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浅水扇三角洲沉积特征及演化规律:以准噶尔盆地玛东斜坡区百口泉组为例

代超 康逊 谭静强 鲁锋 连丽霞 胡瑞璞

代超,康逊,谭静强,等. 浅水扇三角洲沉积特征及演化规律:以准噶尔盆地玛东斜坡区百口泉组为例[J]. 地质科技通报,2025,44(2):1-20 doi: 10.19509/j.cnki.dzkq.tb20230518
引用本文: 代超,康逊,谭静强,等. 浅水扇三角洲沉积特征及演化规律:以准噶尔盆地玛东斜坡区百口泉组为例[J]. 地质科技通报,2025,44(2):1-20 doi: 10.19509/j.cnki.dzkq.tb20230518
DAI Chao,KANG Xun,TAN Jingqiang,et al. Sedimentary characteristics and evolution of the shallow-water fan delta: A case study of the Baikouquan Formation in the Madong slope area, Junggar Basin[J]. Bulletin of Geological Science and Technology,2025,44(2):1-20 doi: 10.19509/j.cnki.dzkq.tb20230518
Citation: DAI Chao,KANG Xun,TAN Jingqiang,et al. Sedimentary characteristics and evolution of the shallow-water fan delta: A case study of the Baikouquan Formation in the Madong slope area, Junggar Basin[J]. Bulletin of Geological Science and Technology,2025,44(2):1-20 doi: 10.19509/j.cnki.dzkq.tb20230518

浅水扇三角洲沉积特征及演化规律:以准噶尔盆地玛东斜坡区百口泉组为例

doi: 10.19509/j.cnki.dzkq.tb20230518
基金项目: 国家自然科学基金项目(42272179)
详细信息
    作者简介:

    代超:E-mail:2362552662@qq.com

    通讯作者:

    E-mail:xunkang@csu.edu.cn

  • 中图分类号: P618.13

Sedimentary characteristics and evolution of the shallow-water fan delta: A case study of the Baikouquan Formation in the Madong slope area, Junggar Basin

More Information
  • 摘要:

    砾岩作为一类特殊的油气储集层,理解其沉积成因及发育规律对于准确预测优质储层的分布至关重要。基于岩心描述、岩矿鉴定、重矿物与粒度分析等研究,结合测井、录井等资料,明确了准噶尔盆地玛东斜坡区下三叠统百口泉组砾岩的沉积特征、空间展布规律与沉积物来源,厘清了该组砾岩的沉积机制并构建了其沉积模式。研究结果表明,玛东斜坡区百口泉组沉积于浅水扇三角洲,扇体发育了扇三角洲平原、扇三角洲前缘、前扇三角洲3个亚相,包括泥石流、水上辫状河道、洪泛沉积、水下泥石流、水下主干河道、水下分支河道、砂质碎屑流、远砂坝、前扇三角洲泥共9种沉积微相,其中包含了10类岩相。结合研究区早三叠世由干旱转为湿润的古气候背景,确定该组砾岩为洪水诱发重力流的沉积产物,具有岩相组合复杂、事件性沉积标志显著、沉积模式受古气候主导、后期湖浪改造明显等特点。在空间上,玛东斜坡区百口泉组砾岩自下而上粒度逐渐变细,体现出湖侵的退覆式沉积序列,同时呈现出泥石流、水下泥石流和水下河道沉积多期叠置的特点。研究结果可为下一步油气勘探开发提供理论支持。

     

  • 图 1  玛湖凹陷基本地质背景[35](a)与百口泉组岩性柱(b)(以达13井为例)

    T2k1. 中三叠统克拉玛依组一段;T1b3. 百口泉组百三段;T1b2. 百口泉组百二段;T1b1百口泉组百一段;P2w. 中二叠统下乌尔禾组;P2w4. 中二叠统下乌尔禾组四段;下同

    Figure 1.  Geological background of the Mahu Sag [35] (a) and lithologic histogram of the Baikouquan Formation (b) (taking Da13 Well as an example)

    图 2  玛东斜坡区百口泉组扇三角洲内部成因单元综合图版

    Gmm. 杂基支撑中砾岩;Gcm. 颗粒支撑中砾岩;St. 槽状交错层理砂岩;Fm. 块状泥岩;Gcs. 砂质细砾岩;Sm. 块状砂岩;Si. 逆粒序砂岩;Sg. 含泥细砂岩;Fl. 纹层状粉砂岩;Fsm. 粉砂质泥岩

    Figure 2.  Comprehensive map of internal genetic units in fan deltas of the Baikouquan Formation, Madong slope area

    图 3  玛东斜坡区百口泉组主要储集岩相镜下、粒度及物性特征

    Figure 3.  Lithofacies, grain size and physical properties of the Baikouquan Formation reservoir in the Madong slope area

    图 4  玛东斜坡区百口泉组典型岩相组合(以达133井为例)

    Figure 4.  Typical lithofacies assemblages of the Baikouquan Formation in the Da133 Well of the Madong slope area

    图 5  玛东斜坡区百口泉组典型岩相组合(以达10井为例)

    Figure 5.  Typical lithofacies assemblages of the Baikouquan Formation in the Da10 Well of the Madong slope area

    图 6  玛东斜坡区百口泉组典型岩相组合(以玛中6井为例)

    Figure 6.  Typical lithofacies assemblages of the Baikouquan Formation in the Mazhong6 Well of the Madong slope area

    图 7  玛东斜坡区百口泉组层序划分对比剖面(AA'剖面位置见图1a

    Figure 7.  Sequence stratigraphic division in the cross section of the Baikouquan Formation in the Madong slope area

    图 8  玛东地区百口泉组夏盐扇和达巴松扇地震剖面

    Figure 8.  Seismic profiles of the Xiayan fan and Dabasong fan of the Baikouquan Formation in the Madong slope area

    图 9  近EW方向沉积相展布特征(AA'剖面位置见图1a)

    Figure 9.  Distribution of sedimentary facies in the EW trending cross section

    图 10  近SN方向沉积相展布特征(BB'剖面位置见图1a)

    Figure 10.  Distribution of sedimentary facies in the SN striking cross section

    图 11  玛东斜坡区夏盐扇和达巴松扇岩矿组成特征

    Figure 11.  Rock composition characteristics of the Xiayan fan and Dabasong fan in the Madong slope area

    图 12  玛东斜坡区百二段重矿物组分分布特征

    Figure 12.  Distribution characteristics of heavy mineral components in T1b2 in the Madong slope area

    图 13  玛东斜坡区百口泉组砾岩成因模式(a)及运移过程示意图(b)[54]

    Figure 13.  Genetic model (a) and transport process (b) of conglomerate in the Baikouquan Formation, Madong slope area[54]

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  • 收稿日期:  2023-09-07
  • 录用日期:  2024-01-17
  • 修回日期:  2024-01-15
  • 网络出版日期:  2024-01-17

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