石油与天然气地质 ›› 2020, Vol. 41 ›› Issue (1): 92-101.doi: 10.11743/ogg20200109
尤东华1(), 曹自成2, 徐明军3, 钱一雄1, 王石4, 王小林5
收稿日期:
2019-08-01
出版日期:
2020-02-01
发布日期:
2020-01-19
第一作者简介:
尤东华(1980-),男,博士、副研究员,碳酸盐岩储层地质学。E-mail:基金项目:
Donghua You1(), Zicheng Cao2, Mingjun Xu3, Yixiong Qian1, Shi Wang4, Xiaolin Wang5
Received:
2019-08-01
Online:
2020-02-01
Published:
2020-01-19
Supported by:
摘要:
塔里木盆地奥陶系鹰山组是油气勘探重要领域之一,发育多类型白云岩储层,其成因机制是较为关注的问题之一。基于构造-沉积背景分析、薄片鉴定、阴极发光与扫描电镜等分析手段,结合原位微区碳氧同位素、全岩碳-氧-锶同位素和流体包裹体等数据,分别解剖了浅埋藏型、岩溶型与热液改造型白云岩储层的显微岩石学与地球化学特征。浅埋藏白云石化相关储层的白云石自形程度好,不同产状白云石具有较一致的碳氧同位素组成,反应了相似的白云石化流体来源特点。岩溶型白云岩储层表现为去白云石化作用与大气淡水成因方解石的胶结,具有贫18O和富放射性87Sr特征。热液改造型白云岩储层通常以萤石和石英等热液矿物为典型标志。热液流体通常具有高温高盐度特点,形成储集空间的过程中相关白云石与方解石胶结物以贫18O和Eu正异常为特征。白云岩储层的多成因特点决定其发育分布受岩相、局部构造位置和流体性质等多因素的控制。
中图分类号:
图3
塔里木盆地玉北8井鹰山组白云岩岩石学特征与原位微区碳氧同位素分析结果 a.加厚薄片,透射光下生屑残余结构及铸模孔轮廓,埋深7 175.39 m;b.阴极发光下白云石整体不发光,孔隙内部白云石的边缘呈砖红色,埋深7 175.39 m,黄色圆圈为原位微区碳、氧同位素样品取样位置,取样直径为0.2 mm(下同);c.生屑铸模孔,阴极发光下白云石整体昏暗发光,孔隙内白云石胶结物边缘呈砖红色,埋深7 175.39 m;d.阴极发光下孔洞发育区白云石整体不发光,埋深7 174.56 m;e.直面自形白云石发育晶间孔隙,埋深7 176.34 m;f.直面自形白云石晶间发育方解石胶结物,阴极发光下白云石具中等强度呈砖红色、方解石整体不发光,埋深7 175.98 mDol.白云石;Cal.方解石;Pore.孔隙"
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