马朗凹陷芦草沟组源岩油储集空间特征及其成因

The Reservoir Space Characteristics and Origins of Lucaogou Formation Source Rock Oil in the Malang Sag

通过场发射环境扫描电子显微镜,背散射电子衍射,X射线能谱,X衍射等分析手段对马朗凹陷芦草沟组源岩油储层储集空间类型及其特征与成因进行研究。结果表明,该区源岩层的储集空间可分为5大类:原生孔,包括粒间孔、晶间孔;次生溶蚀孔隙,包括粒间溶蚀孔、粒内溶蚀孔、溶蚀缝和基质型溶蚀孔隙;有机质热演化生烃残留孔;裂缝,包括构造缝和非构造缝;纹层间由于岩石物理性质差异形成滑脱缝和破裂缝。从微观孔隙结构分析,各类微孔隙、微裂缝是源岩中烃类的主要储集空间,裂缝、微裂缝起主要的输导作用,改善储层渗透性。

The lithology of source rock oil reservoir of Lucaogou Formation in Malang sag is diverse and it mainly has mudstone, carbonatite, the transition lithology between carbonatite and mudstone, tuffaceous mud and small amounts of micrite, dolomicrite, tuff and so on. It is characterized by the lamina structure and the thickness of the lamina is 0. 1 - 10 mm. Based on the foundation of the observation of rock cores and cast slice, the macro and micro characteris- tics of the reservoir of Lucaogou Formation source rock oil in the Malang sag are studied in this paper combining with many methods of experimental analysis, such as Ar-iron polishing, scanning electronic microscopy（SEM） in the field emission environment, electron backscattering diffraction, X-ray energy spectrum, X-ray diffraction, petrographic mi- croscope, fluorescent light, and so on. The reservoir space of Lucaogou Formation source rock oil can be divided into five basic types--primary pores, secondary dissolution pores, organic hydrocarbon generating residual pores, cracks and fractures between layers of lamina and so on. Primary pores include intergranular pores which mainly exist be- tween rigid particles and intercrystal pores which exist mainly between quartz crystals and carbonate mineral crystals. Mainly secondary pores are intergranular and intragranular dissolved pores, dissolution fractures as well as caverns in the matrix. Secondary pores formed by the dissolution of the the iron calcite in shale rock samples can be seen in the scanning electron microscopy （SEM）. Dissolution fractures are formed by the all or part of dissolution of the fractures in acid fluid which are already filled with calcite first. Matrix type dissolution pores are mainly formed by the dissolu- tion of unstable minerals in the matrix of the fine grain scattered rocks, which are commonly developed and scattered distributed. After the argon polishing rock surface, nm to micron grade dissolution holes can be seen in the scanning electron microscopy. This kind of pores mainly develops in calcareous mudstone, argillaceous limestone, dolomitic mudstone and mudstone. Pores formed by the thermal evolution of organic matter, called organic matter pores, com- bon generation pores play an important part in the hydrocarbon source rock reservoir space. The linear density of cracks of source rock oil reservoir of Lucaogou Formation in Malang sag could reach a hundred per meter and are most- ly vertical cracks, followed by horizontal crack and high angle oblique crack. The development of the cracks is influ- enced by brittle mineral content, bed thickness and so on. The survey region is rich in lamina. The slippage between layers and broken cracks in laminite formed the important basis of reservoir space. As a high-quality hydrocarbon source rocks, the hydrocarbon generated in laminite can concentrate in reservoir space after an extremely short of pri- mary migration, which is beneficial to the concentration of oil source rocks. Large mounts of nanometer to micron level micro pores and micro cracks develop in the source rock oil reservoir of Lucaogou Formation and their sizes are basi- cally bigger than the diameter of liquid hydrocarbon molecules, so they could form effective reservoir space.