首页|琼东南盆地天然气水合物与浅层气分布特征与潜力区

琼东南盆地天然气水合物与浅层气分布特征与潜力区

扫码查看
南海北部天然气水合物勘探与钻探揭示天然气水合物与下伏浅层气具有复杂的共存关系,而天然气水合物与浅层气的共存区是未来非常规资源联合开发的目标.为查明琼东南盆地砂质储层高富集水合物与浅层气有利目标区,结合已有钻探结果及三维地震数据,通过频谱分解-RGB振幅属性融合刻画了砂质储层水合物与浅层气的空间分布特征.研究结果表明,第四纪以来块体搬运沉积体底界海底扇体为良好的富砂质储层,局部位置位于气烟囱构造顶部,受深部高通量流体运聚控制,为高富集水合物的主要目标区.研究区浅层气潜力区主要位于水道末端扇体和水道-天然堤沉积体系,多层浅层气在水合物层下方发育,浅层气藏为上方水合物提供充足的气源条件,同时浅层块体搬运沉积体与含水合物地层为浅层气发育提供良好盖层,因此,琼东南盆地存在水合物与浅层气共存的有利砂质储层勘探靶区.此外,受浅层块体搬运沉积体厚度影响,局部浅层气异常区位于水合物稳定带底界附近,有利于更大规模的水合物成藏,该目标具有良好的商业开发潜力.
The distribution characteristics and the potential target of gas hydrate and shallow gas in the Qiongdongnan basin
Gas hydrate exploration and drilling in the northern slope of the South China Sea have revealed a complex coexistence of gas hydrate and underlying shallow gas reservoirs.This coexistence area presents a promising target for future unconventional resource development and test production.This study aims to identify favorable target areas for high-concentration gas hydrate and shallow gas accumulations in sand-rich reservoirs in the Qiongdongnan basin.We use well log data and three-dimensional seismic data to characterize the spatial distribution of these reservoirsby spectral decomposition and RGB color blending techniques.Our findings show that sand-rich reservoirsare predominantly located within submarine fans located at the base of Quaternary mass transport deposits(MTDs).High gas hydrate accumulation sare locally observed at the top of gas chimney structures,which are controlled by high-flux fluid migration from deep sediments.Shallow gas,exhibiting multiplelayers,is trapped at the end of submarine fans and within channel-levee systems beneath the gas hydrate layer.This shallow gas acts as a significant source for overlying gas hydrate accumulation.Conversely,the formation of gas hydrate reduces sediment permeability,hindering upward gas migration and contributing to the enrichment of shallow gas reservoirs.Therefore,the Qiongdongnan basin presents favorable sand reservoir exploration targets characterized by the coexistence of gas hydrate and shallow gas.In addition,due to the changing of thickness of MTDs,local shallow gas anomaly area locate at the base of gas hydrate stability zone,creating conditions conducive to the formation of massive gas hydrate accumulations.This presents a highly promising target for future commercial development and exploration efforts.

gas hydrateshallow gassand-richsubmarine fanQiongdongnan basin

周吉林、李丽霞、朱振宇、王秀娟、靳佳澎、王耀葵、张正一

展开 >

海洋天然气水合物全国重点实验室,北京,100028

深海圈层与地球系统教育部前沿科学中心,海底科学与探测技术教育部重点实验室,中国海洋大学海洋地球科学学院,山东青岛,266100

中海油北京研究院,北京,100028

深海多学科交叉研究中心与海洋矿产资源评价与探测技术功能实验室,崂山实验室,山东青岛,266237

展开 >

天然气水合物 浅层气 砂层 扇体 琼东南盆地

天然气水合物国家重点实验室开放基金国家自然科学基金项目国家自然科学基金项目

2022-KFJJ-SHW4237605842206063

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(9)
  • 1
  • 20