The impacts of diagenetic facies on reservoir quality in tight sandstones

The impact of diagenetic minerals and the characteristics of pore structures on reservoir qualities has been studied separately in the past years. However, the difference in the reservoir quality with different pore structures and having same or similar content of diagenesis minerals has not been as...

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Main Authors: Ren Dazhong, Sun Liang, Li Rongxi, Liu Dengke
Format: Article
Language:English
Published: De Gruyter 2020-10-01
Series:Open Geosciences
Subjects:
Online Access:https://doi.org/10.1515/geo-2020-0174
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spelling doaj-aee2be6b433d408cb498d4837d4efc882021-09-05T20:50:52ZengDe GruyterOpen Geosciences2391-54472020-10-011211060108210.1515/geo-2020-0174geo-2020-0174The impacts of diagenetic facies on reservoir quality in tight sandstonesRen Dazhong0Sun Liang1Li Rongxi2Liu Dengke3School of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaXi’an Geological Survey Center, China Geological Survey, Xi’an 710054, ChinaSchool of Earth Science and Resources, Chang’an University, Xi’an 710054, ChinaShaanxi Key Laboratory of Advanced Stimulation Technolgy for Oil & Gas Reservoirs, College of Petroleum Engineering, Xi’an Shiyou University, Xian 710021, ChinaThe impact of diagenetic minerals and the characteristics of pore structures on reservoir qualities has been studied separately in the past years. However, the difference in the reservoir quality with different pore structures and having same or similar content of diagenesis minerals has not been ascertained. In this study, based on the core samples derived from Chang 6 member in the Ordos basin, various tests were performed to examine the sandstone diagenesis and investigate the pore structure. The results showed that there were five diagenetic facies by diagenetic and pore structure analyses, and the best reservoir quality rocks were found to have relatively low percentage of illite, carbonate cement, pore-filling chlorite, authigenic quartz, and relatively high proportion of intergranular pores. Smectite-to-illite reaction and chemical compaction were main sources for quartz cementation at 60–120°C, and carbonate content was found to increase toward source rocks. The porosity depth trends significantly affected the diagenetic facies. The diagenetic and the pore structure pathways of various diagenetic facies were reconstructed by integrated petrographic, mineralogical, and pore system data. This study provides insights into the porosity evolution and diagenetic pathways of various diagenetic facies of tight sandstones, and the influence of diagenesis minerals and pore structures on their reservoir quality.https://doi.org/10.1515/geo-2020-0174diagenesispore structurediagenetic faciestight sandstoneyanchang formationordos basin
collection DOAJ
language English
format Article
sources DOAJ
author Ren Dazhong
Sun Liang
Li Rongxi
Liu Dengke
spellingShingle Ren Dazhong
Sun Liang
Li Rongxi
Liu Dengke
The impacts of diagenetic facies on reservoir quality in tight sandstones
Open Geosciences
diagenesis
pore structure
diagenetic facies
tight sandstone
yanchang formation
ordos basin
author_facet Ren Dazhong
Sun Liang
Li Rongxi
Liu Dengke
author_sort Ren Dazhong
title The impacts of diagenetic facies on reservoir quality in tight sandstones
title_short The impacts of diagenetic facies on reservoir quality in tight sandstones
title_full The impacts of diagenetic facies on reservoir quality in tight sandstones
title_fullStr The impacts of diagenetic facies on reservoir quality in tight sandstones
title_full_unstemmed The impacts of diagenetic facies on reservoir quality in tight sandstones
title_sort impacts of diagenetic facies on reservoir quality in tight sandstones
publisher De Gruyter
series Open Geosciences
issn 2391-5447
publishDate 2020-10-01
description The impact of diagenetic minerals and the characteristics of pore structures on reservoir qualities has been studied separately in the past years. However, the difference in the reservoir quality with different pore structures and having same or similar content of diagenesis minerals has not been ascertained. In this study, based on the core samples derived from Chang 6 member in the Ordos basin, various tests were performed to examine the sandstone diagenesis and investigate the pore structure. The results showed that there were five diagenetic facies by diagenetic and pore structure analyses, and the best reservoir quality rocks were found to have relatively low percentage of illite, carbonate cement, pore-filling chlorite, authigenic quartz, and relatively high proportion of intergranular pores. Smectite-to-illite reaction and chemical compaction were main sources for quartz cementation at 60–120°C, and carbonate content was found to increase toward source rocks. The porosity depth trends significantly affected the diagenetic facies. The diagenetic and the pore structure pathways of various diagenetic facies were reconstructed by integrated petrographic, mineralogical, and pore system data. This study provides insights into the porosity evolution and diagenetic pathways of various diagenetic facies of tight sandstones, and the influence of diagenesis minerals and pore structures on their reservoir quality.
topic diagenesis
pore structure
diagenetic facies
tight sandstone
yanchang formation
ordos basin
url https://doi.org/10.1515/geo-2020-0174
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