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- W4285288354 abstract "Summary Marine clastic reservoirs have good petrophysical properties, high reserves abundance. However, dolomitic barrier and baffle are developed in those reservoirs which will affect development and further enhancement of oil recovery. Identification, mechanism and distribution of dolomitic barrier and baffle are important for development and it can shed light on the mechanism of dolomitization. The research shows that: (1)The main lithology are dolomite bearing sandstone, dolomitic sandstone, sandy dolomite and sand bearing dolomite. (2) Qualitative and quantitative criteria were made to identify different degrees of dolomitization. With the increase degree of dolomitization, core appears to brighten under white light. Gamma, density and resistivity value increase. (3) The underground magnesium-rich brine and mudstone compaction water are the main ion sources. Sand with good properties and unconformity are the main fluid channels. Difference in the petrophysical properties determined contact time between pore fluid and particles, which leads to the difference degree of dolomization. (4) At macro-level, barriers and baffles tend to occur in middle period of sea level rising or descending. While at meso-level, they are more likely to occur in top and edge of channel. When it comes to micro-level, they tend to occur in areas where pore throats are poorly connected." @default.
- W4285288354 created "2022-07-14" @default.
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- W4285288354 date "2022-01-01" @default.
- W4285288354 modified "2023-09-26" @default.
- W4285288354 title "Identification, Mechanism and Distribution of Dolomitic Barrier and Baffle in Marine Clastic Reservoir" @default.
- W4285288354 doi "https://doi.org/10.3997/2214-4609.202210659" @default.
- W4285288354 hasPublicationYear "2022" @default.
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