. Kerogen types include type Ⅱ1,typeⅡ2 and type Ⅲ,particularly type Ⅱ1 and Ⅱ2. The vitrinite reflectance ranges from 0. 50% to 2. 22%,it indicates that the shales have a high maturity of organic matter. Given the thickness of black shale,TOC,kerogen types,and vitrinite reflectance,Shuinan section of Laiyang formation is a favorable target for shale gas study in Laiyang sag.

     

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