火山岩气藏

松辽盆地营城组火山岩相发育特征——以吉林省九台地区野外露头为例

  • 沈艳杰 ,
  • 李钧如 ,
  • 张立亚 ,
  • 周洋 ,
  • 程日辉
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  • 1.吉林大学地球科学学院,吉林 长春130061
    2.中国石化东北油气分公司,吉林 长春 130062
    3.沈阳市皇姑区创新发展研究中心,辽宁 沈阳 110031
沈艳杰(1981—),女,博士,副教授,主要从事石油地质勘探、火山沉积学和沉积矿床的研究工作。地址:吉林省长春市朝阳区西民主大街6号,邮政编码:130061。E-mail:shenyj@jlu.edu.cn

收稿日期: 2023-12-05

  网络出版日期: 2024-05-07

基金资助

国家自然科学基金项目“松辽盆地营城组火山物质分散-堆积及古火山机构重建”(41602106)

Volcanic facies development characteristics of Yingcheng Formation in Songliao Basin: A case study of field outcrops in Jiutai area of Jilin Province

  • Yanjie SHEN ,
  • Junru LI ,
  • Liya ZHANG ,
  • Yang ZHOU ,
  • Rihui CHENG
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  • 1. College of Earth Sciences, Jilin University, Changchun, Jilin 130061, China
    2. Sinopec Northeast Oil & Gas Company, Changchun, Jilin 130062, China
    3. Huanggu Research Center, Shenyang, Liaoning 110031, China

Received date: 2023-12-05

  Online published: 2024-05-07

摘要

为了解松辽盆地营城组火山岩类型、火山岩相类型及成因模式的复杂性、相关性之间的关系,明确其对于油气勘探的意义,利用野外露头、钻井资料、岩石薄片等多种地质资料,识别火山岩类型,划分火山岩相,分析了火山岩相成因特征。结果表明:①营城组发育4大类火山岩类型,即熔岩、火山碎屑熔岩、火山碎屑岩及碎屑沉积岩;②营城组野外露头划分了5种岩相类型,即火山口—火山通道型、火山口—破火山口型,近火山口—火山斜坡型、火山斜坡型和火山穹窿型;③建立了2类火山岩相成因模式,火山口堆积成因模式和火山斜坡成因模式。

本文引用格式

沈艳杰 , 李钧如 , 张立亚 , 周洋 , 程日辉 . 松辽盆地营城组火山岩相发育特征——以吉林省九台地区野外露头为例[J]. 油气藏评价与开发, 2024 , 14(2) : 224 -236 . DOI: 10.13809/j.cnki.cn32-1825/te.2024.02.008

Abstract

To explore the intricate relationship between volcanic rock types, volcanic facies, and genetic models within the Yingcheng Formation of the Songliao Basin, and to understand their implications for oil and gas exploration, a comprehensive analysis was conducted using a wide array of geological data. This included field outcrops, drilling data, and rock slices, allowing for the identification of volcanic rock types, classification of volcanic facies, and analysis of the genesis characteristics of these facies. It is concluded that: ①Four types of volcanic rocks are developed in Yingcheng Formation, which are lava, pyroclastic lava, pyroclastic rock, and clastic sedimentary rock; ②The outcrops of Yingcheng Formation are divided into five lithofacies types,which are crater facies-volcano channel type, crater-post volcanic type, near crater-volcano slope type, volcanic slope type and volcanic dome type; ③Two genetic modes of volcanic facies, crater accumulation genetic mode and volcanic slope genetic mode, are established.

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