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塔中4井区东河砂岩段中的河口湾沉积
引用本文:郭建华,翟永红.塔中4井区东河砂岩段中的河口湾沉积[J].石油天然气学报,1995,17(4):5-11.
作者姓名:郭建华  翟永红
作者单位:江汉石油学院石油地质系,江汉石油学院学报编辑部
基金项目:塔里木石油勘探开发指挥部资助
摘    要:地震、测井、岩心以及微量元素资料的分析表明,塔中4井区石炭系东河砂岩段中下部发育有河口湾沉积体系,其主体由潮下潮汐沙坝、滨面、潮坪及河流沉积积组成。河口湾沉积体的垂向序列由一组向上变细的旋回层构成,这种旋回层是由潮下潮汐通道的迁移或摆动造成的,区域上不能进行横向对比。

关 键 词:沉积  沉积特征  塔里木盆地  沉积作用  水力作用

Estuary Sedimentary System of Carboniferous Donghe Sand in Tazhong 4 Well Area
Guo Jianhua,Wu Zhiyong Zhai Yonghong Liu Shengguo.Estuary Sedimentary System of Carboniferous Donghe Sand in Tazhong 4 Well Area[J].Journal of Oil and Gas Technology,1995,17(4):5-11.
Authors:Guo Jianhua  Wu Zhiyong Zhai Yonghong Liu Shengguo
Abstract:An analysis of seismic,logging, cores and elements data demonstrates that an estuary sedimentary system in the middle-lower parts of Carboniferous Donghe Sand member in Tazhong 4 well area,Tarim Basin is made up mainly of tidal bar,shoreface, tidal flat and fluvial deposits.Up-finer cyclothems resulting from the shift of tidal channels constitute the main part of a vertical sequence of estuary deposits. The cyclothems are not used to correlate laterally in region. Nevertheless, overall characteristics of up-finer and retrogradation show that the estuary deposits are accumulated in the process of transgression.
Keywords:estuary  deposition(geology)  depositional cycle  depositional feature  Carboniferous period  Tarim Basin
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