东濮凹陷胡状集北岩性油藏地层微电阻率测井地质分析

2004年 11卷 第04期
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Geologic Analysis of Lithologic Deposit with FMI in Northern Huzhuangji of Dongpu Depression


何 方1  郑宇霞1  周燕萍1  周承文2  李建荣1
He Fang , Zheng Yuxia , Zhou Yanping,et  al.


1. 中原油田分公司勘探开发科学研究院 2. 中原石油勘探局地质录井处
胡状集北岩性油藏位于东濮凹陷西部斜坡带,由于近物源快速堆积,沉积相带复杂多变,通过胡99 井地层微电阻率成像测井产生的电图像,结合常规测井曲线特征变化,对该区岩石结构、沉积砂体、构造特征进行分析,认为胡状集北岩性油藏为三角洲—湖泊相沉积,河口坝、水下分流水道相是油气聚集的有利部位,并指出了下一步的勘探开发方向。
Northern Huzhuangji lithologic deposit lies in west slope belt
of Dongpu depression. Because of proximal and rapid
accumulation ,the sedimentary facies is complicated and variable.
According to the electric image generated by FMI of Hu99 ,the
study analyzed rock texture , sedimentary sand body and
structural propert , combined with characteristic variation of
conventional log. This paper considered that northern Huzhuangji
lithologic deposit is delta2lacustrine sedimentation ,the glutenite of
major oil2bearing series is respectively mouth bar and underwater
distributary channel facies. the major object of further exploration
and development ought to be mouth bar and underwater
distributary channel facies.


胡状集北 岩性油藏 成像测井 地质分析 沉积相;
Northern Huzhuangji , lithologic deposit ,Imaging logging ,Geologic analysis ,Sedimentary facies.


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