LAPSE:2023.14470
Published Article

LAPSE:2023.14470
The Nonuniform Distribution of Stylolite in Bioclastic Limestones and Its Influence on Reservoir Petro-Physical Properties—A Case Study of the Mishrif Formation from the Ah Oilfield
March 1, 2023
Abstract
The effect of stylolite caused by the pressure dissolution process on the reservoir petro-physical properties is still controversial. This study aims to reveal the effect of stylolite on the porosity and permeability of packstone and wackestone in the Mishrif Formation from the Ah oilfield in the Middle East. Based on the observation of thin sections and cores, X-ray diffraction analysis and porosity and permeability measurement, the lithofacies, diagenesis and patterns of stylolites have been investigated. There are six lithofacies in the Mi4 member, including bivalve green algae packstone, green algae packstone, pelletoid green algae packstone, echinoderm packstone, rudist packstone, planktonic foraminifera wackestone and bioclastic wackestone. The mechanical compaction and pressure dissolution could be observed in these lithofacies, with the development of dissolution seams and stylolites. The density of stylolite has a relationship with the lithofacies and early cementation. The boundary between the echinoderm packstone and the green algae packstone mostly developed as stylolites. There are four types of stylolite on the cores. Type A is the wave-like stylolite developed at the boundary between the echinoderm packstones and green algae packstones. Type B is the zigzag stylolite with high amplitude in the green algae packstones. Type C is the stylolites with low amplitude in the bioclastic wackestones. Type D is the high-angle stylolite, which is oblique to the bedding plane. The permeability of reservoir rocks could be improved by dissolution along the type B stylolite, while the type A and type C stylolite have little effect on permeability. The permeability of green algae packstone and echinoderm packstone will decrease with the development of stylolites. The porosity and permeability of bivalve green algae packstone will decrease after stylolitization, resulting from the relatively high density of stylolite. The physical properties of bioclastic wackestone could be improved by the bioturbation and formation of stylolite. According to the analysis of production performance in the same lithofacies, the occurrence of stylolites could result in the development of oil baffles. This study could be extended to evaluate the effect of stylolite in carbonate reservoir rocks.
The effect of stylolite caused by the pressure dissolution process on the reservoir petro-physical properties is still controversial. This study aims to reveal the effect of stylolite on the porosity and permeability of packstone and wackestone in the Mishrif Formation from the Ah oilfield in the Middle East. Based on the observation of thin sections and cores, X-ray diffraction analysis and porosity and permeability measurement, the lithofacies, diagenesis and patterns of stylolites have been investigated. There are six lithofacies in the Mi4 member, including bivalve green algae packstone, green algae packstone, pelletoid green algae packstone, echinoderm packstone, rudist packstone, planktonic foraminifera wackestone and bioclastic wackestone. The mechanical compaction and pressure dissolution could be observed in these lithofacies, with the development of dissolution seams and stylolites. The density of stylolite has a relationship with the lithofacies and early cementation. The boundary between the echinoderm packstone and the green algae packstone mostly developed as stylolites. There are four types of stylolite on the cores. Type A is the wave-like stylolite developed at the boundary between the echinoderm packstones and green algae packstones. Type B is the zigzag stylolite with high amplitude in the green algae packstones. Type C is the stylolites with low amplitude in the bioclastic wackestones. Type D is the high-angle stylolite, which is oblique to the bedding plane. The permeability of reservoir rocks could be improved by dissolution along the type B stylolite, while the type A and type C stylolite have little effect on permeability. The permeability of green algae packstone and echinoderm packstone will decrease with the development of stylolites. The porosity and permeability of bivalve green algae packstone will decrease after stylolitization, resulting from the relatively high density of stylolite. The physical properties of bioclastic wackestone could be improved by the bioturbation and formation of stylolite. According to the analysis of production performance in the same lithofacies, the occurrence of stylolites could result in the development of oil baffles. This study could be extended to evaluate the effect of stylolite in carbonate reservoir rocks.
Record ID
Keywords
anticline, Mishrif Formation, permeability, pressure dissolution, stylolite
Subject
Suggested Citation
Xu J, Deng Y, Fu M, Guo R, Chen P, Duan G, Ma R. The Nonuniform Distribution of Stylolite in Bioclastic Limestones and Its Influence on Reservoir Petro-Physical Properties—A Case Study of the Mishrif Formation from the Ah Oilfield. (2023). LAPSE:2023.14470
Author Affiliations
Xu J: Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
Deng Y: Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
Fu M: Energy College, Chengdu University of Technology, Chengdu 610059, China [ORCID]
Guo R: Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
Chen P: Energy College, Chengdu University of Technology, Chengdu 610059, China
Duan G: Energy College, Chengdu University of Technology, Chengdu 610059, China
Ma R: Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
Deng Y: Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
Fu M: Energy College, Chengdu University of Technology, Chengdu 610059, China [ORCID]
Guo R: Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
Chen P: Energy College, Chengdu University of Technology, Chengdu 610059, China
Duan G: Energy College, Chengdu University of Technology, Chengdu 610059, China
Ma R: Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
Journal Name
Energies
Volume
15
Issue
9
First Page
3032
Year
2022
Publication Date
2022-04-21
ISSN
1996-1073
Version Comments
Original Submission
Other Meta
PII: en15093032, Publication Type: Journal Article
Record Map
Published Article

LAPSE:2023.14470
This Record
External Link

https://doi.org/10.3390/en15093032
Publisher Version
Download
Meta
Record Statistics
Record Views
159
Version History
[v1] (Original Submission)
Mar 1, 2023
Verified by curator on
Mar 1, 2023
This Version Number
v1
Citations
Most Recent
This Version
URL Here
https://psecommunity.org/LAPSE:2023.14470
Record Owner
Auto Uploader for LAPSE
Links to Related Works
(0.21 seconds)
