岩性油气藏 ›› 2022, Vol. 34 ›› Issue (2): 17–30.doi: 10.12108/yxyqc.20220202

• 地质勘探 • 上一篇    下一篇

塔里木盆地顺北一区奥陶系鹰山组与一间房组沉积特征

彭军1,2, 夏梦1, 曹飞3, 夏金刚1, 李峰3   

  1. 1. 西南石油大学 地球科学与技术学院, 成都 610500;
    2. 天然气地质四川省重点实验室, 成都 610500;
    3. 中国石化西北油田分公司 勘探开发研究院, 乌鲁木齐 830000
  • 收稿日期:2021-12-06 修回日期:2021-12-23 出版日期:2022-03-01 发布日期:2022-03-14
  • 第一作者:彭军(1968-),男,博士,教授,博士生导师,主要从事沉积学、储层地质学及层序地层学方面的教学和研究工作。地址:(610500)四川省成都市新都区新都大道8号。Email:445371976@qq.com
  • 通信作者: 夏梦(1995-),女,西南石油大学在读硕士研究生,研究方向为沉积学。Email:593098239@qq.com。
  • 基金资助:
    四川省科技厅区域创新合作项目“复杂油藏高效开发相关技术研究及推广应用”（编号：2021YFQ0048）资助

Sedimentary characteristics of Ordovician Yingshan Formation and Yijianfang Formation in Shunbei-1 area, Tarim Basin

PENG Jun1,2, XIA Meng1, CAO Fei3, XIA Jingang1, LI Feng3   

  1. 1. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China;
    2. Sichuan Key Laboratory of Natural Gas Geology, Chengdu 610500, China;
    3. E Research Institute of Exploration and Development, Sinopec Northwest Oilfield Branch, Urumqi 830000, China
  • Received:2021-12-06 Revised:2021-12-23 Online:2022-03-01 Published:2022-03-14

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摘要： 近年来，塔里木盆地顺北地区油气藏的持续发现揭示了其较大的勘探潜力。通过开展岩心观察、薄片鉴定、常规测井曲线和成像测井图像分析以及元素地球化学测试，对顺北一区奥陶系鹰山组上段与一间房组沉积环境进行了分析，结合沉积相识别标志，系统描述了研究区沉积特征，指明了优质储层类型及有利发育区。研究结果表明：①顺北一区奥陶系鹰山组上段与一间房组Mn的质量分数大于200×10-6，Sr/Ba平均值为2.025 4~3.260 2，U/Th平均值为2.02，多大于0.75，δU平均值为1.29，多大于1，显示沉积时整体处于水体由深变浅、盐度正常、温暖潮湿的弱氧化-弱还原的海相沉积环境。②研究区奥陶系鹰山组上段与一间房组为开阔台地相沉积，发育台坪和台内滩2种亚相，可细分为灰坪、云灰坪、云坪、砂屑滩、生屑滩、颗粒滩等6个微相。③研究区整体以灰坪微相为主，纵向上一间房组砂屑滩与生屑滩微相较鹰山组上段更为发育，平面上自东向西台内滩亚相发育减弱。

关键词: 开阔台地, 海相, 鹰山组上段, 一间房组, 奥陶系, 顺北一区, 塔里木盆地

Abstract: In recent years, the continuous discovery of oil and gas reservoirs in Shunbei area of Tarim Basin reveals its great exploration potential.Through core observation, thin section identification, conventional logging curves and imaging logging image analysis and element geochemistry test, the sedimentary environment of the upper member of Yingshan Formation and Yijianfang Formation of Ordovician(O1-2y-O2yj) in Shunbei-1 area was analyzed. Combined with the identification marks of sedimentary facies, the sedimentary characteristics of the study area were described, and the high-quality reservoir types and favorable reservoir development areas were pointed out. The results show that:(1) The mass fraction of Mn of the upper member of Yingshan Formation and Yijianfang Formation of Ordovician in Shunbei-1 area 1 is greater than 200×10-6, the average value of Sr/BA is 2.025 4-3.260 2, and the average value of U/Th is 2.02, mostly greater than 0.75, the average value of δU is 1.29, mostly greater than 1, which shows that the whole study area was in a marine sedimentary environment with water depth changing from deep to shallow, normal salinity, warm and humid weak oxidation-weak reduction.(2) The upper member of Yingshan Formation and Yijianfang Formation of Ordovician in the study area is an open platform facies deposit, with two subfacies developed:platform flat and intra-platform shoal, and six microfacies, such as limestone flat, dolomite-limestone flat, dolomite flat, sandy debris shoal, bioclastic shoal and granular beach.(3) As a whole, the study area is mainly dominated by limestone flat microfacies.In the vertical direction, the sandy debris shoal and bioclastic shoal microfacies are more developed in Yijianfang Formation than in the upper member of Yingshan Formation.The development of intra-platform shoal subfacies is weakened from east to west in the plane.

Key words: open platform, marine, upper member of Yingshan Formation, Yijianfang Formation, Ordovician, Shunbei-1 area, Tarim Basin

中图分类号: 

  • TE122
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