A Quantitative Analysis Method for Multilayer Near-Surface Seismic Geological Complexity
A quantitative analysis and complexity technology, applied in the field of geophysical exploration, can solve problems such as inability to apply quantitative analysis of surface complexity and difficulty in finding
- Summary
- Abstract
- Description
- Claims
- Application Information
AI Technical Summary
Problems solved by technology
Method used
Image
Examples
experiment example 1
[0190] Experimental example 1. Mountain topography models with different heights
[0191] In this experimental example, four models with peak heights of 160m, 240m, 320m and 400m are set, which are respectively recorded as model (a), model (b), model (c) and model (d), as Figure 3 ~ Figure 6 As shown, the horizontal spans of the four models are all 2000m, and the number of boundary elements is 200. Utilize the method provided by the present invention to quantitatively analyze its complexity, and its corresponding Matrix such as Figure 7 ~ Figure 10 As shown, its gray value increases with the increase of mountain height, and its complexity coefficient is as follows Figure 64 As shown in the middle curve 1, it also increases with the increase of mountain height, and the increasing complexity coefficient reflects that the complexity increases with the increase of relative height difference.
experiment example 2
[0192] Experimental Example 2 Mountain topography models with different slopes
[0193] In this experimental example, four models with gradually increasing mountain slopes are set, and the slopes are 25°, 35°, 45° and 65° respectively, which are respectively denoted as model (a), model (b), and model (c ) and model (d), such as Figure 11 to Figure 14 As shown, using the method provided by the invention to quantitatively analyze its complexity, its corresponding Matrix such as Figure 15 ~ Figure 18 As shown, its gray value increases with the increase of the slope of the mountain, and its complexity coefficient is as follows Figure 64 As shown in the middle curve 2, it also increases with the increase of the slope of the mountain.
experiment example 3
[0194] Experimental example 3 Landform models with different horizontal spans
[0195] In this experimental example, four geomorphic models with different horizontal spans are set, respectively 2000m, 1500m, 1000m and 500m, which are respectively recorded as model (a), model (b), model (c) and model (d) ,Such as Figure 19 ~ Figure 22 As shown, using the method provided by the invention to quantitatively analyze its complexity, its corresponding Matrix such as Figure 23 to Figure 26 As shown, its gray value decreases as the horizontal span increases, and its complexity coefficient is as follows Figure 64 As shown in curve 3, by Figure 64 The middle curve 3 shows that the smaller the horizontal span, the stronger the complexity, that is, when the mountain peak remains unchanged and the horizontal part extends infinitely, the influence of the mountain peak will gradually weaken.
PUM
Login to View More Abstract
Description
Claims
Application Information
Login to View More 


