岩性油气藏 ›› 2026, Vol. 38 ›› Issue (5): 71–82.doi: 10.12108/yxyqc.20260507

• 地质勘探 • 上一篇    下一篇

四川盆地中部中三叠统雷口坡组一段沉积特征及有利储层分布

青春1(), 吴学妍2(), 唐松1, 刘博文1, 淦文杰1, 余燕1, 梁新玉1, 廖月1   

  1. 1 中国石油西南油气田公司 川中油气矿四川 遂宁 629000
    2 西南石油大学 地球科学与技术学院成都 610500
  • 收稿日期:2026-03-30 修回日期:2026-04-29 出版日期:2026-09-01 发布日期:2026-09-04
  • 第一作者:青春(1971—),男,高级工程师,主要从事天然气开发方面的研究管理工作。地址:(629000)遂宁市河东新区香林南路178号。 Email:qingchun@petrochina.com.cn
  • 通信作者: 吴学妍
  • 基金资助:
    新型油气勘探开发国家科技重大专项“四川盆地全油气系统与新领域勘探技术”(2025ZD1400403);国家自然基金(面上项目)“海相白云岩与蒸发岩共生组合形成机制研究:以四川盆地雷口坡组为例”(42572194)

Sedimentary characteristics and favorable reservoirs distribution of the first member of Leikoupo Formation in Middle Triassic, central Sichuan Basin

QING Chun1(), WU Xueyan2(), TANG Song1, LIU Bowen1, GAN Wenjie1, YU Yan1, LIANG Xinyu1, LIAO Yue1   

  1. 1 Central Sichuan Oil and Gas DistrictPetroChina Southwest Oil & Gasfield CompanySuining 629000, Sichuan, China
    2 School of Geoscience and TechnologySouthwest Petroleum UniversityChengdu 610500, China
  • Received:2026-03-30 Revised:2026-04-29 Online:2026-09-01 Published:2026-09-04
  • Contact: WU Xueyan E-mail:qingchun@petrochina.com.cn;15913269101@163.com

摘要:

综合岩心观察、薄片鉴定、测井相分析,制定了川中地区中三叠统雷口坡组一段(雷一段)的沉积相划分方案;通过连井剖面对比,对沉积相展布及演化规律进行了系统剖析;基于常规、非常规油气双领域视角,划分了有利储集区带。研究结果表明:①川中地区雷一段主要发育蒸发台地与局限台地,进一步划分为蒸发潮坪、局限潮坪、台内滩3个亚相及膏坪、膏云坪、云坪、灰坪、泥云坪、颗粒滩6个微相。②研究区沉积演化受古构造、古地貌与海平面变化协同控制,具有“早期滩坪发育、晚期蒸发增强”的阶段性沉积演化序列,雷一1亚段沉积期,盆地西高东低、海平面相对较高,发育局限台地云坪与颗粒滩沉积;雷一2亚段沉积期,气候干旱、海平面下降,膏云坪广泛发育,陆源泥质输入增多,沉积体系演化为蒸发岩为主的咸化沉积体系,构成海退序列。③研究区储层特征存在明显分层差异,雷一1亚段以颗粒滩和云坪相控常规储层为主,储集岩性为颗粒白云岩与晶粒白云岩,经准同生期暴露、早期岩溶及白云石化作用叠加改造而形成优质储层;雷一2亚段发育泥质白云岩非常规储层,具有“源-储一体”的成藏优势,顶底板受膏岩层封堵,构成密闭型成藏系统。④磨溪地区为颗粒滩相最有利发育区,川中西部—南部为云坪相有利储集分布区,蓬阳地区为泥云坪相非常规油气“甜点”区。

关键词: 沉积相, 颗粒滩相, 非常规油气, “甜点”预测, 局限台地相, 测井相, 雷口坡组一段, 中三叠统, 川中地区

Abstract:

Based on core observation, thin section identification, and logging facies analysis, a sedimentary facies classification scheme for the first member of Leikoupo Formation(Lei 1 Member)in Middle Triassic of central Sichuan Basin was established. Through cross-well profiles correlation, the distribution and evolution of sedimentary facies are systermatically analyzed. From dual perspectives of conventional and unconventional oil and gas fields, favorable reservoir zones were delineated. The results show that:(1) Lei 1 Member in central Sichuan Basin mainly develops evaporative platform and restricted platform,which can be further divided into three subfacies (evaporative tidal flat, restricted tidal flat, and intra-platform shoal) and six microfacies (gypsum flat, gypsiferous dolomite flat, dolomite flat, limestone flat, argillaceous dolomite flat, and grain shoal). (2) Sedimentary evolution of the study area was jointly controlled by paleostructure, paleogeomorphology, and sea level changes, exhi-biting the staged sedimentary evolution sequence of “shoal and flat developed in the early stage, and evaporation enhanced in the late stage”. During the deposition of Lei 11 submember, the basin was characterized by a topography of “high west and low east” with a relatively high sea level, developing dolomite flats and grain shoals in a restricted platform setting. During the deposition of Lei 12 submember, the climate turned arid and sea level fell, leading to widespread gypsiferous dolomite flats, increased terrestrial argillaceous material input. The depositional system evolved into an evaporite‑dominated saline system, constituting a regressive sequence. (3) Reservoir characteristics in the study area show obvious stratification differences. Lei 11 submember is dominated by facies‑ controlled conventional reservoirs of grain shoals and dolomite flats, with reser-voir lithologies consisting of grain dolostone and crystalline dolostone, which were transformed into high‑quality reservoirs through penecontemporaneous exposure, early karstification, and dolomitization. Lei 12 submember features “source‑reservoir integrated” unconventional argillaceous dolomite reservoirs, with the top and bottom sealed by gypsum layers, forming a closed hydrocarbon accumulation system. (4) Moxi area is the most favorable zone for grain shoal facies. The west and south parts of central Sichuan Basin are favorable for dolomite flat facies, and Pengyang area is the “sweet spot” for unconventional exploration of argillaceous dolomite flats.

Key words: sedimentary facies, grain shoal facies, unconventional oil and gas, “sweet spot” prediction, restri-cted platform facies, logging facies, the first member of Leikoupo Formation, Middle Triassic, central Sichuan Basin

中图分类号: 

  • TE121.3

图1

四川盆地中部地区构造位置(a)和中三叠统雷口坡组岩性地层综合柱状图(b)(据文献[13,22]修改)"

图2

四川盆地中部中三叠统雷口坡组一段主要岩石类型宏观和微观照片 (a) 灰白色晶粒白云岩,华探1井,4 217.21~4 217.55 m,岩心照片;(b) 泥—细粉晶白云岩,磨4井,2 752.69 m,铸体薄片,单偏光;(c) 纹层状泥质白云岩,华探1井,4 203.08~4 203.23 m,岩心照片;(d) 泥质白云岩,充探1井,4 090.00 m,普通薄片,单偏光;(e)灰 色砂屑白云岩,充探1井,4 028.54~4 028.73 m,岩心照片;(f) 砂屑白云岩,磨溪22井,3 132.00 m,铸体薄片,单偏光;(g) 粉晶灰岩,兴华1井,3 290.97~3 291.30 m,岩心照片;(h) 泥晶灰岩,兴华1井,3 291.00 m,普通薄片,单偏光;(i) 膏岩,鸡笼铁丝构造,广元宝轮石灰窑剖面;(j) 膏岩,磨溪4井,2 785.21 m,铸体薄片,正交偏光;(k) 膏质白云岩,兴华1井,3 312.63~3 314.14 m,岩心照片;(l) 云质膏岩,磨溪22井,3 002.00 m,铸体薄片,正交偏光。"

图3

四川盆地中部中三叠统雷口坡组一段测井相类型与特征"

表1

四川盆地中部中三叠统雷口坡组一段沉积相类型划分"

沉积体系 亚相 微相 主要岩性
碳酸盐岩
台地
蒸发
台地
蒸发
潮坪
膏云坪 膏质白云岩、膏岩与白云岩、
泥质白云岩互层
膏坪 膏岩、云质膏岩
局限
台地
局限
潮坪
云坪 泥—粉晶白云岩、结晶白云岩
灰坪 泥—粉晶灰岩
台内滩 泥云坪 泥质白云岩、含泥白云岩
颗粒滩 砂屑白云岩、鲕粒白云岩

图4

川中地区北东—南东向三叠统雷一1亚段沉积相连井剖面对比(剖面位置见图1a)"

图5

川中地区西—南部三叠统雷一1亚段沉积相连井剖面对比(剖面位置见图1a)"

图6

川中地区北东—南东向三叠统雷一2亚段沉积相连井剖面对比(剖面位置见图1a)"

图7

川中地区西—南部中三叠统雷一2亚段沉积相连井剖面对比(剖面位置见图1a)"

图8

四川盆地中部中三叠统雷一1亚段沉积相平面展布"

图9

四川盆地中部中三叠统雷一2亚段沉积相平面展布"

图10

四川盆地中部中三叠统雷一段沉积模式"

图11

四川盆地中部中三叠统雷一1亚段储层物性特征 注:N为研究区所取样品数量,个;K为渗透率,mD;ϕ为孔隙度,%。"

图12

四川盆地中部中三叠统雷口坡组一段有利储集区带预测"

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