Configuration cutting method of braided river tight-sandstone gas reservoir layer
A technology of tight sandstone gas reservoirs and braided rivers, applied in knowledge expression, instrumentation, electrical digital data processing, etc., can solve the problem of low recovery rate of gas fields and achieve significant benefits
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Embodiment 1
[0038] In order to overcome the problem of low recovery factor of existing gas field, the present invention provides such as figure 1 A braided river tight sandstone gas reservoir architecture anatomy method shown in the present invention is a practical and reliable braided river tight sandstone gas reservoir architecture anatomy method. The present invention improves the recovery rate of this type of gas field, and fine geological research urgently needs to carry out fine anatomical research on the reservoir configuration of braided river tight sandstone gas pools. This method is universal for reservoir architecture dissection, and is suitable for braided river reservoir gas fields with larger well pattern and well spacing than oil wells.
[0039] A method for dissecting the reservoir architecture of braided river tight sandstone gas reservoirs, the specific steps are as follows:
[0040] Step 1: Analyze the sedimentary discontinuities through the data of the braided river r...
Embodiment 2
[0056] Based on the basis of embodiment 1, in the present embodiment, in the step one, the braided river reservoir geological knowledge base includes:
[0057] a. Single channel width, thickness range and shape;
[0058] b. Width, thickness range and shape of braided channels;
[0059] c. Shoal width, length, thickness range and shape.
[0060] The content of the braided river reservoir geological knowledge base described in this step is the prior art, and will not be described in detail in the present invention.
[0061] The sedimentary discontinuities in the step 1 are three types of argillaceous interlayers, calcareous interlayers, or cut-and-stack sandstone electrical curve abrupt changes, wherein the lithology of the argillaceous interlayers is mudstone, silty mudstone, and argillaceous siltstone. Fine-grained material deposits formed due to lacustrine flooding; calcareous interlayers are conglomerate and coarse sandstone, at the end of channel deposition, the sedimenta...
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