Quantitative Prediction Method of Compaction Porosity Reduction
A prediction method and database technology, applied in the direction of prediction, data processing applications, instruments, etc., can solve the problem of not being able to comprehensively consider the physical property change law of sand body reservoirs, the reduction of primary pores, and the inability to further reveal the physical property change law of clastic rock reservoirs And other issues
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Embodiment 1
[0193] A quantitative prediction method for compaction porosity reduction, including the following steps:
[0194] 1) Collect geological data in the study area, which includes:
[0195] ①Study result map of sedimentary facies of the target layer in the study area;
[0196] ② Contour map of target layer interface structure;
[0197] ③ Contour map of the interface structure of the overlying strata on the target layer;
[0198] ④Reservoir physical property data in the study area;
[0199] ⑤Research results map of reservoir diagenetic facies in the study area;
[0200] ⑥Diagenetic evolution sequence in the study area;
[0201] ⑦The burial history and thermal evolution history of the study area;
[0202] 2) Establish the original data database
[0203] (1) Establishment of sedimentary facies type database
[0204] To study the original fabric of clastic rock reservoirs and the development of primary pores under the control of different sedimentary facies types, that is, the ...
Embodiment 2
[0360] Prediction of BZ19-2-1 in Bozhong Sag based on the above quantitative prediction method of porosity reduction by compaction: Analysis of D2 of the second member of East Member of Well BZ19-2-1 is shore-shallow lacustrine facies, and the lithology is medium-grained quartzite feldspar sandstone , the rock sorting is good, the grain size is sub-round, the average content of rigid particles is 68%, the mineral components are mainly feldspar and quartz, and the average content of feldspar in clastic rock is 53%. D2 of the second member of the East has experienced three evolutionary stages in the entire geological history, namely: IA, IB, and IIA. In the ⅠA evolution stage, the cementation type is muddy cement and calcareous cementation, and the cementation strength is medium; in the ⅠB evolution stage, the cementation type is muddy cementation and calcareous cementation, and the cementation strength is medium; in the ⅡA evolutionary stage, the cementation type is argillaceous...
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