盆1井西凹陷东环带三工河组层序地层格架及沉积特征OA
Sequence stratigraphic framework and sedimentary characteristics of Sangonghe Formation in the eastern ring of West Sag of Well Pen-1
盆 1 井西凹陷东环带位于准噶尔盆地腹部,是中国油气勘探重要目标区之一,但当前下侏罗统三工河组层序地层格架划分仍存在分歧.文中基于测井和岩心资料,利用最大熵谱、预测误差滤波、合成预测误差滤波、瞬时相位余弦和小波时频等分析方法,对岩性敏感的测井曲线进行处理,得到频率趋势、瞬时相位余弦和不同尺度下的小波系数等曲线及时频色谱;通过分析所得曲线不同幅度的趋势拐点、振荡特征和时频色谱图的能量变化等,识别不同级次层序界面;通过对研究区钻遇三工河组的 53 口钻井进行单井地层划分,并选取其中 28 口井进行层序格架连井对比分析,对三工河组二段(J1s2)和三段(J1s3)层序地层格架及沉积分布特征进行研究.研究结果表明,研究区 J1s2 和 J1s3 整体构成一个三级层序,内部发育低位(LST)、湖侵(TST)和高位(HST)三个体系域,且 J1s2 可划分为 4 个四级层序;研究区沉积中心呈迁移特征,主要分布在西北和东北区域,最大的沉积中心在 Z11 和 QS4 井区附近.最终建立了 J1s2 和 J1s3 高精度层序地层对比格架,识别了各级层序和沉积界面,明确了其空间沉积特征,为研究区油气精细勘探奠定了基础.
Located in the central Junggar Basin,the eastern ring of the West Sag of Well Pen-1 is a significant tar-get for oil and gas exploration in China.However,controversies persist in terms of the sequence stratigraphic framework division of the Lower Jurassic Sangonghe Formation.Based on logging and core data,this paper adopts analytic methods including maximum entropy spectral analysis,prediction error filter analysis(PEFA),integrated prediction error filter analysis(INPEFA),cosine of instantaneous phase,and wavelet time-frequency analysis to process lithology-sensitive logging curves.As a result,curves such as the frequency trend,cosine of instantaneous phase,and wavelet coefficients at different scales as well as time-frequency chromatograms are ob-tained.Sequence boundaries of different orders are identified by analyzing trend inflection points of varying am-plitudes,oscillation characteristics of the obtained curves,and energy variations in the time-frequency chromato-grams.Single-well stratigraphic division is conducted on 53 drilled wells penetrating the Sangonghe Formation in the study area,and 28 of them are selected for cross-well sequence framework correlation analysis.Addition-ally,the sequence stratigraphic framework and sedimentary distribution characteristics of the second member of Sangonghe Formation(J1s2)and the third member of Sangonghe Formation(J1s3)are studied.The research re-sults indicate that J1s2 and J1s3 in the study area collectively constitute a third-order sequence,internally de-veloping three system tracts of the lowstand system tract(LST),transgressive system tract(TST),and high-stand system tract(HST).Furthermore,J1s2 can be divided into four fourth-order sequences.The depocenter of the study area exhibits migratory patterns,primarily distributed in the northwestern and northeastern parts,with the most significant depocenters located near the Z11 and QS4 wells.Finally,a high-precision sequence strati-graphic correlation framework for J1s2 and J1s3 is established,various sequences and sedimentary boundaries are identified,and their spatial sedimentary characteristics are clarified,thus laying a foundation for the detailed oil and gas exploration in the study area.
殷文;周银风;许涛
中国石油大学(北京)克拉玛依校区,新疆 克拉玛依 834000中国石油大学(北京)克拉玛依校区,新疆 克拉玛依 834000中国石油大学(北京)克拉玛依校区,新疆 克拉玛依 834000
天文与地球科学
盆1井西凹陷三工河组层序分析层序地层格架沉积特征
West Sag of Well Pen-1Sangonghe Formationsequence analysissequence stratigraphic frameworksedimentary characteristic
《石油地球物理勘探》 2026 (2)
426-437,12
本项研究受新疆维吾尔自治区重点研发计划项目"超高温高压环境下复杂油气藏地球物理关键技术研发"(2024B01016)资助.
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