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准噶尔盆地中拐凸起二叠系佳木河组砂砾岩沸石胶结特征及其成岩机制分析

吴和源 唐勇 孙玮 王学勇 常秋生

岩石矿物学杂志2018,Vol.37Issue(1):75-86,12.
岩石矿物学杂志2018,Vol.37Issue(1):75-86,12.

准噶尔盆地中拐凸起二叠系佳木河组砂砾岩沸石胶结特征及其成岩机制分析

An analysis of the zeolite cement in sand-conglomerate and the diagenetic mechanism of Jiamuhe Formation, Zhongguai area, Junggar Basin

吴和源 1唐勇 2孙玮 3王学勇 3常秋生4

作者信息

  • 1. 西安石油大学地球科学与工程学院,陕西西安710065
  • 2. 中国石油新疆油田公司博士后工作站,新疆克拉玛依834000
  • 3. 中国石油新疆油田分公司勘探开发研究院,新疆克拉玛依834000
  • 4. 中国石油新疆油田分公司采油二厂,新疆克拉玛依834000
  • 折叠

摘要

Abstract

Zeolite cementation is extensively developed in sand-conglomerate of Jiamuhe Formation in Zhongguai bulge,Junggar Basin.The analysis of cement characteristics and diagenesis of zeolite is of great importance for genetic mechanism exploration of the reservoir.Based on core and microscope observation,in combination with geochemical test methods such as electronic microprobe analysis,the authors studied the lithologic features,cementation and dissolution characteristics of Jiamuhe Formation.The results show that the sand-conglomerate of Jiamuhe Formation has developed zeolite,analcite,laumontite,and heulandite.There is no obvious cement zonality between different types of zeolite.Meanwhile the sand-conglomerate is often cemented by multi-period and multi-type zeolite,it is concluded that these cement characteristics had an inseparable relationship with diagenetic environment.It was a comprehensive response result of different stages of diagenetic environment on the basis of a transient openness alkaline diagenetic environment of the early stage,assisted by several alternations between acid-base diagenetic environments of the middle stage,and dominated by a long-term closed alkaline diagenetic environment of the late stage.

关键词

沸石/胶结作用/准噶尔盆地/佳木河组

Key words

zeolite/cementaion/Junggar Basin/Jiamuhe Formation

分类

天文与地球科学

引用本文复制引用

吴和源,唐勇,孙玮,王学勇,常秋生..准噶尔盆地中拐凸起二叠系佳木河组砂砾岩沸石胶结特征及其成岩机制分析[J].岩石矿物学杂志,2018,37(1):75-86,12.

基金项目

National Oil and Gas Major Projects(2016ZX05047001-004)国家油气重大专项(2016ZX05047001-004) (2016ZX05047001-004)

岩石矿物学杂志

OA北大核心CSCDCSTPCD

1000-6524

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