Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia)

Thirty-eight samples of minerals from Paleoproterozoic Layered PGE Intrusion Monchepluton, located in NE Fennoscandia, were tested. An automated computational technique was used which involved counting the sides superimposed on vectorized graphics using separated crystal boundaries. The results were...

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Published in:Minerals
Main Authors: Miłosz Huber, Klaudia Stępniewska
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/min11101140
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author Miłosz Huber
Klaudia Stępniewska
author_facet Miłosz Huber
Klaudia Stępniewska
author_sort Miłosz Huber
collection MDPI Open Access Publishing
container_issue 10
container_start_page 1140
container_title Minerals
container_volume 11
description Thirty-eight samples of minerals from Paleoproterozoic Layered PGE Intrusion Monchepluton, located in NE Fennoscandia, were tested. An automated computational technique was used which involved counting the sides superimposed on vectorized graphics using separated crystal boundaries. The results were obtained for olivine, orthopyroxene, clinopyroxene, and plagioclase. On this basis, an interpretation of the mineral box fractal dimension was made, along with an interpretation of its nature in the rock in which it was found. The performed calculations were applied to the sampling positions, and maps of changes in fractal dimensions were prepared. The nature of the minerals studied was correlated with the type of rocks present in Monchepluton. Then, the fractal dimensions were scaled to a percentage scale determining the mean value for the euhedral crystal as 100%, and a map was obtained representing the advancement of secondary processes after summing these data for all four investigated minerals. This method was analyzed and its advantages and limitations shown.
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op_doi https://doi.org/10.3390/min11101140
op_relation Crystallography and Physical Chemistry of Minerals & Nanominerals
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op_rights https://creativecommons.org/licenses/by/4.0/
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spelling ftmdpi:oai:mdpi.com:/2075-163X/11/10/1140/ 2025-01-16T21:50:19+00:00 Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia) Miłosz Huber Klaudia Stępniewska agris 2021-10-17 application/pdf https://doi.org/10.3390/min11101140 EN eng Multidisciplinary Digital Publishing Institute Crystallography and Physical Chemistry of Minerals & Nanominerals https://dx.doi.org/10.3390/min11101140 https://creativecommons.org/licenses/by/4.0/ Minerals; Volume 11; Issue 10; Pages: 1140 fractal dimension rock-forming minerals Monchepluton NE Fennoscandia Text 2021 ftmdpi https://doi.org/10.3390/min11101140 2023-08-01T02:58:59Z Thirty-eight samples of minerals from Paleoproterozoic Layered PGE Intrusion Monchepluton, located in NE Fennoscandia, were tested. An automated computational technique was used which involved counting the sides superimposed on vectorized graphics using separated crystal boundaries. The results were obtained for olivine, orthopyroxene, clinopyroxene, and plagioclase. On this basis, an interpretation of the mineral box fractal dimension was made, along with an interpretation of its nature in the rock in which it was found. The performed calculations were applied to the sampling positions, and maps of changes in fractal dimensions were prepared. The nature of the minerals studied was correlated with the type of rocks present in Monchepluton. Then, the fractal dimensions were scaled to a percentage scale determining the mean value for the euhedral crystal as 100%, and a map was obtained representing the advancement of secondary processes after summing these data for all four investigated minerals. This method was analyzed and its advantages and limitations shown. Text Fennoscandia MDPI Open Access Publishing Minerals 11 10 1140
spellingShingle fractal dimension
rock-forming minerals
Monchepluton
NE Fennoscandia
Miłosz Huber
Klaudia Stępniewska
Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia)
title Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia)
title_full Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia)
title_fullStr Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia)
title_full_unstemmed Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia)
title_short Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia)
title_sort application of the fractal dimension calculation technique to determine the shape of selected monchepluton intrusion crystals (ne fennoscandia)
topic fractal dimension
rock-forming minerals
Monchepluton
NE Fennoscandia
topic_facet fractal dimension
rock-forming minerals
Monchepluton
NE Fennoscandia
url https://doi.org/10.3390/min11101140