以山东李楼煤矿为研究背景，采用现场调研、工程对比、现场监测等方法，对李楼煤矿2020年以来发生的大能量事件展开研究，得出如下结论：①系统分析了支承压力分布、工作面“见方”、过断层以及回采速度等4个影响因素与大能量微震事件的关系以及大能量事件的诱发原因。1302（上）工作面采动影响范围约为工作面后方30 m至工作面前方170 m，超前应力峰值约为工作面前方70 m，而侧向微震事件主要分布在沿空巷道附近，整体向采空区一侧偏移；1303工作面微震事件在工作面推进方向的分布范围为工作面后15 m至工作面前200 m，超前应力峰值约为工作面前80 m，1303工作面微震事件在侧向分布形态呈双峰型，向运输巷一侧偏移，受宽煤柱影响，运输巷一侧应力集中程度高于回风巷一侧；工作面“见方”前，微震事件频次和能量逐渐增高，“见方”后趋于平稳；在过断层前，微震事件逐渐升高，过断层期间急剧下降，过断层后逐渐趋于平稳，事件峰值位置距离“见方”前或断层前40 m左右；当1302（上）工作面回采速度为50 m/月，1303工作面回采速度为60 m/月时，频次与能量最大。②通过分析大能量事件的诱发因素及发生位置，可将大能量事件划分为3类：“能量积聚型”大能量事件、“断层活化型”大能量事件及“孤岛结构型”大能量事件，并针对不同类型事件提出具体的防控措施，本研究将为周边类似地质因素和开采技术条件的矿井提供参考。

Based on the research background of Shandong Lilou Coal Mine, this paper used methods such as on-site investigation, engineering comparison, and on-site monitoring to research on the high-energy events that have occurred in Lilou Coal Mine since 2020, and drew the following conclusions: ①Systematically analyzed the relationship between four influencing factors and high-energy microseismic events including the distribution of abutment pressure, working face “square”, crossing faults, and mining speed, and searched the causes of large energy events. The mining influence range of No.1302 (top) working face is about 30 m behind the face to 170 m in front, and the advanced stress peak is about 70 m in front. The lateral microseismic events are mainly distributed along the gob-side entry, and the whole is offset to the side of the goaf. The distribution of microseismic events at No.1303 working face in the advancing direction of the working face ranges from 15 m behind the face to 200 m in front of the face, and the advanced stress peak is about 80 m in front of the face. The microseismic event at the No.1303 working face is bimodal in the lateral distribution pattern, shifting to the belt grooves. Affected by the wide coal pillar, the stress concentration on the belt grooves is higher than that on the track tunnel. The frequency and energy of microseismic events gradually increased before the \"square\" of the work face, and stabilized after the \"square\". Before crossing the fault, the microseismic events gradually increased, decreased sharply during the crossing, and gradually stabilized after crossing the fault. The peak position of the event was about 40 m in front of the \"square\" or before the fault. When the mining speed of 1302 (top) working face is 50 m/month and the 1303 working face is 60 m/month, the frequency and energy are the largest. ②By analyzing the inducing factors and locations of large-energy events, large-energy events can be divided into three categories: \"energy accumulation type\" high-energy events, \"fault activation type\" high-energy events, and \"island structure type\" high-energy events, and put forward specific prevention and control measures for different types. The research in this article will provide reference for surrounding mines with similar geological factors and mining technical conditions.