Logging and seismic data fusion-based formation lithology inversion method
A technology of lithology and formation, applied in seismology, geophysical measurement, seismic signal processing, etc., can solve the problem of low vertical resolution of seismic lithology prediction, and achieve the effect of improving vertical resolution
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Embodiment 1
[0160] In this example, based on the geological characteristics and data quality of the actual data of a sag in the Bohai Bay Basin, given the geological model and pseudo-well, the forward modeling simulation of seismic data is carried out, and the conventional constrained sparse pulse inversion and the embodiment of the present invention are respectively carried out by using the forward modeling data. The formation lithology inversion of well-seismic fusion is provided, and the two methods are compared.
[0161] Firstly, a sand-mudstone geological model is established, and its section is shown in figure 1 As shown, the model length is 1000 channels, the channel spacing is 12.5m, the sandstone velocity is 3280m / s, and the density is 2.28g / cm 3 , mudstone velocity is 3600m / s, density is 2.4g / cm 3 , the Guantao Formation is shielded by extremely thick igneous rocks, and the quality of middle-deep seismic data is poor.
[0162] The formation lithology inversion using the well-s...
Embodiment 2
[0179] The MTY bulge is located in the northeast of a certain depression in the Bohai Bay Basin. It is a draped structure developed on the Archaean granite basement. The fluvial reservoirs of the Guantao Formation are the main distribution area of oil and gas, and the reservoirs are thin and change rapidly. The deposition of the third member of Guan is in the stage of filling and filling, and the second member of Guan is in the stage of steady deposition. Petrophysical analysis shows that the wave impedance of sandstone and mudstone has a cross phenomenon, and the thin sand layer of the Guan 2 Member and the thick sand body of the Guan 3 Member cannot be accurately identified by using constrained sparse pulse inversion, and the geostatistical inversion cannot objectively reflect the lateral direction of the sand bodies. Distribution characteristics, the boundary of channel sand bodies cannot be identified.
[0180] Based on the above background, this embodiment uses the same...
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