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新疆百口泉油田百碱滩组沉积体系研究
引用本文:罗顺社,高振中,杨学文. 新疆百口泉油田百碱滩组沉积体系研究[J]. 石油天然气学报, 2006, 28(4): 15-17
作者姓名:罗顺社  高振中  杨学文
作者单位:中国地质大学(武汉)资源学院,湖北,武汉,430074,长江大学地球科学学院,湖北,荆州,434023;长江大学地球科学学院,湖北,荆州,434023;新疆油田分公司第五采油厂,新疆,克拉玛依,834000
摘    要:在详细研究岩性、古生物和测井相等相标志的基础上,认为研究区白碱滩组属辫状河三角洲湖泊沉积体系。辫状河三角洲沉积分布于上三叠统白碱滩组T3b1砂层组,由辫状河三角洲平原、辫状河三角洲前缘及前辫状河三角洲亚相组成;湖泊沉积发育于上三叠统白碱滩组T3b1砂层组,由浅湖亚相、半深湖深湖亚相组成。最后阐述了沉积微相的沉积特征和沉积演化,并提出了沉积模式。

关 键 词:百口泉油田  白碱滩组  沉积体系  辫状河三角洲沉积  湖泊沉积
文章编号:1000-9752(2006)04-0015-03
收稿时间:2006-04-23
修稿时间:2006-04-23

Sedimentary System in Baixiantan Formation of Baikouquan Oilfield in Xinjiang
LUO Shun-she,GAO Zhen-zhong,YANG Xue-wen. Sedimentary System in Baixiantan Formation of Baikouquan Oilfield in Xinjiang[J]. Journal of Oil and Gas Technology, 2006, 28(4): 15-17
Authors:LUO Shun-she  GAO Zhen-zhong  YANG Xue-wen
Abstract:On the basis of studying phase markers of lithology, paleontology and logging facies, it is considered that Baixiantan Formation belongs to braid river delta-lacustrine sedimentary system in studied area, the braid river delta sediment is distributed over the T_3b~1 sand group of Triassic Baixiantan Formation, which is composed of shallow lake subfacies, semi-deep lake-deep lake subfacies. The sedimentary characters and evolution of the sedimentary microfacies are described, and patterns of sediment are proposed.
Keywords:Baikouquan Oilfield  Baixiantan Formation  sedimentary system  braid river delta deposit  lacustrine deposit
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