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    雷竞技app官方版下载ios-雷竞技官方平台

    臧素华

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    文章导航 > 石油实验地质  > 2024 >  46(2): 238-246
    臧素华. 雷竞技app官方版下载ios-雷竞技官方平台[J]. 石油实验地质, 2024, 46(2): 238-246. doi: 10.11781/sysydz202402238
    引用本文:
    臧素华. 雷竞技app官方版下载ios-雷竞技官方平台[J]. 石油实验地质, 2024, 46(2): 238-246. doi: 10.11781/sysydz202402238
    shu
    ZANG Suhua. Reservoir characteristics and hydrocarbon accumulation significance of metamorphic zones of intrusive rocks and surrounding rocks in second member of Paleocene Funing Formation in Qintong Sag, Subei Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(2): 238-246. doi: 10.11781/sysydz202402238
    Citation:
    ZANG Suhua. Reservoir characteristics and hydrocarbon accumulation significance of metamorphic zones of intrusive rocks and surrounding rocks in second member of Paleocene Funing Formation in Qintong Sag, Subei Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(2): 238-246. doi: 10.11781/sysydz202402238
    shu

    雷竞技app官方版下载ios-雷竞技官方平台

    doi: 10.11781/sysydz202402238
  • 臧素华

  • 中国石化 华东油气分公司 勘探开发研究院, 南京 210000

    • 基金项目: 

    国家科技重大专项 2017ZX05049-001-004

    中国石化科技部项目 P21112

    中国石化科技部项目 P23190

    中国石化科技部项目 P24117

    详细信息
    作者简介:

    臧素华(1985—)，男，硕士，副研究员，从事油气勘探部署与综合研究。E-mail: zangsh.hdsj@sinopec.com

  • 中图分类号: TE122.2

  • 文章访问数:  82
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  • PDF下载量:  20
  • 被引次数: 0
    • 出版历程
  • 收稿日期:  2023-05-14
  • 修回日期:  2024-02-03
  • 刊出日期:  2024-03-28

    • Reservoir characteristics and hydrocarbon accumulation significance of metamorphic zones of intrusive rocks and surrounding rocks in second member of Paleocene Funing Formation in Qintong Sag, Subei Basin

  • ZANG Suhua

  • Research Institute of Exploration and Development, SINOPEC East China Oil & Gas Company, Nanjing, Jiangsu 210000, China

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    • 雷竞技官方平台
  • 雷竞技官方平台: 火山岩油气藏是油气勘探的重要领域之一。苏北盆地溱潼凹陷侵入岩分布广泛，油气显示活跃，已成为我国东部陆相盆地油气深化勘探和规模增储的重要领域，具备良好的勘探前景。然而，目前针对火山岩对泥雷竞技app官方版下载ios围岩储层及其成藏影响的研究较为缺乏，泥雷竞技app官方版下载ios围岩变质带能否作为勘探重点领域有待深入评价。为了推动苏北盆地侵入岩围岩变质带新类型油藏勘探，以溱潼凹陷阜二段侵入岩围岩变质带为研究对象，综合岩心、薄片、全岩、测井等资料，系统揭示了泥雷竞技app官方版下载ios变质带储层特征，明确了岩浆侵入对阜二段变质带油气成藏的贡献。研究表明，溱潼凹陷阜二段泥雷竞技app官方版下载ios受岩浆侵入影响，泥雷竞技app官方版下载ios围岩发生蚀变形成环状变质带储层，岩浆的侵入具有明显“增储作用”；变质带储层发育孔隙、裂缝两类储集空间，储层发育程度受侵入岩厚度及烘烤强度控制，岩浆的侵入具有“催熟作用”，同等深度下泥雷竞技app官方版下载iosRo可增加0.4%~0.5%；阜宁组侵入岩形成于吴堡期—三垛期，火成岩侵入形成环状变质带的时间早于油气充注期，具有良好的成藏匹配关系。受岩浆侵入、侵入岩空间分布以及源储匹配关系控制，溱潼凹陷阜二段侵入岩围岩变质带具有源储一体、近源富集的特征，是规模增储的新阵地。

     

    关键词:
  • 储层特征 / 
  • 围岩变质带 / 
  • 阜宁组二段 / 
  • 古新统 / 
  • 溱潼凹陷 / 
  • 苏北盆地 
    • Abstract: Volcanic reservoirs play a crucial role in oil and gas exploration. The intrusive rocks in the Qintong Sag of the Subei Basin are widely distributed within active oil and gas deposits, making them a significant area for further exploration and reserve expansion in East China's continental basins. Despite the promising exploration prospects, there is a research gap regarding the impact of volcanics on shale surrounding rock reservoirs and their accumulation potential. It is essential to evaluate whether the shale metamorphic zones could serve as a key exploration target. This study focuses on the metamorphic zones of intrusive rocks and surrounding rocks in the Qintong Sag's second member of the Funing Formation. By integrating core, thin section, whole rock, and well logging data, this work systematically reveals the reservoir characteristics of the mud shale metamorphic zones and defines the contribution of magma intrusion to hydrocarbon accumulation in the metamorphic zones. The results indicate that magma intrusion alters the mud shale of the Funing Formation, resulting in a circular metamorphic zone reservoir with enhanced reservoir properties. This reservoir exhibits two types of spaces, pores and fractures, with development dependent on the thickness and intensity of intrusive rocks. Magma intrusion also leads to a "ripening effect", increasing the Ro of mud shale by 0.4%-0.5% at the same depth. The intrusive rocks of the Funing Formation were formed during the Wubao to Sanduo periods. The intrusion of igneous rocks created a circular metamorphic zone prior to the hydrocarbon charging stage, indicating a favorable accumulation match. Influenced by magma intrusion, spatial distribution of intrusive rocks, and the source-reservoir relationship, the metamorphic zones of intrusive rocks and surrounding rocks in the second member of Funing Formation in the Qintong Sag exhibit characteristics of integrated source-reservoir and near-source enrichment. This presents a new opportunity for significant reservoir enhancement on a large scale.

     

    Key words:
  • reservoir characteristic / 
  • metamorphic zone of surrounding rock / 
  • second member of Funing Formation / 
  • Paleocene / 
  • Qintong Sag / 
  • Subei Basin 
    • HTML全文

  • 图  1  苏北盆地溱潼凹陷区域构造(a)、地震剖面(b)及综合地层特征(b)

    Figure  1.  Regional structure(a), seismic profile(b) and comprehensive stratigraphic characteristics(c) of Qintong Sag, Subei Basin

    下载: 全尺寸图片 幻灯片

    图  2  苏北盆地溱潼凹陷SD1井古新统阜宁组二段侵入岩及围岩岩石学特征

    Figure  2.  Petrological characteristics of intrusive rocks and surrounding rocks of second member of Paleocene Funing Formation in well SD1 of Qintong Sag, Subei Basin

    下载: 全尺寸图片 幻灯片

    图  3  苏北盆地溱潼凹陷古新统阜宁组二段侵入岩围岩储集空间特征

    Figure  3.  Reservoir space characteristics of intrusive rocks and surrounding rocks of second member of Paleocene Funing Formation in Qintong Sag, Subei Basin

    下载: 全尺寸图片 幻灯片

    图  4  苏北盆地溱潼凹陷古新统阜宁组二段泥雷竞技app官方版下载ios变质带储层物性

    Figure  4.  Physical properties of reservoirs in mud shale metamorphic zone of second member of Paleocene Funing Formation in Qintong Sag, Subei Basin

    下载: 全尺寸图片 幻灯片

    图  5  苏北盆地溱潼凹陷沙垛地区古新统阜宁组二段不同岩性测井响应特征

    Figure  5.  Relationship of response characteristics of different lithologies in second member of Paleocene Funing Formation in Shaduo area of Qintong Sag, Subei Basin

    下载: 全尺寸图片 幻灯片

    图  6  苏北盆地溱潼凹陷SD1井古新统阜宁组二段综合柱状图

    Figure  6.  Comprehensive histogram of second member of Paleocene Funing Formation in well SD1 of Qintong Sag, Subei Basin

    下载: 全尺寸图片 幻灯片

    图  7  苏北盆地溱潼凹陷SD1井锆石年龄谐和图

    Figure  7.  Zircon age harmony diagram of well SD1 in Qintong Sag, Subei Basin

    下载: 全尺寸图片 幻灯片

    图  8  苏北盆地溱潼凹陷阜宁组侵入岩与变质带储层厚度、孔隙度相关性

    Figure  8.  Correlation between reservoir thickness and porosity of intrusive rocks and metamorphic zones in Funing Formation, Qintong Sag, Suibei Basin

    下载: 全尺寸图片 幻灯片

    图  9  苏北盆地溱潼凹陷火山岩相关油藏成藏模式

    Figure  9.  Accumulation model of volcanic-related oil reservoirs in Qintong Sag, Subei Basin

    下载: 全尺寸图片 幻灯片

    表  1  苏北盆地溱潼凹陷SD1井古新统阜宁组二段侵入岩上变质带—泥雷竞技app官方版下载ios主量元素统计

    Table  1.   Statistics of principal elements of mud shale in metamorphic zone of intrusive rocks of second member of paleocene Funing Formation, well SD1, Qintong Sag, Subei Basin %

    样品深度(岩性)
    SiO2
    TiO2
    Al2O3
    Fe2O3
    MnO
    MgO
    CaO
    Na2O
    K2O
    P2O5
    LOI
    3 520 m(正常泥雷竞技app官方版下载ios)
    65.79
    0.235
    6.79
    3.28
    0.190
    1.12
    9.56
    0.77
    0.82
    0.138
    12.23
    3 522 m(正常泥雷竞技app官方版下载ios)
    49.95
    0.421
    9.92
    3.91
    0.123
    2.83
    13.95
    1.83
    1.31
    0.164
    14.32
    3 545 m(蚀变泥雷竞技app官方版下载ios)
    58.03
    0.742
    16.84
    7.11
    0.000
    0.11
    1.63
    9.24
    2.58
    0.127
    3.59
    3 546 m(蚀变泥雷竞技app官方版下载ios)
    59.64
    0.458
    12.72
    5.57
    0.121
    3.08
    9.00
    7.43
    1.14
    0.150
    0.79
    3 546.6 m(蚀变泥雷竞技app官方版下载ios)
    45.48
    0.227
    15.47
    3.16
    0.210
    3.74
    26.77
    0.28
    0.02
    0.236
    4.70
    下载: 导出CSV

    表  2  苏北盆地溱潼凹陷SD1井侵入岩—变质带—正常泥雷竞技app官方版下载ios碳、氧同位素分析结果

    Table  2.   C and O isotopes of intrusive rock, metamorphic zone and normal mud shale in well SD1 in Qintong Sag, Subei Basin

    样品深度/m
    矿物
    δ18OSMOW/‰
    δ13CVPDB/‰
    备注
    3 520.0
    泥雷竞技app官方版下载ios中方解石
    19.70
    0.18
    正常泥雷竞技app官方版下载ios
    3 522.0
    泥雷竞技app官方版下载ios中方解石
    20.09
    0.02
    正常泥雷竞技app官方版下载ios
    3 546.6
    蚀变泥雷竞技app官方版下载ios中方解石
    17.57
    -16.66
    上蚀变带
    3 550.2
    辉绿岩中方解石
    16.04
    -13.37
    辉绿岩
    3 587.8
    橄榄辉长岩中方解石
    15.78
    -13.20
    辉绿岩
    3 595.5
    橄榄辉长岩中方解石
    17.03
    -14.55
    辉绿岩
    3 618.4
    热变质泥岩中方解石
    19.79
    -15.72
    下蚀变带
    下载: 导出CSV
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