Number-average size model for geological systems and its application in economic geology
Various natural objects follow a number-size relationship in the fractal domain. In such relationship, the accumulative number of the objects beyond a given size shows a power-law relationship with the size. Yet in most cases, we also need to know the relationship between the accumulative number of...
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2011-07-01
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Series: | Nonlinear Processes in Geophysics |
Online Access: | http://www.nonlin-processes-geophys.net/18/447/2011/npg-18-447-2011.pdf |
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doaj-85a127629404438ba75833af5e70f0332020-11-24T22:17:58ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462011-07-0118444745410.5194/npg-18-447-2011Number-average size model for geological systems and its application in economic geologyQ. F. WangL. WanY. ZhangJ. ZhaoH. LiuVarious natural objects follow a number-size relationship in the fractal domain. In such relationship, the accumulative number of the objects beyond a given size shows a power-law relationship with the size. Yet in most cases, we also need to know the relationship between the accumulative number of the objects and their average size. A generalized number-size model and a number-average size model are constructed in this paper. In the number-average size model, the accumulative number shows a power-law relationship with the average size when the given size is much less than the maximum size of the objects. When the fractal dimension <i>D</i><sub>s</sub> of the number-size model is smaller than 1, the fractal dimension <i>D</i><sub>s</sub> of the number-average size model is almost equal to 1; and when <i>D</i><sub>s</sub> > 1, the <i>D</i><sub>m</sub> is approximately equal to <i>D</i><sub>s</sub>. In mineral deposits, according to the number-average size model, the ore tonnage may show a fractal relationship with the grade, as the cutoff changes for a single ore deposit. This is demonstrated by a study of the relationship between tonnage and grade in the Reshuitang epithermal hot-spring gold deposit, China.http://www.nonlin-processes-geophys.net/18/447/2011/npg-18-447-2011.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Q. F. Wang L. Wan Y. Zhang J. Zhao H. Liu |
spellingShingle |
Q. F. Wang L. Wan Y. Zhang J. Zhao H. Liu Number-average size model for geological systems and its application in economic geology Nonlinear Processes in Geophysics |
author_facet |
Q. F. Wang L. Wan Y. Zhang J. Zhao H. Liu |
author_sort |
Q. F. Wang |
title |
Number-average size model for geological systems and its application in economic geology |
title_short |
Number-average size model for geological systems and its application in economic geology |
title_full |
Number-average size model for geological systems and its application in economic geology |
title_fullStr |
Number-average size model for geological systems and its application in economic geology |
title_full_unstemmed |
Number-average size model for geological systems and its application in economic geology |
title_sort |
number-average size model for geological systems and its application in economic geology |
publisher |
Copernicus Publications |
series |
Nonlinear Processes in Geophysics |
issn |
1023-5809 1607-7946 |
publishDate |
2011-07-01 |
description |
Various natural objects follow a number-size relationship in the fractal domain. In such relationship, the accumulative number of the objects beyond a given size shows a power-law relationship with the size. Yet in most cases, we also need to know the relationship between the accumulative number of the objects and their average size. A generalized number-size model and a number-average size model are constructed in this paper. In the number-average size model, the accumulative number shows a power-law relationship with the average size when the given size is much less than the maximum size of the objects. When the fractal dimension <i>D</i><sub>s</sub> of the number-size model is smaller than 1, the fractal dimension <i>D</i><sub>s</sub> of the number-average size model is almost equal to 1; and when <i>D</i><sub>s</sub> > 1, the <i>D</i><sub>m</sub> is approximately equal to <i>D</i><sub>s</sub>. In mineral deposits, according to the number-average size model, the ore tonnage may show a fractal relationship with the grade, as the cutoff changes for a single ore deposit. This is demonstrated by a study of the relationship between tonnage and grade in the Reshuitang epithermal hot-spring gold deposit, China. |
url |
http://www.nonlin-processes-geophys.net/18/447/2011/npg-18-447-2011.pdf |
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