岩性油气藏 ›› 2026, Vol. 38 ›› Issue (4): 115–125.doi: 10.12108/yxyqc.20260410

• 地质勘探 • 上一篇    下一篇

塔中地区奥陶系良里塔格组碳酸盐岩储层油气充注期次及成藏模式

孙阳珍1(), 杨鹏1(), 贾坤1, 秦舒欣2, 刘可禹1   

  1. 1 中国石油大学（华东） 深层油气全国重点实验室， 山东 青岛 266580
    2 中国石油长庆油田分公司 第三采油厂， 宁夏 银川 750006
  • 收稿日期:2025-11-12 修回日期:2026-01-04 出版日期:2026-07-01 发布日期:2026-07-06
  • 第一作者:孙阳珍（2001—），女，中国石油大学（华东）在读硕士研究生，研究方向为流体包裹体与油气成藏。地址:（266580）山东省青岛市黄岛区长江西路66号。Email:18953029481@163.com。
  • 通信作者: 杨鹏
  • 基金资助:
    国家自然科学基金项目“沉积盆地超深层碳酸盐矿物中流体包裹体保存温压上限定量研究：以塔里木盆地顺北油田为例”(42402141);山东省自然科学基金项目“塔里木盆地塔北地区超深层液态烃稳定性控制因素及保存下限研究”(ZR2023QD006);中国石油天然气股份有限公司西南油气田分公司勘探开发研究院项目“川中古隆起蓬莱气田震旦系深层-超深层天然气成藏模式研究”(XNS勘研院JS2024-146)

Oil and gas charging episodes and reservoir formation models of Ordovician Lianglitage Formation carbonate rocks in Tazhong area

SUN Yangzhen1(), YANG Peng1(), JIA Kun1, QIN Shuxin2, LIU Keyu1   

  1. 1 State Key Laboratory of Deep Oil and Gas， China University of Petroleum （East China）， Qingdao 266580, Shandong， China
    2 No.3 Oil Production Plant， PetroChina Changqing Oilfield Company， Yinchuan 750006， Ningxia， China
  • Received:2025-11-12 Revised:2026-01-04 Online:2026-07-01 Published:2026-07-06
  • Contact: YANG Peng E-mail:18953029481@163.com;yangpeng@upc.edu.cn

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摘要：

综合采用原位方解石U-Pb定年、流体包裹体分析及盆地模拟等技术方法，对塔中地区奥陶系良里塔格组的岩石学、流体活动特征进行了厘定，系统分析了油气充注期次，并刻画了其成藏模式。研究结果表明：①塔中地区奥陶系良里塔格组储层主要岩石类型为颗粒灰岩和生物灰岩，储集空间类型包括孔隙、溶洞以及裂缝等。②储层中主要发育2期方解石胶结物，其中第1期方解石胶结物发亮红色阴极光，对应的U-Pb年龄为427.0 ± 4.2 Ma，第2期方解石胶结物发橘黄色阴极光，对应的U-Pb年龄为369.0 ± 14.0 Ma。③储层中主要发育2类石油包裹体组合，第1类石油包裹体组合发黄色、淡黄色荧光，对应的油气充注时间为425.0~410.0 Ma；第2类石油包裹体组合发蓝色荧光，对应的油气充注年龄325.0~320.0 Ma。④研究区良里塔格组储层主要经历2期石油和1期天然气充注，其中第1期石油充注事件发生在加里东晚期，第2期石油充注事件发生在海西中期，天然气充注发生在喜山晚期；该套油气藏的形成是优质储层、多期供烃、高效输导、有效封盖与有利构造背景等多因素协同作用的结果。

关键词: 油气充注期次, 碳酸盐岩, 流体包裹体PVT模拟, U-Pb定年, 良里塔格组, 奥陶系, 塔中地区

Abstract:

Based on in-situ calcite U-Pb dating, fluid inclusion analysis, and basin modelling, the petrological and fluid activity characteristics of Ordovician Lianglitage Formation in Tazhong area were delineated. The oil and gas charging episodes were systematically analyzed, and reservoir formation models were characterized. Research results show that: （1） Main rock types of Ordovician Lianglitage Formation reservoir in Tazhong area are granular limestone and biogenic limestone, and storage space types include pores, karst caves, and fractures. （2） Two phases of calcite cements develop in the reservoir, with the first phase of calcite cement emitting bright red catho-doluminescence light, and the corresponding U-Pb age of 427.0 ± 4.2 Ma, and the second phase of calcite cement displaying orange-yellow cathodoluminescence light, and the corresponding U-Pb age of 369.0 ± 14.0 Ma. (3) Two types of oil inclusion assemblages (OIA) have been identified. Type I OIA emits yellow and pale yellow fluorescence, corresponding to the oil charge timing of 425.0-410.0 Ma. Type Ⅱ OIA emits blue fluorescence, corresponding to the oil charge timing of 325.0-320.0 Ma. (4) Lianglitage Formation reservoir in the study area has mainly experienced two episodes of oil charging and one episode of natural gas charging. The first episode of oil charging occurred in the late Caledonian period, the second episode of oil charging occurred in the middle Hercynian period, and the natural gas charging occurred in the late Himalayan period. The formation of this oil and gas reservoir is the result of synergistic effects of multiple factors, including high-quality reservoirs, multi-stage hydrocarbon supply, efficient transportation, effective sealing, and favorable structural backgrounds.

Key words: oil and gas charging episodes, carbonate rock, fluid inclusion PVT modelling, U-Pb dating, Liang-litage Formation, Ordovician, Tazhong area

中图分类号: 

  • TE122.1

图1

塔里木盆地塔中构造位置（a）及岩性地层综合柱状图（b）（据文献[17]修改）"

图2

塔中地区奥陶系碳酸盐岩储层微观特征"

图3

塔中地区奥陶系良里塔格组碳酸盐岩样品中方解石脉体显微照片"

图4

塔中地区TZ243井奥陶系良里塔格组碳酸盐岩样品方解石胶结物的U-Pb同位素年龄"

图5

塔中地区奥陶系奥陶系良里塔格组方解石脉体中油包裹体显微照片"

图6

塔中地区奥陶系良里塔格组油包裹体荧光光谱（a）及光谱参数特征（b）"

图7

塔中地区奥陶系良里塔格组2类油包裹体气体充填度特征"

图8

塔中地区奥陶系良里塔格组油包裹体伴生盐水包裹体激光拉曼光谱特征"

图9

塔中地区奥陶系良里塔格组流体包裹体显微测温特征"

表1

塔中地区奥陶系良里塔格组储集层流体包裹体显微测温数据"

井号 类型 油包裹体Th/℃ 伴生盐水
包裹体Th/℃		 伴生盐水
包裹体Tm/℃		 盐度/%
TZ243 Ⅰ类 68.8~90.1 76.8~100.2 -2.0~-3.9 3.4~6.3
Ⅱ类 88.0~110.0 96.5~120.0 -7.8~8.3 11.4~12.1
TZ242 Ⅱ类 78.8~105.0 88.1~110.0 -8.0~9.8 11.6~13.7
TZ825 Ⅰ类 69.0~90.1 78.1~100.0 -2.0~-4.0 3.4~6.4

图10

塔中地区奥陶系良里塔格组典型井埋藏史和热史及其地层温度-镜质体反射率校正关系"

图11

塔中地区奥陶系良里塔格组2类石油包裹体及伴生盐水包裹体PVT模拟结果"

图12

塔中地区奥陶系良里塔格组含油气系统综合图（据文献[22]修改）"

图13

塔中地区奥陶系良里塔格组多期油气充注模式（据文献[28]修改）"

图14

塔中地区奥陶系良里塔格组油气成藏模式（据文献[36]修改）"

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