准噶尔盆地腹部上二叠统—下三叠统浅水辫状河三角洲沉积特征与模式

王斌; 邱岐; 陆永潮; 刘德志; 王继远; 杜学斌; 李振明; 李祥权

doi:10.11781/sysydz202304606

准噶尔盆地腹部上二叠统—下三叠统浅水辫状河三角洲沉积特征与模式

doi: 10.11781/sysydz202304606

王斌^{1, 2,},
邱岐^{1, 2},
陆永潮³,
刘德志⁴,
王继远^{1, 2},
杜学斌³,
李振明^{1, 2},
李祥权³

1.
中国石化石油勘探开发研究院无锡石油地质研究所，江苏无锡 214126
2.
中国石化油气成藏重点实验室，江苏无锡 214126
3.
中国地质大学(武汉)，武汉 430074
4.
中国石化胜利油田分公司勘探开发研究院，山东东营 257001

基金项目:

中国石化科技部项目“准噶尔盆地石炭—二叠系潜力评价与目标优选” P21077-1

“准噶尔盆地腹部下组合油气成藏条件与勘探方向” P22132

详细信息

作者简介:
王斌(1981—)，男，博士，高级工程师，从事沉积储层与油气成藏研究。E-mail：wangbin.syky@sinopec.com

中图分类号: TE121.3
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- 被引次数: 0
出版历程
- 收稿日期: 2023-05-18
- 修回日期: 2023-06-30
- 刊出日期: 2023-07-28

Sedimentary characteristics and sedimentary model of the Upper Permian-Lower Triassic shallow braided river delta in the hinterland of the Junggar Basin

WANG Bin^{1, 2
,},
QIU Qi^{1, 2},
LU Yongchao³,
LIU Dezhi⁴,
WANG Jiyuan^{1, 2},
DU Xuebin³,
LI Zhenming^{1, 2},
LI Xiangquan³

1.
Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China
2.
Key Laboratory of Petroleum Accumulation Mechanisms, SINOPEC, Wuxi, Jiangsu 214126, China
3.
China University of Geosciences (Wuhan), Wuhan 430074, China
4.
Exploration & Development Research Institute, Shengli Oilfield Company, SINOPEC, Dongying, Shandong 257001, China

摘要

摘要: 准噶尔盆地下组合油气资源规模巨大，是最重要的战略接替领域；腹部四大凹陷二叠系—三叠系发育规模三角洲砂体，并在其中连获油气新发现。为了揭示腹部凹陷区沉积特征、沉积模式和砂体展布规律，基于大量新钻井岩心、测录井和地球物理资料，系统开展了盆地原型、层序格架、古地貌恢复和沉积体系研究。准噶尔盆地腹部上二叠统—下三叠统浅水辫状河三角洲发育期具有大型坳陷湖盆发育背景，沉积时期地形平缓，坡度小，物源供给充足，水体极浅且频繁动荡，氧化和还原环境交替出现，且整体以氧化环境为主；浅水辫状河三角洲具有粒度较粗、低杂基含量、中等结构成熟度、较长距离搬运、强水动力淘洗、发育交错层理和平行层理等沉积特征；腹部地区上乌尔禾组—百口泉组沉积时期优势水系主要来自西北和东北方向，整体自北向南延伸，发育乌尔禾、克拉玛依及克拉美丽3大物源体系。盆内地形分带性明显，形成扇三角洲区、辫状河三角洲平原区、前缘区和湖区4个相带，由此在腹部地区形成了“大平原、小前缘”的浅水辫状河三角洲沉积格局，其中平原区和前缘区均为有利砂体发育地带。
- 浅水辫状河三角洲 /
- 沉积模式 /
- 上乌尔禾组 /
- 百口泉组 /
- 上二叠统 /
- 下三叠统 /
- 准噶尔盆地腹部地区
Abstract: The lower play of the Junggar Basin has huge oil and gas potential, which is the most important strategic succession field for oil and gas exploration. Large-scale delta sand bodies are developed in Permian and Triassic in the four sags in the hinterland, in which new discoveries of oil and gas have been made in succession. In order to reveal the sedimentary characteristics, sedimentary model, and distribution patterns of sand bodies in the hinterland, the studies on basin prototype, sequence framework, paleogeomorphic restoration and sedimentary system were systematically carried out based on a large number of newly drilled cores, logging and geophysical data. The results show that: the development background of large depression lake basin can be identified in the development period of the Upper Permian-Lower Triassic shallow water braided river delta in the hinterland of the basin, and the study area has the characteristics of flat terrain, small slope, sufficient material supply, extremely shallow and frequently turbulent water bodies, alternating oxidation and reduction environments, and overall oxidation environment during the sedimentation period. The shallow braided river delta is characterized by coarse grain size, low impurity content, medium texture maturity, long distance transportation, strong hydrodynamic scouring, cross bedding and parallel bedding. The advantageous water system in the sedimentation period of the Upper Wuerhe and Baikouquan formations in the hinterland mainly comes from the northwest and northeast, and extends from north to south as a whole, with three provenance systems developed, namely Wuerhe provenance, Karamay provenance and Kelameily provenance. The terrain within the basin has obvious zoning characteristics, forming four facies belts namely fan delta area, braided river delta plain area, front area and lake area, thus forming a shallow water braided river delta sedimentary pattern of "large plain, small front" in the hinterland, where plain area and front area are favorable sand body development zones.
- shallow water braided river delta /
- sedimentary model /
- Upper Wuerhe Formation /
- Baikouquan Formation /
- Upper Permian /
- Lower Triassic /
- hinterland of Junggar Basin
注释:

利益冲突声明/Conflict of Interests

所有作者声明不存在利益冲突。

All authors disclose no relevant conflict of interests.

作者贡献/Authors’ Contributions

王斌、邱岐参与论文研究思路设计；王斌、陆永潮、杜学斌完成论文结构搭建；王斌、邱岐、陆永潮、刘德志、杜学斌、李祥权、王继远、李振明参与论文写作和修改。所有作者均阅读并同意最终稿件的提交。

The study was designed by WANG Bin and QIU Qi. The paper structure was constructed by WANG Bin, LU Yongchao and DU Xuebin. The manuscript was drafted and revised by WANG Bin, QIU Qi, LU Yongchao, LIU Dezhi, DU Xuebin, LI Xiangquan, WANG Jiyuan and LI Zhenming. All the authors have read the last version of paper and consented for submission.

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图 1 准噶尔盆地构造单元划分及二叠系—三叠系综合柱状图

Figure 1. Structural unit division and comprehensive histogram of Permian-Triassic in the Junggar Basin

下载: 全尺寸图片幻灯片

图 2 准噶尔盆地腹部典型地震剖面关键不整合界面识别特征

剖面位置见图 1B-B’和C-C’。

Figure 2. Identification characteristics of key unconformity interfaces in typical seismic profiles in the hinterland of the Junggar Basin

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图 3 准噶尔盆地腹部上二叠统上乌尔禾组—下三叠统百口泉组碎屑岩岩石学特征

a.Z10井，6 801 m，T₁b，岩屑细砂岩，分选中等，磨圆次棱角状为主，个别可达次圆状，岩石成分以火山岩屑为主，方解石胶结，正交偏光；b.Z10井，6 961 m，T₁b，含砾岩屑细砂岩，分选中等，磨圆以次棱角状为主，较大的砾石颗粒可达次圆状，岩石成分以火山岩屑为主，石英含量较低，颗粒间硅质胶结，单偏光；c.Z10井，7 059.5 m，T₁b，岩屑细砂岩，分选中等，磨圆次棱角—次圆状，岩石成分以中—基性火山岩屑为主，少量石英，颗粒间浊沸石胶结, 单偏光；d.S15井，6 036 m，P₃w，砂砾岩，分选较差，磨圆次棱角—次圆状，个别较大的砾石颗粒可达圆状，成分以火山岩屑为主，石英含量低，颗粒间硅质胶结，正交偏光；e.S15井，6 196 m，P₃w，岩屑细砂岩，分选中等，磨圆次棱角—次圆状，岩石成分以中—基性火山岩屑为主，颗粒间浊沸石胶结, 单偏光；f.Z10井，7 272 m，P₃w，含砾岩屑细砂岩，分选中等，磨圆次棱角—次圆状，成分以火山岩屑为主，少量石英，颗粒间浊沸石胶结，单偏光；g.ST1井，4 936.98 m，T₁b，灰色细砾岩，砾石分选中等，磨圆次圆状为主，局部次棱角状，砾岩成分复杂，以变质砾岩为主，含变质砂岩，颗粒接触，杂基支撑；h.S12井，5 129.8 m，T₁b，灰色砂砾岩，砾石分选中等，磨圆次棱角—次圆状，砾石沿长轴方向具有定向性；i.KT1井，4 999.05 m，P₃w，灰绿色粉砂岩，发育小型板状交错层理。

Figure 3. Petrology characteristics of clastic rocks in the Upper Permian Upper Wuerhe Formation to Lower Triassic Upper Baikouquan Formation in the hinterland of the Junggar Basin

下载: 全尺寸图片幻灯片

图 4 准噶尔盆地腹部S15井上二叠统上乌尔禾组碎屑岩沉积学特征

Figure 4. Sedimentary characteristics of clastic rocks in the Upper Permian Upper Wuerhe Formation of well S15 in the hinterland of the Junggar Basin

下载: 全尺寸图片幻灯片

图 5 准噶尔盆地腹部上二叠统上乌尔禾组—下三叠统百口泉组色度指数分布

Figure 5. Chromaticity index distribution of the Upper Permian Upper Wuerhe Formation to Lower Triassic Baikouquan Formation in the hinterland of the Junggar Basin

下载: 全尺寸图片幻灯片

图 6 准噶尔盆地腹部过Z10井南北方向上乌尔禾组下段地震剖面

层拉平，井位见图 1。

Figure 6. Seismic profile of the lower section of Upper Wuerhe Formation on the SN direction crossing well Z10 in the hinterland of the Junggar Basin

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图 7 准噶尔盆地三叠系百口泉组沉积期古地貌格局

Figure 7. Paleogeomorphic pattern during the sedimentary period of Triassic Baikouquan Formation in the Junggar Basin

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图 8 准噶尔盆地腹部上二叠统—下三叠统浅水辫状河三角洲沉积模式

Figure 8. Sedimentary model of shallow braided river delta in Upper Permian-Lower Triassic in the hinterland of the Junggar Basin

下载: 全尺寸图片幻灯片

图 9 准噶尔盆地晚二叠世一早三叠世层序格架与沉积相剖面

剖面位置见图 1 A-A'

Figure 9. Sequence framework and sedimentary facies profile of Late Permian- Early Triassic in the Junggar Basin

下载: 全尺寸图片幻灯片

图 10 准噶尔盆地二叠系上乌尔禾组沉积体系平面展布

Figure 10. Plane distribution of sedimentary system of Permian Upper Wuerhe Formation in the Junggar Basin

下载: 全尺寸图片幻灯片

图 11 准噶尔盆地三叠系百口泉组沉积体系平面展布

Figure 11. Plane distribution of sedimentary system of Triassic Baikouquan Formation in the Junggar Basin

下载: 全尺寸图片幻灯片

表 1 准噶尔盆地腹部测井曲线组合特征

Table 1. Logging curve combination characteristics in the hinterland of the Junggar Basin

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