青坨子凸起馆陶组地震相研究

2007年 14卷 第01期
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Seismic Facies Study of Guantao Group in Qingtuozi
Heave
王 伟1 张世奇1 纪友亮2
Wang Wei ,Zhang Shiqi ,Ji Youliang.
1 中国石油大学地球资源与信息学院, 山东东营257061; 2 同济大学海洋与地球科学学院, 上海200092
College of Geo-R esources and
Information, China University of Pe troleum, Dongy ing
257061, China
青坨子凸起馆陶组是东辛油田潜在的油气勘探区带, 但目前对本区的地层分布
和沉积相特征尚未进行系统研究, 区内钻井不多且钻井取心、录井资料较少, 因此开展区域的
沉积相研究必须依靠现有的三维地震资料。通过对青坨子凸起周缘馆陶组地震相的研究, 总
结了该区的沉积模式, 这对于下一步的油气勘探有一定的指导意义。另外, 本区河流地震相的
研究工作也可以作为其他地区地震相研究的借鉴。
Seismic facies is seism ic cells wh ich has certain
d istr ibu tion rang e, and it is the summ ation of m a in se ism ic
characteristics o f sedim entary facies in re flection section.
Guantao group of Q ingtuo zi heave is the po tentia l prospecting
area in Dongx in o ilfield, but the strata distribution and
sedim en tary fac ies have not been researched so far. The re is
few dr illing w e ll he re, ev en cor ing and logg ing inform ation is
much less. As a resu lt, sed im ent resea rch o f this area should
be based on the ex isting 3D seism ic data. Th is paper
summ ar izes sed im ent m ode o f Guantao group of Q ingtuozi
heav e through seism ic fac ies research, wh ich prov ides
gu idance for furthe r prospecting. A lso the work w e did can be
the use for re ference of seism ic fac ies resea rch in other
reg ions.
地震相 河流相 东辛油田 馆陶组;
Seismic facies, Fluvial facies, Dongx in,
Guantao group.;