吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (3): 640-651.doi: 10.13278/j.cnki.jjuese.20170003
李文强1, 郭巍1, 孙守亮2, 杨绪海1, 刘帅1, 侯筱煜1
Li Wenqiang1, Guo Wei1, Sun Shouliang2, Yang Xuhai1, Liu Shuai1, Hou Xiaoyu1
摘要: 本文利用塔里木盆地巴楚—麦盖提地区8口井53块样品开展了流体包裹体的荧光观察和显微测温、测盐系统分析,并结合埋藏史、热演化史确定了研究区古生界油气藏的主要成藏期次及成藏时间。研究结果表明,研究区古生界油气藏曾发生过2期4个幕次的油气运聚事件,即:海西晚期的早成藏阶段,其可进一步划分为晚石炭世—早二叠世(距今309.40~289.20 Ma)和晚二叠世—早三叠世(距今262.90~241.20 Ma)2个幕次;喜马拉雅晚期的晚成藏阶段,主要以高成熟油充注及天然气成藏为主,其可划分为新近纪晚期(距今6.31~4.17 Ma)和第四纪早期(距今2.31~1.62 Ma)2个幕次。结合盆地构造演化史认为,2期油气运聚事件分别受海西晚期和喜马拉雅晚期构造运动控制,印支—燕山期构造抬升中止了烃源岩演化,形成了海西晚期和喜马拉雅晚期2个重要的油气成藏时期。
中图分类号:
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