邢翔;单敬福;

• 1:长江大学油气资源与勘探技术教育部重点实验室

• 2:长江大学地球科学学院

摘要(Abstract)：

松辽盆地东南缘深层沉积相研究程度较浅,以西丁家地区营城组为例,利用岩心观察描述结果,结合测井、地震资料,以及区域构造演化和沉积相分析结果,研究松辽盆地东南缘深层地层沉积相.结果表明:营城组(K1y)主要发育扇三角洲、辫状河三角洲、湖底扇和湖泊4种相类型,其中辫状河三角洲相和湖泊相最为发育;西丁家地区营城组主要表现为"广盆浅水"沉积特征,西南陡坡带发育扇三角洲沉积体系,北部斜坡带发育辫状河三角洲沉积体系,垂向上地层叠加样式表现为由进积向加积演变.该研究结论对西丁家地区深层地层下一步勘探开发及资源评价具有指导意义.

关键词(KeyWords)：西丁家地区;早白垩世;营城组;沉积相;松辽盆地;十屋断陷

Abstract:

Keywords:

基金项目(Foundation):国家科技重大专项(ZX05009);; 湖北省教育厅基金项目(Q20121210);; 中国地质大学(武汉)重点实验室开放基金项目(TPR-2012-23)

作者(Author):邢翔;单敬福;

Email:

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