摘要
Through observing the cores of 3 wells in a structure of the Xihu depression in East China Sea Basin and identifying rock slices,scanning electron microscopy and testing reservoir physical property,the authors recognize and restore the reservoir diagenesis and the pore evolution process.The results show that the Oligocene Huagang Formation compacted sandstone has mainly undergone the compaction,cementation,dissolution and many kinds of diagenesis.At present,it comes to from B period of the middle diagenesis stage to the late diagenesis stage.