Journal
JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING
Volume 197, Issue -, Pages -Publisher
ELSEVIER
DOI: 10.1016/j.petrol.2020.107943
Keywords
Diagenetic variations; Sediment composition; Paleo-fluids evolution; Conglomerate reservoir; Mahu sag
Categories
Funding
- National Natural Science Foundation of China [U1762217, 41702141]
- Innovation Research Group of the Natural Fund Committee [41821002]
- Fundamental Research Funds for the Central Universities [19 C x 02009 A]
- Opening Foundation of State Key Laboratory of Continental Dynamics [16LCD04]
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Understanding reservoir heterogeneity and associated diagenesis is crucial for efficient petroleum exploration. This study investigated diagenetic variations and factors controlling these processes using petrographic and geochemical methods. Mechanical compaction and chemical diagenesis trends varied as a function of rock types and geological locations, with thermodynamic instability leading to dissolution of tuffaceous matrix during burial diagenesis.
Understanding reservoir heterogeneity and associated diagenesis, have a paramount importance for efficient petroleum exploration and development strategies. Diagenetic variations and factors that control these processes have, therefore, been investigated in this study using petrographic and geochemical methods, including cath-odoluminescence, scanning electron microscopy, x-ray fluorescence, electron probe microanalyses and stable isotope analysis. Mechanical compaction and chemical diagenesis trends have obviously varied as a function of rock types and geological locations. The conglomerate reservoirs with high content of tuffaceous matrix and characterized by poor sorting showed stronger compaction. The tuffaceous matrix displays a large degree of dissolution during the progressive burial diagenesis due to its thermodynamic instability. The tuffaceous matrix in Na-rich conglomerate reservoir rocks mainly transformed into analcite, while it transformed into illite in K-rich conglomerate reservoir rocks. In most conglomerate reservoirs far away from deep-rooted faults, calcite cements are indicated to have been sourced from the decarboxylation of organic matter in the interbedded mudstones. Carbonate cements in conglomerate reservoirs near the deep-rooted faults possibly formed from hydrothermal fluids or thermochemical oxidation of pre-existing methane accumulations. This study can serve us an excellent example for the control of sediment composition and paleo-fluid evolution on diagenetic variations in fan-delta conglomerate reservoirs.
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