8Faults can be either conduits or retarders for fluid flow. As the presence of 9 faults increases the risks for hydrocarbon exploration, the sealing behaviour 10 of a fault zone has been a focus for geological studies in the past 30 years. 11Due to the widespread occurrence of fault zones, either in extensional or 12 contractional regimes, knowledge about the fault sealing behaviour is of 13 great importance to a wide spectrum of disciplines in geosciences, for 14 instance, structural geology, geochemistry, petroleum geology, etc. 15Geologists have extensively study the sealing properties of a fault zone over 16 the last decades, ranging from fault zone architecture, fault seal types, fault 17 seal processes, fault rock classification, research methods and controlling 18 factors.
The sealing of a fault zone has been a focus for geological studies in the past decades. The majority of previous studies have focused on the extensional regimes, where the displacement pressure difference between fault rock and reservoir was used to evaluate the fault-sealing property from the basic principle of fault sealing. When considering the displacement pressure difference, the impact of gravity on the fault rock was considered, whereas the impact of horizontal stress was ignored. In this study, we utilize the displacement pressure difference as an index to evaluate the sealing capacity of strike-slip faults, in which both the impacts of gravity and horizontal stress on the fault rocks are all integrated. By calculating the values of σH/σV and σh/σV in the vicinity of fault planes, the coefficient K of compaction impacts on fault rocks between normal stress to fault planes and gravity was then determined. By revealing the quantitative relationship between the displacement pressure of rocks, burial depth and clay content, the displacement pressure difference between fault rocks and reservoirs were calculated. The results suggest that the sealing capacity of a strike-slip fault is not only related to the magnitude of normal stress to the fault plane, but also to the stress regime. The clay content is also an important factor controlling the sealing capacity of strike-slip faults.
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