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深层储集层长石溶蚀增孔的物理模拟与定量计算

高志勇 冯佳睿 崔京钢 王晓琦 周川闽 石雨昕

石油勘探与开发2017,Vol.44Issue(3):359-369,11.
石油勘探与开发2017,Vol.44Issue(3):359-369,11.DOI:10.11698/PED.2017.03.05

深层储集层长石溶蚀增孔的物理模拟与定量计算

Physical simulation and quantitative calculation of increased feldspar dissolution pores in deep reservoirs

高志勇 1冯佳睿 2崔京钢 1王晓琦 2周川闽 1石雨昕2

作者信息

  • 1. 提高石油采收率国家重点实验室,北京100083
  • 2. 中国石油勘探开发研究院,北京100083
  • 折叠

摘要

Abstract

The physical simulation of diagenesis was conducted for the Cretaceous Bashijiqike Formation deep sandstone reservoir in Kelasu structural belt of Kuqa Depression,Tarim Basin,and the dissolution rate and increased dissolution pores of feldspar matrix grains in such reservoirs were quantitatively calculated in the process from long-term shallow burial in early stage to quick deep burial in late stage.Through the field emission large-area SEM analysis,the dissolution rate and increased dissolution pores of feldspar matrix grains in core samples taken from Dabei and Keshen areas were quantitatively calculated.After the experimental data and the actual core data were cross-checked,the evolution model was established for increased feldspar dissolution pores in deep continental reservoirs with high content of feldspar matrix grains.According to the calculation results,the maximum increased feldspar dissolution pores in Keshen area during the process from long-term shallow burial in early stage to quick deep burial in late stage is by 0.86%-2.05%.The simulated sandstone reservoir with burial depth of more than 7 000 m reveals a larger quantity of increased feldspar dissolution pores,with the absolute error value of 0.23% after calibration.In Dabei area,calcite is the primary contributor to secondary dissolution pores,followed by feldspar.Quantitative calculation shows the maximum increased feldspar dissolution pores in Dabei area to be by 0.62%-1.48%.Similarly,the simulated sandstone reservoir with burial depth of more than 7 000 m reveals a larger quantity of increased feldsPar dissolution pores,with the absolute error value of 0.15% after calibration.There are two causes of the experiment errors:One cause is that the simulation experiment uses ideal conditions and the simulation reservoirs are homogeneous;Another one is that deep reservoirs have strong heterogeneity and there are big differences in the dissolution within different areas.

关键词

库车坳陷/深层储集层/长石溶蚀/溶蚀增孔/成岩物理模拟

Key words

Kuqa Depression/deep reservoir/feldspar dissolution/increased dissolution pore/physical simulation of diagenesis

分类

能源科技

引用本文复制引用

高志勇,冯佳睿,崔京钢,王晓琦,周川闽,石雨昕..深层储集层长石溶蚀增孔的物理模拟与定量计算[J].石油勘探与开发,2017,44(3):359-369,11.

基金项目

国家科技重大专项“前陆冲断带及复杂构造区地质演化过程、深层结构与储集层特征”(2016ZX05003-001) (2016ZX05003-001)

中国石油天然气股份有限公司课题(2014E-3209 ()

2016B-0502 ()

2016B-0302) ()

石油勘探与开发

OA北大核心CSCDCSTPCDSCI

1000-0747

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