作者:张健;孙雷;苏飞;张德军;郑月娟;陈树旺;刘建勋; 时间:2019-01-01 点击数:
张健;孙雷;苏飞;张德军;郑月娟;陈树旺;刘建勋;
1:中国地质调查局沈阳地质调查中心
2:中国地质科学院地球物理地球化学勘查研究所
摘要(Abstract):
以探查松辽盆地西缘高力板断陷油气资源前景为目的实施的高D1井,在巨厚层中生代火山岩之下钻遇中侏罗统万宝组、上二叠统林西组两套油气勘探层系。根据高D1井资料,探讨研究区地层充填序列及沉积特征,分析高D1井暗色泥岩有机地球化学特征。结果表明:万宝组沉积环境为扇三角洲前缘沉积亚相,林西组沉积环境为滨浅湖和半深湖沉积亚相。万宝组烃源岩有机质丰度高、有机质类型为Ⅱ1型,整体处于低熟—成熟阶段,具备较好的生烃物质基础;林西组烃源岩有机质丰度中等,有机质类型以Ⅱ1型为主,整体处于成熟阶段,具有良好的生气前景。中侏罗统万宝组和上二叠统林西组生储盖组合完整,可以作为松辽盆地西缘油气勘探的新层系。
关键词(KeyWords):松辽盆地;高力板断陷;万宝组;林西组;沉积特征;烃源岩特征
Abstract:
Keywords:
基金项目(Foundation):中国地质调查局项目(DD20160163);中国地质调查局项目(DD20190097)
作者(Author):张健;孙雷;苏飞;张德军;郑月娟;陈树旺;刘建勋;
Email:
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