Research on the Diagenetic Facies Division and Pore Structure Characteristics of the Chang 6
Journal
ACS omega
ISSN: 2470-1343
Titre abrégé: ACS Omega
Pays: United States
ID NLM: 101691658
Informations de publication
Date de publication:
18 Jun 2024
18 Jun 2024
Historique:
received:
15
03
2024
revised:
20
05
2024
accepted:
21
05
2024
medline:
24
6
2024
pubmed:
24
6
2024
entrez:
24
6
2024
Statut:
epublish
Résumé
In tight sandstone reservoirs, diagenesis has a significant impact on the development of reservoirs and pore structures. To clarify the effect of diagenesis on the pore structure of tight sandstone, 12 samples of the Yanchang Formation in the basin were studied based on experiments such as high-pressure mercury intrusion and low-temperature nitrogen adsorption. The diagenetic facies in the study area are divided into two categories: strong cementation facies of carbonate minerals and strong compaction facies of soft component minerals, which are relatively unfavorable diagenetic facies, and stable facies of felsic minerals and strong dissolution facies of feldspar minerals, which are dominant diagenetic facies. The pore structure of the Chang 6
Identifiants
pubmed: 38911801
doi: 10.1021/acsomega.4c02550
pmc: PMC11191104
doi:
Types de publication
Journal Article
Langues
eng
Pagination
26363-26379Informations de copyright
© 2024 The Authors. Published by American Chemical Society.
Déclaration de conflit d'intérêts
The authors declare no competing financial interest.