塔里木盆地中东部中下奥陶统颗粒滩发育特征及分布

doi:10.3969/j.issn.1673-8926.2017.05.008

岩性油气藏 ›› 2017, Vol. 29 ›› Issue (5): 67–75.doi: 10.3969/j.issn.1673-8926.2017.05.008

塔里木盆地中东部中下奥陶统颗粒滩发育特征及分布

姜海健¹, 陈强路¹, 乔桂林¹, 曹自成², 储呈林¹

1. 中国石化勘探开发研究院无锡石油地质研究所, 江苏无锡 214151;
2. 中国石化西北油田分公司勘探开发研究院, 乌鲁木齐 830011

收稿日期:2016-12-10 修回日期:2017-03-03 出版日期:2017-09-21 发布日期:2017-09-21
第一作者:姜海健(1983-),男,硕士,工程师,主要从事碳酸盐岩地层沉积方面的研究工作。地址:(214151)江苏省无锡市滨湖区蠡湖大道2060号无锡石油地质研究所。Email:haijian_08@sina.com。
基金资助:
中国石化科技开发部项目“塔中、塔河奥陶系岩溶储层形成机理与分布”（编号：P13069）与中国石化西北油田分公司项目“塔里木盆地南部奥陶纪岩相古地理研究”（编号：KY2013-S-039）联合资助

Characteristics and distribution of Lower-Middle Ordovician grain bank in mid-eastern Tarim Basin

JIANG Haijian¹, CHEN Qianglu¹, QIAO Guilin¹, CAO Zicheng², CHU Chenglin¹

1. Wuxi Institute of Petroleum Geology, Research Institute of Petroleum Exploration & Production, Sinopec, Wuxi 214151, Jiangsu, China;
2. Research Institute of Exploration & Production, Sinopec Northwest Oilfield Company, Urumqi 830011, China

Received:2016-12-10 Revised:2017-03-03 Online:2017-09-21 Published:2017-09-21

摘要/Abstract

摘要： 塔里木盆地中东部顺托果勒地区及邻区已取得重大油气突破，为了对该区早中奥陶世颗粒滩的发育及分布展开进一步研究，应用钻测井、岩心、薄片、地震等资料，对颗粒滩的特征、演化、分布规律等进行综合分析。研究区发育局限台地中低能颗粒滩、开阔台地中低能颗粒滩、开阔台地中高能颗粒滩、台地边缘颗粒滩、台地边缘生物丘-生物礁等沉积亚相，且不同滩体间常交互沉积。鹰山组沉积时期，顺托果勒地区为台内缓斜坡—低凹带，广泛发育开阔台地颗粒滩，导致局部地层厚度增大；一间房组沉积时期，随着海平面快速上升，台内颗粒滩向古城地区和顺托果勒北部地区迁移，从而使得这2个地区地层厚度增大。研究认为，古地貌是颗粒滩发育与否及其发育模式的决定性因素，而海平面的变化控制了颗粒滩的发育过程和沉积样式。

关键词: 冲积扇, 河流扇, 河流沉积, 分支河流体系, 沉积体系

Abstract: There are several new gas discoveries in Shuntuoguole area of mid-eastern Tarim Basin in recent years. So,it is necessary to re-understanding Lower-Middle Ordovician carbonate sedimentary facies for further exploration. Based on cores,thin sections,logging and seismic data,the characteristics,evolution and distribution of Lower-Middle Ordovician carbonate sedimentary facies were analyzed. Grain bank developed in variety of facies such as low-energy grain bank in the restricted platform,middle to high-energy grain bank facies and middle to lowenergy grain bank facies in open platform,bank facies and reef facies on margin of platform. In Yingshan period, grain bank facies widely developed in gentle slope and low-lying zone of intraplatform in Shuntuoguole area, which open platform grain bank increased local strata thickness. With rapid uprising of sea level,In Yijianfang period,open platform extended to whole Shuntuoguole area,grain bank migrated to Gucheng area and northern Shuntuoguole area. Platform is the key factor to develop grain bank,and the sea level change controls the process and pattern of grain bank.

Key words: alluvial fan, fluvial fan, fluvial deposits, distributive fluvial system, sedimentary system

中图分类号:

TE112.2

姜海健, 陈强路, 乔桂林, 曹自成, 储呈林. 塔里木盆地中东部中下奥陶统颗粒滩发育特征及分布[J]. 岩性油气藏, 2017, 29(5): 67–75.

JIANG Haijian, CHEN Qianglu, QIAO Guilin, CAO Zicheng, CHU Chenglin. Characteristics and distribution of Lower-Middle Ordovician grain bank in mid-eastern Tarim Basin[J]. Lithologic Reservoirs, 2017, 29(5): 67–75.

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塔里木盆地中东部中下奥陶统颗粒滩发育特征及分布

Characteristics and distribution of Lower-Middle Ordovician grain bank in mid-eastern Tarim Basin

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