录井工程 ›› 2020, Vol. 31 ›› Issue (1): 120-124.doi: 10.3969/j.issn.1672-9803.2020.01.022

• 地质研究 • 上一篇    下一篇

松辽盆地中央古隆起带(北部)基底岩性识别方法

张晏奇①,②, 罗光东, 李义   

  1. ①中国石油大庆钻探工程公司地质录井一公司;
    ②吉林大学地球科学学院
  • 修回日期:2019-11-22 出版日期:2020-03-25 发布日期:2020-04-13
  • 作者简介:张晏奇 工程师,1983年生,毕业于大庆石油学院地质工程专业,吉林大学岩石矿物矿床学在读博士,现在大庆钻探工程公司地质录井一公司从事地质综合研究工作。通信地址:163000 黑龙江省大庆市让胡路区地质录井一公司地质研究中心。电话:(0459)5696230。E-mail:yqzhang14@mails.lju.edu.cn

Identification method of basement lithology in the central paleo-uplift belt(north) of Songliao basin

ZHANG Yanqi①,②, LUO Guangdong, LI Yi   

  1. ①No.1 Mud Logging Company of Daqing Drilling & Exploration Engineering Corporation, Daqing, Heilongjiang 163000, China;
    ②College of Earth Science, Jilin University, Changchun, Jilin 130061 China
  • Revised:2019-11-22 Online:2020-03-25 Published:2020-04-13

摘要: 松辽盆地中央隆起带(北部)具有良好的天然气成藏条件,是近年来天然气风险勘探的重要领域之一。由于已钻井少,地层揭示厚度薄等原因,目前对该区域特殊岩性、地层特征等认识不清。为此,综合已钻井岩屑镜下观察、XRF元素分析、岩屑薄片分析等资料,在大量数据分析和地质研究的基础上,总结松辽盆地古中央隆起带(北部)岩性特征,归纳得出了几点认识:一是松辽盆地基底构造特征复杂,多期构造运动形成了复杂的岩性,确定变质砂砾岩+板岩+千枚岩+片岩、花岗岩+闪长岩以及碎裂化+糜棱化花岗岩三组基底岩石序列;二是古中央隆起带基底长期暴露于地表,顶部风化壳发育网状裂缝,氧化特征明显,风化指数指示明显;三是通过元素组成判断变质岩原岩成分可靠程度高。利用这几点认识指导现场,能有效增强现场岩性识别的及时性、准确性,为松辽盆地古中央隆起带基底的滚动勘探与研究提供重要地质资料。

关键词: 松辽盆地, 古中央隆起带, 特殊岩性, 基底, 网状裂缝, XRF元素分析

Abstract: The central uplift belt(north) of Songliao basin has good natural gas accumulation conditions and is one of the important areas of natural gas rick exploration in recent years. Due to the lack of drilled wells and thin drilled strata, the special lithology and stratigraphic characteristics of the area are currently unknown. To this end, based on the microscope observation of cuttings, XRF element analysis and cuttings thin section analysis and other data of drilled wells, on the basis of a large amount of data analysis and geological research, the lithologic characteristics of central paleo-uplift belt(north) in Songliao basin was summarized. A couple of understandings were drawn. First, the basement structure of Songliao basin is complex, and complex lithology was formed after multistage tectonic movement. Three groups of basement rock sequence were determined, which are metamorphic glutenite+slate+phyllite+schist, granite+diorite, and fragmentation+mylonization granite. Second, the basement of central paleo-uplift belt has been exposed to the surface for a long time. Map cracking is developed on the top weathering crust with obvious oxidation characteristics and weathering index indication. Third, the element composition is highly reliable in determining country rock component of the metamorphic rock. Guiding the site through these understandings can effectively enhance the timeliness and accuracy of lithologic discrimination on site and provide important geological data for the rolling exploration and research of the basement of central paleo-uplift belt in Songliao basin.

Key words: Songliao basin, central paleo-uplift belt, special lithology, basement, map cracking, XRF element analysis

中图分类号: 

  • TE132.1
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