合肥盆地安参1井石炭二叠系的发现及其地质意义  

Discovery and geological significance of Permo-Carboniferous in Well Ancan-1,Hefei basin,China

作　　者：徐春华[1] 宋明水[2] 李学田[2] 雷敏[3] 邱连贵[3] 徐佑德[3] 江来利[4] 储东如[4] 杜森官[4] 

机构地区：[1]中国地质大学研究生院,武汉430074 [2]胜利油田有限公司勘探项目管理部,东营257000 [3]胜利油田有限公司地质科学研究院,东营257000 [4]安徽省地质调查院,合肥230001

出　　处：《成都理工大学学报（自然科学版）》2005年第6期576-580,共5页Journal of Chengdu University of Technology: Science & Technology Edition

摘　　要：合肥盆地安参1井的钻探,发现了既不同于北淮阳型,也不同于淮南型的石炭-二叠系。通过对安参1井石炭-二叠系的研究,认为是一套斜坡相-三角洲前缘沉积。结合北淮阳型石炭系和淮南型石炭-二叠系的沉积特征研究,提出了石炭-二叠纪沉积期在华北地台南缘存在完整的沟-弧-盆体系的认识;同时根据安参1井石炭-二叠系类型,结合地震、电法和平衡剖面恢复,认为合肥盆地的基底应该属于统一的华北型。The new type of Permo-Carboniferous strata is different from the northern Huaiyang type and Huainan type. It has been discovered through the drilling of Well Ancan-1. The Permo-Carboniferous strata in Well Ancan-1 are the slope-delta front deposit. There is a complete trench-arcbasin system in the south margin of North China platform based on the research of the three types of Permo-Carboniferous strata. Besides, the basement of Hefei basin belongs to a unique North China type according to the analysis of Permo-Carboniferous strata of Well Ancan-1 combined with the research of seismic, electricity and profile of equilibrium recovery.

关 键 词：合肥盆地 石炭-二叠系 沉积类型 沟-弧-盆体系 

分 类 号：P534.4[天文地球—古生物学与地层学]