Braided river reservoir architecture unit quantitative characterization method
A quantitative characterization, braided river technology, applied in special data processing applications, instruments, electrical digital data processing, etc., can solve the difficult to meet the preconditions for the estimation of the average thickness of the cross-bed series, the lack of coring data, the constraints and constraints. verification and other issues, to achieve the effect of loose application prospects, easy access, and accurate quantitative characterization
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Embodiment 1
[0057] This embodiment provides a quantitative characterization method for a braided river reservoir configuration unit, the reservoir configuration unit includes a braided channel and a composite channel in a single braided channel, including the following steps:
[0058] Step 1) Identify braided river reservoir architecture units according to the single well identification characteristics of channel banks and braided channels, draw a single-layer sand isopach map, and determine the planar distribution of braided channels in the same period;
[0059] Step 2) establishing a vertical braided channel well contrast section, and determining the boundary position between a single braided channel in a plurality of joint well contrast sections;
[0060] Step 3) Combining the single braided channel boundary between multiple well-connected comparison profiles, determining the plane distribution of the single braided channel in the single-layer sand body, and measuring the width of the s...
Embodiment 2
[0067] The braided river reservoir configuration unit quantitative characterization method provided by the present invention is used to analyze the 1-3 single-layer braided river gas reservoirs in the lower section of He 8 in Su X region.
[0068] The lower submember H of He 8 at the bottom of the Shihezi Formation in Su X area 8 The x sandstone is one of the most important reservoir sand bodies in this area. The lithology is mainly composed of medium-coarse lithic quartz sandstone and fine-medium lithic sandstone. The pore structure is composed of lithic dissolution pores and intercrystalline pores. Mainly secondary pores, with an average porosity of 9.6% and an average permeability of 0.71×10 -3 μm 2 , belonging to tight sandstone gas reservoirs with low porosity, low permeability and strong heterogeneity.
[0069] Subdivide box 8 lower subsection into H from top to bottom 8 x 1 and H 8 x 2 Two small layers and H 8 x 1-1 、H 8 x 1-2 、H 8 x 1-3 、H 8 x 2-1 、H 8 x...
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