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苏北盆地白驹凹陷深层油气成藏研究
引用本文:刘成林,朱筱敏,费安玮,朱玉新,张英.苏北盆地白驹凹陷深层油气成藏研究[J].西南石油学院学报,2003,25(5):23-26.
作者姓名:刘成林  朱筱敏  费安玮  朱玉新  张英
作者单位:[1]石油大学,北京昌平l02200 [2]中国石油勘探开发研究院 [3]中国石油勘探开发研究院廊坊分院
摘    要:通过有机相分析、二次生烃机理研究、油气成藏静态要素和动态要素分析,对苏北盆地白驹凹陷深层油气成藏进行研究。认为:白驹凹陷深层烃源岩有机相包括B、B1和D亚相,下寒武统幕府山组(∈1mu)、下志留统高家边组(S1g)烃源岩为B亚相,生油气潜力大;无论一次生烃还是二次生烃,烃源岩总的产烃能力是一定的,二次生烃与一次生烃有一定连续性;白驹凹陷深层烃源岩二次生烃史极为复杂,大致经历了加里东期、海西-印支期、燕山期、燕山晚期-喜山期;根据成藏基本要素的不同,白驹凹陷深层油气成藏模式可分为下部油气成藏模式(下古生界)和上部油气成藏模式(上古生界)。

关 键 词:苏北盆地  白驹凹陷  烃源岩  有机相  二次生烃  油气成藏
文章编号:1000-2634(2003)05-0023-04
修稿时间:2002年10月16

A Study on Petroleum Accumulation of Deep Strata in Baiju Depression of Subei Basin
LIU Cheng,lin.A Study on Petroleum Accumulation of Deep Strata in Baiju Depression of Subei Basin[J].Journal of Southwest Petroleum Institute,2003,25(5):23-26.
Authors:LIU Cheng  lin
Abstract:The study is made up of 4 parts, which are organic facies, Secondary hydrocarbon generation mechanism, hydrocarbon generation history, and reservoir formation analyses. First, organic facies of hydrocarbon source rock are divided into B, B1 and D facies, i.e., the S1g belongs to B facies while P1q B1 facies. Second, secondary hydrocarbon generation model is made by hydrocarbon thermal simulation. Third, through basin modeling, hydrocarbon generation history is divided into 4 phases, which are Caledonian, Hercynian Indonsinian, Yanshanian, Late Yanshanian Himalayan. In the end, reservoir formation models are constructed in Baiju depression of Subei basin: one is upper reservoir formation model,the other is lower.
Keywords:Subei basin  Baiju depression  hydrocarbon source rock  organic facies  secondary hydrocarbon generation  reservoir formation
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