River island form quantitative characterization method
A quantitative characterization and morphology technology, applied in geophysical surveying, special data processing applications, instruments, etc., can solve problems such as high data requirements and complex quantitative analysis and description of reservoir mid-shoals
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Embodiment 1
[0031] Taking a fluvial facies reservoir development area A in the northern margin of a certain basin as an example, the quantitative characterization method for channel shoal morphology provided by the present invention is introduced in detail, figure 1 It is a flow chart of the quantitative characterization method of the shoal morphology of the present invention, specifically, including the following steps:
[0032] (1) According to the actual drilled core data of 20 coring single wells in the target area, the single-period mid-shoal is identified and the thickness of the single-stage mid-shoal is measured; Table 1 shows the statistics of the single-stage mid-shoal thickness.
[0033] Table 1
[0034]
[0035]
[0036] In this example, the sandstone particle size value in the known coring data is used. When the sandstone particle size value is <2mm, and the pebble-coarse sandstone or coarse sandstone is oriented, it is judged as a core bank. Combined with the core data...
Embodiment 2
[0059] The difference between the quantitative characterization method of the mid-shoal proposed in this example and the first embodiment of the quantitative characterization method of the mid-shoal lies in the different means of measuring the thickness of the mid-shoal. This embodiment uses the combination of well logging data, such as figure 2 As shown, the single-period cardiac beach thickness was measured.
[0060] The single-period mid-shoal thickness in this embodiment is obtained through the well logging curve in the known logging data, that is, GR<55API in the natural gamma ray curve in the logging data, when the logging curve presents a box-shaped feature, then It is judged as the central beach, which is obtained by directly reading the single-phase central beach thickness at the central beach position.
[0061] The other implementation steps of the quantitative characterization method for the midshore are basically the same as in the first embodiment of the quantita...
Embodiment 3
[0063] The difference between the channel shoal quantitative characterization method proposed in this example and the first embodiment of the channel shoal quantitative characterization method is that the means of geological statistics are different, that is, the geological statistics of modern rivers in typical braided river depositional areas are carried out by ArcGIS software , to establish a quantitative midshore geological database.
[0064] Wherein, in this embodiment, the river network in the braided river deposition area is directly extracted and analyzed through ArcGIS software, and the specific means are existing technologies, which will not be described in this embodiment.
[0065] The other implementation steps of the quantitative characterization method for the midshore are basically the same as in the first embodiment of the quantitative characterization method for the midshore, which have been introduced in the first embodiment of the quantitative characterizatio...
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