石油与天然气地质 ›› 2022, Vol. 43 ›› Issue (4): 990-1004.doi: 10.11743/ogg20220419
刘贤1(), 葛家旺1,2(), 赵晓明1,2, 阴国峰3, 周雪松1, 王建伟3, 代茂林1, 孙莉3, 范廷恩4
收稿日期:
2022-04-01
修回日期:
2022-05-06
出版日期:
2022-07-14
发布日期:
2022-07-14
通讯作者:
葛家旺
E-mail:3474180093@qq.com;gjwddn@163.com
第一作者简介:
刘贤(1996—),男,在读硕士研究生,层序地层学及沉积学。E?mail: 基金项目:
Xian Liu1(), Jiawang Ge1,2(), Xiaoming Zhao1,2, Guofeng Yin3, Xuesong Zhou1, Jianwei Wang3, Maolin Dai1, Li Sun3, Tingen Fan4
Received:
2022-04-01
Revised:
2022-05-06
Online:
2022-07-14
Published:
2022-07-14
Contact:
Jiawang Ge
E-mail:3474180093@qq.com;gjwddn@163.com
摘要:
西湖凹陷是东海陆架盆地中重要的含油气凹陷,近期勘探证实渐新统花港组是当前主力产气层段;截至目前,西湖凹陷花港组层序地层划分方案还存在较大争议,严重制约了砂体等时对比及油气精细勘探进程。依据层序地层学结合天文旋回理论,利用小波变换和INPEFA技术对自然伽马曲线进行数学分析得到小波信号曲线、频谱及INPEFA曲线,建立了西湖凹陷花港组年代标尺及高精度层序界面格架。通过小波变换将GR曲线重构成不同阶次的小波信号曲线和频谱,以异常振动和能量团变化趋势凸显层序界面和旋回信息;同时,利用最大熵谱分析技术对GR曲线进行积分处理获得INPEFA曲线,以拐点和正负趋势定量拾取层序界面和旋回特征,将花港组划分为5套三级层序(自下而上分别命名为SQ1—SQ5)。利用频谱分析明确三级层序内部地层叠置旋回,结合小波信号曲线变化特征,可将花港组划分为12套四级层序(自下而上分别命名为H12—H1)。花港组GR曲线的多窗口频谱分析结果表明,5套三级层序发育持续时间介于1 ~ 3 Myr。通过多尺度多方法融合测井技术对缺少岩心和古生物化石区构建多级次等时层序地层格架具有一定推广意义,为渐新统花港组后期勘探开发提供一定的技术支持。
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