孤岛油田西区北馆上段3-6砂层组层序地层学研究

2006年 13卷 第02期
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Study of Sequence Stratigraphy for the 3-6 Sands of Upper Guantao Formation in the Nor th of Western Area of Gudao Oilfield
(中南大学地学与环境工程学院)
Geo logy and Environment School
of Central South U niversity, Changsha 410083, China)
孤岛油田西区北馆陶组属坳陷盆地背景下曲流河沉积, 按T - R 旋回划分的标
准西区北馆上段3 6砂层组可划分为3个层序: GS1、GS2和GS3, 7个副层序组, 其中GS1仅
发育R 旋回, GS2发育一个完整的T- R旋回, GS3仅发育T旋回。在岩心观察、粒度分析及
测井资料识别的基础上, 将孤岛油田西区北沉积相定为曲流河, 这有别于前人认为的辫状河沉
积。研究区沉积相模式与经典的曲流河沉积模式极为相似。

The Guantao Fo rm ation in the no rth o f the western area
o f Gudao O ilfield is depo sited in them eandering stream under
the depression env ironm ent. According to stratig raph ic
sequences div id ing standard o fVa i,l the Ng3-6 sands in study
area can be div ided into three sequences, GS1, GS2 and
GS3, and 7 subsequences. GS1 on ly presen ted R cyc le, GS2
presented an integrated T-R cyc le and GS3 only presen ted T
cyc le. On the basis of the core observation and the g rain s ize
analysis and the log data identify ing, the sedim entary fac ies
in study area is m eande ring stream, and th is is d iffe rent from
trad itional idea,l bra ided stream. The sed imentary m ode l in
study area is sim ilar w ith class ica lm eander ing stream.
孤岛油田西区北;坳陷盆地;曲流河;辫状河;边滩微相;
No rth o f the w estern area in Gudao
o ilfie ld, Depression bas in, M eande ring stream, Braided
stream, Po int barm icrofac ies;