济阳坳陷上古生界碎屑岩优质储集层发育成因机制与分布

    Genesis mechanism and distribution of high-quality reservoirs in the Upper Paleozoic clastic rocks in Jiyang Depression

    • 摘要: 围绕济阳坳陷上古生界石炭系—二叠系开展的油气资源勘探开发不断取得新突破,显示该区上古生界碎屑岩储集层具有较好的油气勘探潜力,但储集层物性特征、成岩特征、储集层发育控制因素等方面的研究程度较低。通过开展岩心观察、岩石薄片鉴定及物性测试,分析上古生界碎屑岩储集层特征和发育主控因素。结果表明: 济阳坳陷上古生界本溪组砂体岩性主要为长石岩屑砂岩和岩屑长石砂岩,太原组砂体岩性主要为岩屑石英砂岩,山西组和下石盒子组砂体岩性主要为岩屑长石砂岩和长石岩屑砂岩,上石盒子组万山段砂体岩性主要为岩屑砂岩,奎山段富集岩屑石英砂岩及石英砂岩,孝妇河段则发育单一的岩屑砂岩; 上古生界碎屑岩储集层的储集空间类型主要包括粒间孔、粒间溶孔、晶间微孔和裂缝,其中粒间溶孔最为发育,是主要的储集空间; 济阳坳陷上古生界碎屑岩储集层由本溪组到上石盒子组孔隙度和渗透率增大,中生界隆起型、浅坳型构造型式相比深坳型储集层压实程度较低、物性较好; 压实作用和胶结作用明显制约着上古生界各组段砂体优质储集层的形成,储集层中缺乏碳酸盐和长石等有利溶蚀作用对象,风化淋滤作用对储集层的改善有限; 在中生界沉积前,大王庄地区、义和庄凸起东部、孤西断裂带、王家岗地区存在剥蚀区,沿着剥蚀区周缘是上古生界有利勘探区。优质储集层发育成因机制研究与有利勘探区评价可推动对济阳坳陷上古生界油气储集层的高效勘探。

       

      Abstract: The exploration and development of oil and gas resources in the Carboniferous-Permian system of the Upper Paleozoic in Jiyang Depression have continuously achieved new breakthroughs, demonstrating that the clastic rock reservoirs in this area possess good potential for oil and gas exploration. However, the research level on reservoir physical properties, diagenetic characteristics, and controlling factors of reservoir development remains relatively low. The characteristics and main controlling factors of the development of clastic rock reservoirs in the Upper Paleozoic were studied through technical means such as core observation, rock thin section identification, and physical property testing. The results indicated that the sandstone lithology of the Upper Paleozoic Benxi Formation in Jiyang Depression was primarily composed of feldspathic lithic sandstone and lithic feldspathic sandstone. The sandstone lithology of Taiyuan Formation was mainly lithic quartz sandstone. The sandstone lithology of Shanxi Formation and Lower Shihezi Formation was primarily composed of lithic feldspathic sandstone and feldspathic lithic sandstone. The sandstone lithology of Wanshan Member of Upper Shihezi Formation was dominated by lithic sandstone, Kuishan Member was enriched in lithic quartz sandstone and quartz sandstone, and Xiaofuhe Member developed a single type of lithic sandstone. The reservoir space types of sandstone reservoirs in various formations of the Upper Paleozoic mainly included intergranular pores, intergranular dissolved pores, intercrystalline micropores, and fractures. Among them, intergranular dissolved pores were the most developed and served as the most important reservoir space. In Jiyang Depression, the porosity and permeability of the Upper Paleozoic Carboniferous-Permian clastic rock reservoirs increased from Benxi Formation to Upper Shihezi Formation, but they decreased again to Shiqianfeng Formation. In the uplifted and shallow sag tectonic style of the Mesozoic, the reservoirs had lower compaction and better physical properties compared with the deep sag tectonic style. Compaction and cementation significantly restricted the formation of dominant reservoirs in sand bodies of various formations in the Upper Paleozoic. The reservoirs lacked favorable dissolution targets such as carbonates and feldspar, and weathering and leaching had limited improvement on the reservoirs. Before the deposition of the Mesozoic, there were erosion areas in Dawangzhuang area and the east of Yihezhuang uplifts Guxi fault zone, and Wangjiagang area. The areas surrounding these erosion zones were favorable exploration zones for the Upper Paleozoic. Research on the genetic mechanism of high-quality reservoir development and the evaluation of favorable exploration zones could promote efficient exploration of the Upper Paleozoic oil and gas reservoirs in Jiyang Depression.

       

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