| 注册
首页|期刊导航|沉积与特提斯地质|渝东北地区龙马溪组页岩孔隙结构特征及其主控因素

渝东北地区龙马溪组页岩孔隙结构特征及其主控因素

付文鼎 密文天 尚福华 麻书玮 朱悦雯 戴涛杰 朱炎铭 苗科 闫静 高海涛

沉积与特提斯地质2024,Vol.44Issue(4):796-808,13.
沉积与特提斯地质2024,Vol.44Issue(4):796-808,13.DOI:10.19826/j.cnki.1009-3850.2024.07001

渝东北地区龙马溪组页岩孔隙结构特征及其主控因素

Pore structure characteristics and main controlling factors of the Longmaxi shales in northeastern Chongqing

付文鼎 1密文天 1尚福华 2麻书玮 3朱悦雯 4戴涛杰 5朱炎铭 6苗科 1闫静 5高海涛7

作者信息

  • 1. 内蒙古工业大学资源与环境工程学院,内蒙古 呼和浩特 010051
  • 2. 内蒙古工业大学资源与环境工程学院,内蒙古 呼和浩特 010051||中国矿业大学 煤层气资源与成藏过程教育部重点实验室,江苏 徐州 221008||内蒙古矿业开发有限责任公司,内蒙古 呼和浩特 010051||内蒙古工业大学地质技术与岩土工程内蒙古自治区工程研究中心,内蒙古 呼和浩特 010051
  • 3. 中国石油长庆油田分公司勘探开发研究院,陕西 西安 710018
  • 4. 内蒙古工业大学地质技术与岩土工程内蒙古自治区工程研究中心,内蒙古 呼和浩特 010051
  • 5. 内蒙古矿业开发有限责任公司,内蒙古 呼和浩特 010051
  • 6. 中国矿业大学 煤层气资源与成藏过程教育部重点实验室,江苏 徐州 221008
  • 7. 中国科学院广州地球化学研究所,广东 广州 510640
  • 折叠

摘要

Abstract

To investigate the pore characteristics and controlling factors of the Longmaxi shales in northeastern Chongqing,this study samples 12 shales from the Longmaxi Formation and utilizes physical experiments,including field emission scanning electron microscopy(FE-SEM),liquid nitrogen adsorption and carbon dioxide adsorption,to characterize the pore structures.The pore structure parameters are then compared with those of shales from different tectonic zones in the Sichuan Basin.The results indicate that the pores of shales in the Longmaxi Formation in northeastern Chongqing are predominantly comprised of organic matter pores,inorganic pores and micro-fractures.Compared to the marine shales with similar maturity in southern Sichuan,these samples exhibit relatively fewer and smaller organic matter pores but more developed inorganic pores and micro-fractures.Based on the pore-fracture characteristics,inorganic pores can be classified into three types:intergranular pores,interlayer pores in clay minerals,and intragranular pores.Micro-fractures are categorized as organic matter-related micro-fractures and inorganic mineral-related micro-fractures.The influence of TOC content on pore structure occurs in two stages:when TOC content is less than 5.93%,it exhibits a strong positive correlation with micropore volume and specific surface area;when TOC content is more than 5.93%,it shows a negative correlation with these factors,and no correlation with mesoporous parameters.In addition,there is no significant correlation between the inorganic mineral(clay and brittle mineral)content and pore parameters.The SEM images also show that the tectonic compression reduces pore volume and pore connectivity,leading to the conversion of free gas into adsorbed gas in shale reservoirs,thus improving the gas storage capacity of the shales.The research results provide a theoretical basis for shale gas exploration in complex structural areas.

关键词

渝东北/龙马溪组/变形页岩/孔隙结构/主控因素

Key words

northeastern Chongqing/Longmaxi Formation/deformed shale/pore structure/controlling factor

分类

天文与地球科学

引用本文复制引用

付文鼎,密文天,尚福华,麻书玮,朱悦雯,戴涛杰,朱炎铭,苗科,闫静,高海涛..渝东北地区龙马溪组页岩孔隙结构特征及其主控因素[J].沉积与特提斯地质,2024,44(4):796-808,13.

基金项目

国家自然科学基金项目(42362022) (42362022)

内蒙古自然科学基金(2023QN04003,2024QN04003) (2023QN04003,2024QN04003)

内蒙古科技厅中央引导地方科技发展资金项目(2022ZY0083) (2022ZY0083)

内蒙古自治区高等学校碳达峰碳中和研究专项(STZX202212) (STZX202212)

中央引导地方科技发展资金(2022SZY0482) (2022SZY0482)

沉积与特提斯地质

OA北大核心CSTPCD

1009-3850

访问量0
|
下载量0
段落导航相关论文