首页|塔里木盆地满加尔坳陷西缘鹰山组台地沉积分异及其油气地质意义

塔里木盆地满加尔坳陷西缘鹰山组台地沉积分异及其油气地质意义

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塔里木盆地满加尔坳陷西缘中下奥陶统鹰山组已经发现了塔河、富满、顺北等岩溶、断控型大型油气田,是塔里木盆地油气勘探的主要层系.针对相控领域迟迟未见突破、台地沉积结构不明确的问题,本次研究依据最新钻井、连片地震资料,开展沉积相、台地结构解剖和油气地质意义分析工作.从连井相-地震相对比分析,明确了满加尔坳陷西缘由东向西奥陶系沉积相变化快,碳酸盐岩台地分异性强.鹰山组下段为盆地—斜坡—台缘—开阔台地—局限台地沉积格局;到鹰山组上段随着海平面上升,台地边缘逐渐向西迁移退缩,发展成盆地—斜坡—台缘—宽缓开阔台地.台地边缘表现为南北差异:从南到北台缘斜坡带坡度减小,台缘带由南部加积结构转变为北部退积结构.这种台地结构的差异造成了与相带有关的碳酸盐岩规模储集体的差异分布,鹰山组台缘丘滩从古城到草湖西部由加积转变为退积为主,造成古城地区发育垂向叠加的礁滩相储层,厚度较大;北部由于鹰山组下段到上段台缘表现为退积特征,形成鹰下段高能丘滩储集体与上覆鹰上段斜坡相形成良好储盖组合,这种结构处于满加尔坳陷烃源岩运移方向,对于形成大型原生岩性圈闭油气聚集区带具有重要意义.
Sedimentary differentiation and its oil-gas geological significance of the Yingshan Formation platform in the west of Manjiaer depression in the Tarim basin
Large karst and fault-controlled oil and gas fields,such as Tahe,Fuman,and Shunbei,have been discovered in the middle and lower Ordovician Yingshan Formation in the western Manjiaer depression.This formation is the primary target for oil and gas exploration in the Tarim basin.However,the lack of breakthroughs in facies-controlled fields and the ambiguity surrounding platform sedimentary structures have hindered further exploration.This study analyzes sedimentary facies,platform structure,and oil and gas geological significance based on the latest drilling and contiguous seismic data.Analysis of interwell and seismic facies reveals a rapid east-west transition in Ordovician sediments and strong differentiation of the carbonate platform.The lower part of the Yingshan Formation exhibits a sedimentary pattern transitioning from basin-slope-open platform-restricted platform to basin-slope-open platform.As sea level rose in the upper part of Yingshan Formation,the platform margin gradually regressed westward,developing into a basin-slop-wide and slowly evolving open platform.The platform margin displays a north-south difference:the gradient decreases from south to north,and the platform margin transitions from an accretion structure in the south to a regressive structure in the north.This difference in platform structure results in the varied distribution of carbonate reservoir groups related to specific facies zones.From Gucheng westward to Caohu,the Yingshan Formation platform margin shifts from accretion to retrogradation,resulting in the development of thick,vertically superimposed reef-flat reservoirs.In the north,the retrograde characteristics of the platform margin in both the lower and upper Yingshan Formation members result in a favorable reservoir-cap combination:high-energy mound reservoirs in the lower Yingshan Member and slope facies in the upper Yingshan Member formed a good reservoir-cap combination.This structure lies in the migration direction of source rocks in the Manjiaer depression,making it highly significant for the formation of large-scale hydrocarbon accumulations in primary lithology traps.

carbonate platformplatform marginsedimentary differentiationlarge-scale reservoirTarim basin

杨孝群、焦存礼、邓尚、张继标、韩俊、李映涛、徐勤琪

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中国石化石油勘探开发研究院,北京,102206

中国石化西北油田分公司,新疆乌鲁木齐,830011

碳酸盐岩台地 台地边缘 沉积分异 规模储集体 塔里木盆地

2024

地质学报
中国地质学会

地质学报

CSTPCD北大核心
影响因子:2.17
ISSN:0001-5717
年,卷(期):2024.98(12)