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准噶尔西北缘红山嘴地区克上组辫状河三角洲沉积-储层耦合关系与综合定量评价

高阳, 刘文峰, 于兴河, 杨新涛

高阳, 刘文峰, 于兴河, 杨新涛. 准噶尔西北缘红山嘴地区克上组辫状河三角洲沉积-储层耦合关系与综合定量评价[J]. 中国地质, 2020, 47(4): 971-984. DOI: 10.12029/gc20200405
引用本文: 高阳, 刘文峰, 于兴河, 杨新涛. 准噶尔西北缘红山嘴地区克上组辫状河三角洲沉积-储层耦合关系与综合定量评价[J]. 中国地质, 2020, 47(4): 971-984. DOI: 10.12029/gc20200405
GAO Yang, LIU Wenfeng, YU Xinghe, YANG Xintao. Coupling relationship of sedimentation-reservoir and comprehensive quantitative evaluation of braided river delta facies in Upper Karamay Formation, Hongshanzui area, northwestern margin of Junggar Basin[J]. GEOLOGY IN CHINA, 2020, 47(4): 971-984. DOI: 10.12029/gc20200405
Citation: GAO Yang, LIU Wenfeng, YU Xinghe, YANG Xintao. Coupling relationship of sedimentation-reservoir and comprehensive quantitative evaluation of braided river delta facies in Upper Karamay Formation, Hongshanzui area, northwestern margin of Junggar Basin[J]. GEOLOGY IN CHINA, 2020, 47(4): 971-984. DOI: 10.12029/gc20200405

准噶尔西北缘红山嘴地区克上组辫状河三角洲沉积-储层耦合关系与综合定量评价

基金项目: 

国家自然科学基金项目 No. 41472091

详细信息
    作者简介:

    高阳, 男, 1988年生, 博士, 工程师, 主要从事沉积学、储层表征与建模研究; E-mail:gaoyangdzdx@126.com

  • 中图分类号: TE111.3

Coupling relationship of sedimentation-reservoir and comprehensive quantitative evaluation of braided river delta facies in Upper Karamay Formation, Hongshanzui area, northwestern margin of Junggar Basin

Funds: 

National Science Foundation of China No. 41472091

More Information
    Author Bio:

    GAO Yang, male, born in 1988, doctor, engineer, engages in sedimentology, reservoir characteristization and modeling; E-mail:gaoyangdzdx@126.com

  • 摘要:

    综合岩心、薄片、分析测试资料厘定辫状河三角洲不同相带储层特征及控制因素,选取孔隙度、含砂率、优势砂厚、优势砂岩分层系数及杂基含量作为评价参数,基于灰色关联法确定权重、拐点法确定分类阈值对储层进行综合定量评价。结果表明辫状河三角洲下平原地区由于储层物性好且优势砂岩(粗砂岩)占比高而Ⅰ类储层发育;三角洲上平原地区砂体发育但以砾岩沉积为主,杂基含量高而储层质量差,多为Ⅱ类储层;三角洲前缘地区正韵律特征显著,中、粗砂岩储层质量要优于细砂岩,但优势砂岩发育规模有限,因此多以Ⅱ类、Ⅲ类储层为主。该成果可为复杂砂砾岩储层的定量评价提供借鉴。

    Abstract:

    Core observation, thin section identification and data test were applied to analyzing the characteristics and quality-controlling factors of reservoirs in braided river delta. 5 parameters of porosity, ratio of sandbody, effective sandbody thickness, stratification coefficient of effective sandbody and matix content were chosen to evaluate the reservoir quantitatively, and gray correlation method was used to determine the weight coefficient and make critical point analysis to confirm the threshold value of various reservoirs. The results show that the lower delta plain is mainly classified as TypeⅠreservoir due to its good reservoir physical property and well-development of effective sandbody, while, in the upper delta plain, conglomerates of high matix content and poor physical property are assigned to typeⅡreservoir. The reservoir quality in delta front varies as its remarkable grain rhythm, with good quality in medium and coarse sandstone and poor quality in fine sandstone. And a limited development scale of the effective sandbody causes the delta front to be more likely recognized as TypeⅡand type Ⅲ reservoir. The results can provide reference for the quantitative evaluation of complex conglomerate reservoirs.

  • 图  1   研究区区域地理位置与地层发育特点

    Figure  1.   The regional location of the study area and the stratigraphic column

    图  2   克上组辫状河三角体系沉积岩石学特征

    a—灰绿色块状中砾岩, 分选差, 次棱—次圆, 为碎屑流快速堆积结果;b—灰色砂质细砾岩, 可见砾石定向排列, 反映牵引流底负载沉积;c—灰色细砾岩, 正粒序, 槽状交错层理发育, 为河道下切充填产物;d—深灰色粗砂岩, 槽状交错层理;e—灰褐色含砾粗砂岩, 块状, 反映物源供给充足且快速沉积;f—深灰色粗砂岩, 板状交错层理, 反映河道顺流加积或侧积;g—灰色中砂岩, 平行层理, 河道序列顶部高流态层流产物;h—灰色粗砂岩, 见泥岩滑塌, 多为前缘快速堆积背景下滑塌结果;i—灰黑色粉砂岩, 浪成沙纹, 反映波浪淘洗作用;j—深灰色粉砂质泥岩, 水平层理, 反映静水沉积环境;k—灰绿色细砾岩, 基质支撑;l—红褐色块状泥岩;m—红褐色粉砂质泥岩, 与l主要响应陆上暴露环境;n—灰黑色泥岩, 块状, 代表静水还原环境;o—深灰色泥岩, 见碳化植物茎干, 说明沉积时期地层坡度大, 沉积物快速堆积埋存

    Figure  2.   Sedimentary petrological characteristics of braided river delta system in Upper Karamay Formation

    a- Grayish green massive medium conglomerate, poorly sorted, sub-edge to sub-circle, which is the result of rapid accumulation of clastic flow; b- Gray sandy fine conglomerate with directional arrangement of gravels, reflecting the bottom load deposition of traction flow; c-Gray fine conglomerate, fining-upward sequence, trough cross bedding, mostly the product of channel cutting and filling; d-Dark gray coarse sandstone with trough cross bedding; e- Grayish brown gravelly coarse sandstone, massive bedding, showing that the source supply is sufficient and deposition rate is fast; f- Dark gray coarse sandstone, tabular cross bedding, reflecting the downstream accretion or lateral deposition of the channel; g-Gray medium sandstone, parallel bedding, developed at the top of the channel sequence in a high flowing laminar flow; h-Gray coarse sandstone, mudstone slump seen, which is mostly the result of rapid accumulation of delta front; i- Grayish black siltstone, with small-scale wave-ripple cross bedding, reflecting the wave washing; j- Dark gray silty mudstone with horizontal bedding, deposited in the still water sedimentary environment; k- Grayish green fine conglomerate, supported by matrix; l-Reddish brown block mudstone; m- Reddish brown silty mudstone, like l, mainly responding to a exposure environment; n- Grayish black block mudstone, representing a still water, restore environment; o-Dark gray mudstone, with carbonized plant stems, indicating that the terrain slope was large during the sedimentation period, and the sediments were rapidly accumulated and buried

    图  3   辫状河三角洲上平原地区沉积储层综合特征

    Figure  3.   Sedimentary and reservoir characteristics in the upper delta plain of braided river delta

    图  4   辫状河三角洲下平原地区沉积储层综合特征

    Figure  4.   Sedimentary and reservoir characteristics in the lower plain of braided river delta

    图  5   辫状河三角洲前缘地区沉积储层储层特征

    Figure  5.   Sedimentary and reservoir characteristics in braided river delta front

    图  6   辫状河三角洲不同相带储层响应特征

    Figure  6.   Reservoir response characteristics of different microfacies in braided river delta

    图  7   克上组辫状河三角洲储层岩性与孔隙度关系

    Figure  7.   Relationship between lithology and porosity in braided river delta of Upper Karamay Formation

    图  8   储层杂基含量与物性关系

    Figure  8.   Relationship between matix content and reservoir physical properties

    图  9   用于储层评价的不同沉积参数概念及其计算方法

    Figure  9.   The concept and calculation method of different sedimentary parameters for reservoir evaluation

    图  10   储层综合评价指标概率累计曲线

    Figure  10.   Cumulative probability curve of comprehensive reservoir evaluation index

    图  11   沉积微相与储层评价结果展布特征对比

    a—MSC1上升半旋回沉积微相平面展布图;b—MSC1上升半旋回储层综合评价结果平面图展布

    Figure  11.   Comparison of sedimentary microfacies and reservoir evaluation results

    a-Plane distribution of MSC1 rising sub-cycle sedimentary microfacies; b-Plan view distribution of comprehensive evaluation results of MSC1 rising sub-cycle reservoir

    表  1   不同储层质量评价参数权重系数

    Table  1   Weight coefficient of different reservoir quality evaluation parameters

    下载: 导出CSV

    表  2   辫状河三角洲体系储层综合定量评价参数统计特征

    Table  2   Parameter characteristics of reservoir evaluation in braided river delta

    下载: 导出CSV
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出版历程
  • 收稿日期:  2018-06-04
  • 修回日期:  2018-09-05
  • 网络出版日期:  2023-09-25
  • 刊出日期:  2020-08-24

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