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四川盆地中二叠世岩相古地理及其油气地质意义

彭金宁 杜崇娇 李龙龙 蒋小琼 潘文蕾 陆永德 罗开平

彭金宁, 杜崇娇, 李龙龙, 蒋小琼, 潘文蕾, 陆永德, 罗开平. 四川盆地中二叠世岩相古地理及其油气地质意义[J]. 石油实验地质, 2023, 45(1): 49-59. doi: 10.11781/sysydz202301049
引用本文: 彭金宁, 杜崇娇, 李龙龙, 蒋小琼, 潘文蕾, 陆永德, 罗开平. 四川盆地中二叠世岩相古地理及其油气地质意义[J]. 石油实验地质, 2023, 45(1): 49-59. doi: 10.11781/sysydz202301049
PENG Jinning, DU Chongjiao, LI Longlong, JIANG Xiaoqiong, PAN Wenlei, LU Yongde, LUO Kaiping. Lithofacies palaeogeography of Middle Permian in the Sichuan Basin and its petroleum geological significance[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2023, 45(1): 49-59. doi: 10.11781/sysydz202301049
Citation: PENG Jinning, DU Chongjiao, LI Longlong, JIANG Xiaoqiong, PAN Wenlei, LU Yongde, LUO Kaiping. Lithofacies palaeogeography of Middle Permian in the Sichuan Basin and its petroleum geological significance[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2023, 45(1): 49-59. doi: 10.11781/sysydz202301049

四川盆地中二叠世岩相古地理及其油气地质意义

doi: 10.11781/sysydz202301049
基金项目: 

中国石油化工股份有限公司项目“川西二叠系成藏条件及勘探潜力分析” P18069-2

详细信息
    作者简介:

    彭金宁(1979-), 男, 博士, 高级工程师, 从事油气地质综合评价研究。E-mail: pengjn.syky@sinopec.com

  • 中图分类号: TE121.3

Lithofacies palaeogeography of Middle Permian in the Sichuan Basin and its petroleum geological significance

  • 摘要: 近期四川盆地中二叠统陆续取得勘探发现,展现出很大的勘探潜力。中二叠世该区构造—沉积分异明显,导致油气成藏规律复杂,层序岩相古地理的重建对认识构造—沉积演化、沉积建造和油气勘探具有重要意义。通过综合油气勘探成果、典型钻井及野外露头资料,并以三级层序为最小纵向编图单元,重建了四川盆地中二叠世栖霞—茅口期各层序的岩相古地理。四川盆地中二叠统可划分为5个三级层序,即SQq1(梁山组—栖一段B)、SQq2(栖一段A—栖二段)、SQm1(茅一段—茅二段C)、SQm2(茅二段B—A)和SQm3(茅三—茅四段)。SQq1和SQm1沉积期总体以海侵和填平补齐过程为主,盆内局部古高地存在点状、带状滩体;SQq2、SQm2和SQm3沉积期以持续海退、地貌分异为主,盆缘发育镶边的碳酸盐岩台地沉积体系,台内可形成较大规模多个滩体;SQq2沉积期是中二叠世主要成滩期,较漫长的海退过程和局部块体升降,促使川西台缘、川中南部台内形成较大规模多个滩体;SQm3沉积期在盆地北部沉积分异明显加剧,全面转换为台缘—斜坡—陆棚的隆凹相间沉积分异格局;SQq2和SQm3沉积期高位体系域(HST)的台缘、台内滩体为白云石化、溶蚀等后期建设性成岩改造提供了物质基础。坡折带地貌的刻画和台缘、台内滩体预测应成为下一步勘探研究的重点。

     

  • 图  1  四川盆地中二叠统层序地层划分方案

    Figure  1.  Sequence stratigraphic division of Middle Permian, Sichuan Basin

    图  2  四川盆地下二叠统梁山组岩电响应特征

    Figure  2.  Rock electrical response characteristics of Lower Permian Liangshan Formation, Sichuan Basin

    图  3  四川盆地SQq1和SQq2层序野外露头和镜下特征

    a.P1l和P2q界面,旺苍金龙村剖面;b.P1l和P2q界面,华蓥二崖剖面;c.P2q1B,薄层状微晶生物碎屑灰岩夹硅质结核(A),华蓥二崖剖面;d.中—厚层状微晶生物碎屑灰岩,P2q1A,剑阁猫儿塘剖面;e.微晶生物碎屑灰岩,照片d镜下显微照片,单偏光;f.厚层状白云岩,P2q2,剑阁何家梁剖面;g.细—粗晶白云岩,照片f镜下显微照片;h.豹斑灰岩(A为灰质白云岩,B为白云质灰岩),P2q2,旺苍鹿渡坝剖面;i.P2q1B和P2q2界面,旺苍鹿渡坝剖面

    Figure  3.  Outcrop and microscopic characteristics of SQq1 and SQq2 sequences, Sichuan Basin

    图  4  四川盆地中二叠统茅口组SQm1、SQm2和SQm3层序野外露头和镜下特征

    a.P2q和P2m界面,綦江藻渡剖面[26];b.P2q和P2m界面,广元西北乡剖面;c.P2m1,“眼球眼皮”状灰岩(A为眼球,B为眼皮),广元西北乡剖面;d.P2m2(A为燧石条带),剑阁马儿岩剖面;e.P2m2,灰白色厚层状生物碎屑微晶灰岩,茂县燕子岩剖面;f.图片e镜下显微照片,单偏光;g.P2m3,深灰色薄—中层状含生物碎屑微晶灰岩,城口渡口剖面;h.图片g镜下显微照片,单偏光;i.广元车家坝剖面(A为茅口组硅质岩,B为吴家坪组王坡页岩,C为吴家坪组灰岩)[26];j.YDD3井岩心(A为茅口组灰岩,B为风化壳,C为玄武岩)[26];k.绵阳千佛镇剖面(A为茅口组灰岩,B为玄武岩,C为吴家坪组灰岩);l. P2m4,中—厚层状微晶生物碎屑灰岩,茂县燕子岩剖面

    Figure  4.  Outcrop and microscopic characteristics of SQm1, SQm2 and SQm3 sequences, Sichuan Basin

    图  5  四川盆地中二叠世层序—岩相古地理分布

    Figure  5.  Sequence-lithofacies palaeogeography of Middle Permian, Sichuan Basin

    图  6  四川盆地及周缘中二叠统滩相白云岩储层特征

    a.HS1井SQq2,白云岩中可见溶孔、溶洞发育;b.HS1井SQq2,中粗晶白云岩中可见晶间孔发育;c.广元长江沟SQq2,中粗晶白云岩中见溶洞发育;d.MX108井SQq2,中晶白云岩晶间孔发育

    Figure  6.  Characteristics of Middle Permian beach facies dolomite reservoirs in Sichuan Basin and its periphery

    图  7  四川盆地中二叠统SQm3沉积分异模式

    a.YB8井SQm3,生屑灰岩;b.YB7井SQm3,亮晶生屑灰岩;c.旺苍正源SQm3,泥页岩发育;d.旺苍正源SQm3,硅质岩

    Figure  7.  Sedimentary differentiation model of Middle Permian SQm3 sequence, Sichuan Basin

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出版历程
  • 收稿日期:  2022-02-15
  • 修回日期:  2022-11-15
  • 刊出日期:  2023-01-28

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