张健;郑月娟;张德军;陈树旺;孙雷;张海华;苏飞;黄欣;

• 1:中国地质调查局沈阳地质调查中心

摘要(Abstract)：

以岩石组合特征、同位素测年及孢粉化石组合特征为依据,参考区域地层发育状况,对高力板断陷高D1井钻遇地层进行划分对比。结果表明:高D1井钻遇地层自下而上划分为晚二叠世林西组(2.911 5～2.749 0km)、早三叠世老龙头组(2.749 0～2.461 0km)、中侏罗世万宝组(2.461 0～2.191 0km)、晚侏罗世—早白垩世满克头鄂博组(2.191 0～1.206 0km)、早白垩世玛尼吐组(1.206 0km～330.0m)、早白垩世白音高老组(330.0～198.0m),以及第四系松散砂砾层(198.0～0m)。发育晚二叠世林西组和中侏罗世万宝组两套重要的生烃层系,为松辽盆地侏罗系及二叠系油气资源潜力调查与评价提供支撑。

关键词(KeyWords)：松辽盆地西缘;高力板断陷;高D1井;林西组;万宝组;地层划分

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(DD20160198);中国地质调查局项目(20190097);; 国家自然科学基金项目(31670215)

作者(Author):张健;郑月娟;张德军;陈树旺;孙雷;张海华;苏飞;黄欣;

Email:

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