河流相地层高精度地层构型界面形成机制及识别方法_纪友亮.pdf
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2012 年 第 36 卷 中国石油大学学报( 自然科学版) Vol. 36 No. 2
第 2 期 Journal of China University of Petroleum Apr. 2012
文章编号: 1673-5005( 2012) 02-0008-08
河流相地层高精度地层构型界面形成机制
及识别方法
纪友亮,周 勇,吴胜和,史长林,岳大力
( 中国石油大学 油气资源与探测国家重点实验室,北京 102249)
摘要: 分析了河流相单砂层级别的高精度地层构型界面的形成机制及河流相自旋回对异旋回的改造和影响,总结了
单砂层级别高精度地层构型界的识别标志,及在异旋回控制下进行自旋回对比高精度地层构型界面的对比方法。
结果表明: 一个单层主要由河道侵蚀前期沉积物掠夺可容空间并逐渐充填、洪水期形成洪泛泥岩后形成; 共有 5 种河
道砂体的叠置模式和对比模式,而且河道砂体的叠置模式受可容空间增加速率与沉积物供应速率比值控制。
关键词: 河流相地层; 单层; 界面形成机制; 界面识别; 方法
中图分类号: TE 121. 34 文献标志码: A doi: 10. 3969 /j. issn. 1673-5005. 2012. 02. 002
Formation mechanism and recognizing method of high resolution
strata architecture boundary in fluvial strata
JI You-liang,ZHOU Yong,WU Sheng-he,SHI Chang-lin,YUE Da-li
( State Key Laboratory of Petroleum Resource and Prospecting in China University of Petroleum,Beijing 102249,China)
Abstract: The formation mechanism and recognizing method of high resolution strata architecture boundary of single sand bed
in fluvial strata were analyzed. The results show that the fluvial channel incises former sediments and gets accommodation
first,and then the accommodation is filled,and after the flood mud is deposited,a single bed is formed. On the basis of the
analysis,5 types of superimposed style and correlation modes of channel sand body are summarized,and it is considered that
the superimposed style of channel sand body is controlled by A /S. On the basis of the analysis of reforming and effects of auto
cycle on differen
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