石油与天然气地质 ›› 2025, Vol. 46 ›› Issue (2): 599-616.doi: 10.11743/ogg20250218
收稿日期:2024-09-23
修回日期:2024-11-10
出版日期:2025-04-30
发布日期:2025-04-27
第一作者简介:张倩(1992—),女,博士、助理研究员,油气储层沉积学。E-mail: zq_191class@163.com。
基金项目:Received:2024-09-23
Revised:2024-11-10
Online:2025-04-30
Published:2025-04-27
摘要:
物源分析对于追溯源-汇过程、明确有利储层展布规律具有重要意义。渤海湾盆地东营凹陷孔店组-沙河街组四段(沙四)下亚段是盆地裂陷初期充填的一套红色沉积,受多个物源共同控制,但其物源方向仍存在争议。为明确该时期物源发育特征,系统开展了砂岩碎屑组分统计、重矿物分析、泥岩全岩主量和微量元素地球化学测试以及碎屑锆石U-Pb同位素年龄研究。结果显示:①东营凹陷孔店组-沙四下亚段砂岩主要为岩屑质长石砂岩,成分成熟度较低,岩屑成分以变质岩和岩浆岩为主。②重矿物类型主要有锆石、石榴石、钛铁矿和磷灰石等。③泥岩全岩主量元素具有高硅、高铝和富碱的特征,微量元素中Li,Cr和Cs元素相对富集,稀土元素表现为轻稀土富集和Eu元素负异常的特点。④碎屑锆石U-Pb年龄范围为2 817 ~ 75 Ma,呈现多峰特征,主要年龄区间有175 ~ 130,315 ~ 250,1 900 ~ 1 855 Ma和大约2 500 Ma。研究表明,东营凹陷孔店组-沙四下亚段沉积时期具有强烈构造活动背景下的复杂母岩供源条件,母岩主要有太古宇中-酸性岩浆岩和变质岩、古元古界中-基性岩浆岩、下古生界碳酸盐岩以及中生界中-基性岩浆岩,中生界和古生界碎屑岩的再旋回对孔店组-沙四下亚段物源也具有重要贡献。结合区域构造背景和凸起区母岩性质,认为研究区在孔店组-沙四下亚段沉积时期以发育近源沉积体系为特征,主要有滨县-陈家庄体系、广饶体系和鲁西-青城体系等3大物源体系。
中图分类号:
图13
东营凹陷孔店组-沙四下亚段母岩类型判识图版a. SiO2-TiO2母岩判别图版(底图据Roser和Korsch[59]);b. TiO2-Al2O3母岩判别图版(底图据Hayashi等[60]);c. F1-F2物源判别图版(底图据Roser和Korsch[59]);d.ΣREE-La/Yb母岩判别图版(底图据Allègre和Minster[61])(F1=-1.773TiO2+0.607Al2O3+0.760Fe2O3T-1.500MgO+0.616CaO+0.509Na2O-1.224K2O-9.09;F2=0.445TiO2+0.070Al2O3-0.250Fe2O3T-1.142MgO+0.438CaO+1.475Na2O+1.426K2O-6.861;其中氧化物分子式代表氧化物含量,%。ΣREE为稀土元素总量;(La/Yb)N为球粒陨石标准化元素含量比值。)"
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