2015
DOI: 10.1016/j.gexplo.2015.04.013
|View full text |Cite
|
Sign up to set email alerts
|

A comparative study of trend surface analysis and spectrum–area multifractal model to identify geochemical anomalies

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
12
0

Year Published

2017
2017
2022
2022

Publication Types

Select...
10

Relationship

0
10

Authors

Journals

citations
Cited by 56 publications
(14 citation statements)
references
References 52 publications
0
12
0
Order By: Relevance
“…In this study, the results of the moving weighted trend surface analysis showed that the ESV losses pattern of the agro-pastoral ecotone was similar to an “inclined surface”, i.e., the northeastern section of the ecotone lost more ESV than the other sections. This virtual “surface” is an expression of ecological vulnerability on a macro scale that is more sensitive to external disturbances [51,52]. The surface, which is a visible manifestation of strained human-land relations, was mainly formed by the long-term improper use of land resources and it provides a quantitative description of ESV losses.…”
Section: Discussionmentioning
confidence: 99%
“…In this study, the results of the moving weighted trend surface analysis showed that the ESV losses pattern of the agro-pastoral ecotone was similar to an “inclined surface”, i.e., the northeastern section of the ecotone lost more ESV than the other sections. This virtual “surface” is an expression of ecological vulnerability on a macro scale that is more sensitive to external disturbances [51,52]. The surface, which is a visible manifestation of strained human-land relations, was mainly formed by the long-term improper use of land resources and it provides a quantitative description of ESV losses.…”
Section: Discussionmentioning
confidence: 99%
“…The TSA method is a multivariate statistical analysis method that fits the spatial distribution and variability 0.4 ~ 1.6 τ ¼ 0:974290 À 0:08007ω 1.6 ~ 3.0 τ ¼ 1:031412 À 0:11536ω Low air (winter) 0.4 ~ 1.6 τ ¼ 0:982007 À 0:09611ω 1.6 ~ 3.0 τ ¼ 1:053710 À 0:14142ω of geographic drought variables and provides additional information by constructing surfaces that are usually decomposed into trend surfaces and residual surfaces (Eppler & Full, 1992;Wang & Zuo, 2015). Based on a previous study (Bai et al, 2017), we select the quadratic polynomial trend surface to produce the trend surface.…”
Section: Trend Surface Analysis Methodsmentioning
confidence: 99%
“…In spectrum method, the input data are transformed to frequency field using Fourier transforms. This means that the variations of the standard for all the positions of the input map (raw data) are converted to the frequency domain [21]. To execute, input data is prepared using an interpolation method in the form of a co-concentration line map.…”
Section: Spectrum-area Methodsmentioning
confidence: 99%