琼东南盆地黄流组中央峡谷水道 储层特征及主控因素

作    者:钟佳1,2,代龙1,2,朱沛苑1,2,吴仕玖1,2,焦垚祺1,2
单    位:1 中海石油(中国)有限公司湛江分公司;2 中海石油(中国)有限公司海南分公司
基金项目:
摘    要:
琼东南盆地中央峡谷水道气田是我国海域自营勘探发现的第一个深水大气田,是南海西部油气田上产的重 要支撑。为合理制定气田开发方案,基于岩心微观分析测试资料与工程测试数据,针对琼东南盆地乐东—陵水凹陷 黄流组中央峡谷水道开展储层岩石学、物性、孔隙结构特征研究,划分储层类别并探究储层特征差异性的控制因素。 结果表明:① 峡谷水道储层以粉砂岩、细砂岩为主,储集空间以粒间孔为主,其次为粒间溶孔、粒内溶孔,喉道介于 中—微喉。② 综合储层物性、流动性、产能(米无阻流量)、岩性及孔隙结构特征,可将峡谷水道储层划分为好、中等、 差以及致密等4类。研究区峡谷水道自西向东储层品质逐渐变好:好储层分布于东部陵水X区、陵水ZX区,中等储层 分布于陵水Z区,差储层分布于西部崖城A区、崖城B区,致密储层在以上区域均有少量分布。③ 峡谷水道的水动力 条件是制约储层品质的基础因素,压实作用和碳酸盐胶结会缩小和堵塞孔喉,异常超压可延缓压实进程、保留粒间 孔,这些因素共同决定了峡谷水道在不同区块的孔隙结构、储集物性差异明显。研究成果可为中央峡谷水道气田群 下一步的油气勘探目标优选以及后续开发方案的优化提供依据。
关键词:孔隙结构;储层;中央峡谷水道;黄流组;乐东—陵水凹陷;琼东南盆地

Reservoir characteristics and its main controlling factors of the Central Canyon-Channel of Huangliu Formation in Qiongdongnan Basin

Author's Name: ZHONG Jia, DAI Long, ZHU Peiyuan, WU Shijiu, JIAO Yaoqi
Institution: 
Abstract:
The Central Canyon-Channel Gasfield in Qiongdongnan Basin is the first deep-water large-scale gas field discovered by self operated exploration in China sea area, which is an important support for the production of oil and gas fields in the western South China Sea. Influenced by the large-scale decline of global sea level, the basin had sufficient sediment sources during the deposition of the upper Miocene Huangliu Formation, and incised turbidity channels called the Central Canyon-Channel (CCC) developed through the whole basin. In order to reasonably formulate the gas field development plan, based on the core analysis data and engineering test data, the petrology, physical property, and pore structure of the CCC sandstone of Huangliu Formation in Ledong Sag-Lingshui Sag were revealed, and the reservoir types were classified and the control factors for the difference of reservoir characteristics were explored. The results show that: (1) The lithology of the CCC is dominated by siltstone and fine sandstone. The pore space is dominated by intergranular pores, followed by intergranular and intragranular dissolution pores. The pore throat size varies from medium to micro, being different among different development blocks. (2) Based on the physical property, fluidity, petrology, productivity, lithology and pore structure, the CCC reservoir can be divided into four types: good, medium, poor and tight. The quality of the CCC reservoir gradually improves from west to east: the good reservoir is distributed in the Lingshui X, ZX blocks, the medium reservoir is distributed in the Lingshui Z block, the poor reservoir is distributed in the Yacheng A, B blocks, and tight reservoir is distributed commonly in a small amount in all blocks. (3) Hydrodynamic conditions primarily control the CCC reservoir quality. Compaction and carbonate cementation reduce pore throat. Abnormal overpressure inhibit the compaction process and retain intergranular pores. These factors together determine the distinct variation in the pore structures among different development blocks. This research will provide a new visual angle that is beneficial for the optimization of exploration targets and development plans of the CCC Gasfield.
Keywords: pore structure; reservoir; Central Canyon-Channel; Huangliu Formation; Ledong Sag-Lingshui Sag; Qiong⁃ dongnan Basin
投稿时间: 2023-07-07  
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