Quantitative prediction method of feldspar dissolution and porosity increase
A prediction method and dissolution technology, applied in the field of oil and gas exploration and development, can solve problems such as one-sidedness, single prediction method, and inability to carry out comprehensive quantitative prediction
- Summary
- Abstract
- Description
- Claims
- Application Information
AI Technical Summary
Problems solved by technology
Method used
Image
Examples
Embodiment 1
[0083] The quantitative prediction method of feldspar dissolution and porosity increase comprises the following steps:
[0084] 1) Analyze the geological situation of the study area
[0085] Including regional geological background, basin type, structural features, background content of related strata
[0086] 2) Establish a diagenetic stage prediction model
[0087] (1) Determine the evolution period
[0088] According to the development of the overlying strata of the target layer, the evolution stages of the target layer in the geological history period are divided. The overlying stratum of the target layer L has i layers, which are marked from top to bottom: L1, L2, L3...Li-1 , Li, then there are a total of i target layers in the evolution stages of the geological history period, according to the time evolution, the evolution stages of the target layer L are successively counted as Li, Li-1, Li-2...L2, L1;
[0089] (2) Determine the buried depth of different phases
[0...
Embodiment 2
[0135] Based on the above method, the quantitative prediction of feldspar dissolution and porosity increase in the second member of Dongying Formation in Bozhong sag is carried out. The specific method steps are as follows:
[0136] 1) Analyze the geological situation of the study area
[0137] Taking the second member of the Dongying Formation in the Bozhong Sag as an example, the structural contour maps of the second member of the Dongying Formation at each evolution stage were collected ( figure 1 , figure 2 , image 3 , Figure 4 ), fluid distribution map ( Figure 5 , Image 6 , Figure 7 ),Geothermal( Figure 8 , Figure 9 , Figure 10 ) to determine the diagenetic stage
[0138] 2) Determine the diagenetic stage
[0139] (1) Determine the evolution period
[0140] The overlying strata of the second member of the Dongying Formation are Pingyuan Formation, Minghuazhen Formation, and Guantao Formation from top to bottom, which are marked as L1, L2, and L3 from ...
PUM
Login to View More Abstract
Description
Claims
Application Information
Login to View More 


