基于无人机倾斜摄影的辫状河三角洲露头构型表征:以克孜努尔沟侏罗系阿合组为例OA
Conformational characterization of braided river delta outcrops using UAV oblique photography:A case study from the Jurassic Ahe Formation of Kezinuer Gully
为了揭示塔里木盆地库车坳陷阿合组辫状河三角洲的形成过程与沉积特征,将传统野外考察方式与无人机倾斜摄影技术相结合,对克孜努尔沟阿合组剖面进行系统观测,以储层构型理论为指导,通过旋回约束和分级解剖分析,定量表征储层砂体构型.结果显示:(1)共识别出 6种典型沉积构造、13种岩相,以及 3种典型的 4级构型单元,即分流河道、分流砂坝和废弃河道.(2)4级构型单元在垂向上呈现为分流河道与分流河道叠置、分流河道与分流砂坝叠置以及分流河道与废弃河道叠置.在侧向上呈现为分流河道与分流河道的切叠和并置、分流砂坝与分流河道的切叠,以及分流砂坝与分流砂坝的切叠.(3)分流河道厚度分布在 1.18~8.38 m,平均 4.27 m;分流河道宽度分布在 24.8~74.36 m,平均 48.92 m;分流河道宽度与厚度的相关系数为 0.74.分流砂坝厚度分布在 1.02~6.84 m,平均 3.19 m;分流河道厚度与分流砂坝厚度的相关系数为 0.71.通过实地测量,对各构型单元进行定量化分析,建立定量化模型,并对定量化模型的计算结果进行约束和校正,从而更好地实现对阿合组的定量表征.研究成果为塔里木盆地侏罗系的油气勘探提供了理论依据.
In order to reveal the formation process and depositional characteristics of the braided river delta of the Ahe Formation in the Kuqa Depression of the Tarim Basin,traditional fieldwork methods were combined with unmanned aerial vehicle(UAV)oblique photography technology to systematically observe the profile of the Ahe Formation in the Kezinuer Gully.In this study,the reservoir sand body was quantitatively characterized through cyclical constraints and hierarchical anatomical analyses with the guidance of the reservoir conformation theory.The results showed that:(1)6 typical sedimentary structures,13 lithofacies,and 3 typical fourth-level conformational units,i.e.,distributary channel,distributary bar,and abandoned channel,were identified.(2)Vertically,the fourth-order conformational units showed superimposition patterns,such as distributary channel over distributary channel,distributary channel over distributary bar,and distributary channel over abandoned channel.Laterally,the structure demonstrated the cut and stacking features,including distributary channel paired with the distributary channel,the cut and stack of the distributary bar with the distributary channel,and the cut and stacking of the distributary bar with the distributary bar.(3)The thickness of the distributary channel ranged from 1.18 to 8.38 m,with an average of 4.27 m.The width of the distributary channel spaned from 24.8 to 74.36 m,with an average of 48.92 m.The correlation coefficient between the width of the distributary channel and the thickness of the distributary bar was 0.74.The thickness of the distributary bar ranged from 1.02 to 6.84 m,with an average of 3.19 m.The correlation coefficient between the thickness of the distributary channel and the distributary bar was 0.71.Field measurements and quantitative analyses of each constitutive unit allowed the establishment of quantitative models.These models were constrained and corrected through computational adjustments,facilitating an improved quantitative characterization of the Ahe Formation.The research results provided a theoretical basis for Jurassic hydrocarbon exploration in the Tarim Basin.
万莅君;程乐利;朱柏宇;陈恭洋;叶小斌;黄保童;朱光宇
长江大学录井技术与工程研究院,湖北 荆州 434023长江大学录井技术与工程研究院,湖北 荆州 434023长江大学录井技术与工程研究院,湖北 荆州 434023长江大学录井技术与工程研究院,湖北 荆州 434023长江大学录井技术与工程研究院,湖北 荆州 434023长江大学录井技术与工程研究院,湖北 荆州 434023长江大学录井技术与工程研究院,湖北 荆州 434023
天文与地球科学
辫状河三角洲无人机倾斜摄影构型阿合组塔里木盆地
braided river deltaunmanned aerial vehicle(UAV)oblique photographyconformationAhe FormationTarim Basin
《沉积与特提斯地质》 2026 (1)
66-79,14
油田公司科技项目"库车坳陷新区新领域地质综合研究与目标优选"下设课题《北部构造带侏罗系区带评价与目标落实》(T202105.04)
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