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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Main Authors: Q. F. Wang, L. Wan, Y. Zhang, J. Zhao, H. Liu
Format: Article
Language:English
Published: Copernicus Publications 2011-07-01
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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spelling 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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