深水少井条件下重力流水道隔夹层识别与预测OA
Identification and prediction of gravity flow channel interlayers under deep-water and few-well conditions
琼东南盆地陵水X气田已探明天然气地质储量 128.09 亿m3,但受限于海域盆地水体深度大、钻井资料少、地震资料分辨率低、隔夹层识别不清,无法满足油气勘探需求.基于岩心、测井和地震资料,建立了隔夹层识别标准,并结合拓频与反演技术,揭示了黄流组重力流水道中不同成因隔夹层展布规律,为油气开发方案部署优化提供了依据.结果表明:①研究区整体为峡谷水道沉积体系,发育重力流水道、水道-堤岸、席状砂、滑塌沉积和深海泥 5 种微相.②黄流组发育泥质隔层、泥质夹层和钙质夹层.其中,泥质隔夹层具有高自然伽马、高密度、中声波时差以及低电阻特征;钙质夹层则表现为低自然伽马、高密度、低声波时差及高电阻特征.③泥质隔层主要分布在峡谷边缘及外部,呈大规模稳定分布;泥质夹层在峡谷内部水道两翼小规模局限分布;钙质夹层分布面积小且稳定性差.④隔夹层发育受沉积微相控制,重力流能量强时,其多出现在水道两侧堤岸泥沉积区,能量弱时则以深水原地沉积为主.⑤优化新开发井A-1 部署方案及其井轨迹,形成了一套隔夹层半定量预测技术.研究成果可为研究区和类似深水气田隔夹层识别及预测、后续油气开发提供理论指导和技术支撑.
[Objective]The X gas field of Lingshui in Qiongdongnan Basin has proven natural gas reserves of 12.809 billion cubic meters.However,oil and gas exploration has been hindered by challenges such as the large water depths of the offshore basin,limited well data,low resolution of seismic data,and unclear identification of interlayers,thereby failing to meet the requirements of oil and gas exploration.This study aims to address these challenges by establishing identification criteria for interlayers and optimizing the oil and gas development plan of the X gas field of Lingshui.[Methods]This research utilized core samples,well logging data,and seismic data,which were used to create a set of criteria for identifying interlayers in the Huangliu Formation's gravity flow channels.Additionally,frequency extension and seismic inversion techniques were employed to reveal the distribution patterns of interlayers with different genetic origins in the gravity flow channels of the Huangliu Formation,thus providing a basis for the optimization of oil and gas exploration and development deployment.[Results]The results indicated that:(1)The overall sedimentary system in the study area was a canyon-channel system,characterized by the development of five distinct microfacies:Gravity flow channels,channel-levee complexes,sheet sands,slump deposits,and deep-sea mud.(2)The Huangliu Formation contained mudstone interlayers,mudstone interbeds,and calcareous interbeds.Mudstone interlayers and mudstone interbeds show the characteristics of high natural gamma ray values,high density,moderate acoustic travel time,and low resistivity,while calcareous interbeds were distinguished by low natural gamma ray values,high density,low acoustic travel time,and high resistivity.(3)Mudstone interlayers predominantly occurred in the external and marginal areas of the canyon,forming a large-scale stable distribution,while mudstone interbeds were confined to small,local areas on the flanks of the canyon channels.Calcareous interbeds have a small distribution area and poor stability.(4)The development of these interlayers was influenced by the sedimentary microfacies.When the gravity flow energy was strong,interlayers were more commonly found in the levee mud deposits along the channel sides.Conversely,when the energy was low,interlayers were dominated by deep-water in-situ deposits.(5)An optimized deployment plan and well trajectory for the newly developed Well A-1 were proposed,leading to the establishment of a semi-quantitative prediction techniques for interlayers,which improves support for subsequent oil and gas exploration and development.[Conclusion]In conclusion,the results of this study provide significant theoretical and technical support for the identification,prediction,and subsequent oil and gas development in X gas field of Lingshui and similar deep-water gas fields.The technical methodology established in this study is expected to improve the exploration efficiency and optimizing the development strategies of deep-water hydrocarbon reservoirs.
李达;陶倩倩;刘娜;叶蓉;李华
中海石油(中国)有限公司海南分公司,海口 570100中海石油(中国)有限公司海南分公司,海口 570100长江大学地球科学学院,武汉 430100长江大学地球科学学院,武汉 430100长江大学地球科学学院,武汉 430100
天文与地球科学
琼东南盆地黄流组重力流水道沉积微相隔夹层测井识别
Qiongdongnan BasinHuangliu Formationgravity flow channelsedimentary microfaciesinterlayerwell logging identification
《地质科技通报》 2026 (2)
20-32,13
国家自然科学基金项目(4227211542272113)
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